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array:23 [ "pii" => "S0016716915000240" "issn" => "00167169" "doi" => "10.1016/j.gi.2015.04.021" "estado" => "S300" "fechaPublicacion" => "2015-07-01" "aid" => "21" "copyrightAnyo" => "2015" "documento" => "article" "crossmark" => 0 "licencia" => "http://creativecommons.org/licenses/by-nc-nd/4.0/" "subdocumento" => "fla" "cita" => "Geofisica Internacional. 2015;54:267-76" "abierto" => array:3 [ "ES" => true "ES2" => true "LATM" => true ] "gratuito" => true "lecturas" => array:2 [ "total" => 2073 "formatos" => array:3 [ "EPUB" => 106 "HTML" => 1452 "PDF" => 515 ] ] "itemSiguiente" => array:18 [ "pii" => "S0016716915000227" "issn" => "00167169" "doi" => "10.1016/j.gi.2015.04.019" "estado" => "S300" "fechaPublicacion" => "2015-07-01" "aid" => "19" "documento" => "article" "crossmark" => 0 "licencia" => "http://creativecommons.org/licenses/by-nc-nd/4.0/" "subdocumento" => "fla" "cita" => "Geofisica Internacional. 2015;54:277-87" "abierto" => array:3 [ "ES" => true "ES2" => true "LATM" => true ] "gratuito" => true "lecturas" => array:2 [ "total" => 1861 "formatos" => array:3 [ "EPUB" => 85 "HTML" => 1193 "PDF" => 583 ] ] "en" => array:11 [ "idiomaDefecto" => true "titulo" => "Evidence of pre-Columbian settlements in the forest of the Tuxtla Volcanic Field, Veracruz, Mexico" "tienePdf" => "en" "tieneTextoCompleto" => "en" "tieneResumen" => array:2 [ 0 => "es" 1 => "en" ] "paginas" => array:1 [ 0 => array:2 [ "paginaInicial" => "277" "paginaFinal" => "287" ] ] "contieneResumen" => array:2 [ "es" => true "en" => true ] "contieneTextoCompleto" => array:1 [ "en" => true ] "contienePdf" => array:1 [ "en" => true ] "resumenGrafico" => array:2 [ "original" => 0 "multimedia" => array:7 [ "identificador" => "fig0030" "etiqueta" => "Figure 6" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr6.jpeg" "Alto" => 1356 "Ancho" => 1455 "Tamanyo" => 267110 ] ] "descripcion" => array:1 [ "en" => "<p id="spar0040" class="elsevierStyleSimplePara elsevierViewall">Arroyo Toro Prieto (a) Schematic section of the deposit. (b) Aspect of the deposit. The insert shows some of the fragments collected at this site.(c) Granulometry of the matrix of the deposit.</p>" ] ] ] "autores" => array:1 [ 0 => array:2 [ "autoresLista" => "Araceli Zamora-Camacho, Juan Manuel Espíndola, Peter Schaaf, Angel Ramírez, María de Lourdes Godínez Calderón" "autores" => array:5 [ 0 => array:2 [ "nombre" => "Araceli" "apellidos" => "Zamora-Camacho" ] 1 => array:2 [ "nombre" => "Juan Manuel" "apellidos" => "Espíndola" ] 2 => array:2 [ "nombre" => "Peter" "apellidos" => "Schaaf" ] 3 => array:2 [ "nombre" => "Angel" "apellidos" => "Ramírez" ] 4 => array:2 [ "nombre" => "María de Lourdes Godínez" "apellidos" => "Calderón" ] ] ] ] ] "idiomaDefecto" => "en" "EPUB" => "https://multimedia.elsevier.es/PublicationsMultimediaV1/item/epub/S0016716915000227?idApp=UINPBA00004N" "url" => "/00167169/0000005400000003/v2_201509120041/S0016716915000227/v2_201509120041/en/main.assets" ] "itemAnterior" => array:18 [ "pii" => "S0016716915000203" "issn" => "00167169" "doi" => "10.1016/j.gi.2015.04.017" "estado" => "S300" "fechaPublicacion" => "2015-07-01" "aid" => "17" "documento" => "article" "crossmark" => 0 "licencia" => "http://creativecommons.org/licenses/by-nc-nd/4.0/" "subdocumento" => "fla" "cita" => "Geofisica Internacional. 2015;54:255-66" "abierto" => array:3 [ "ES" => true "ES2" => true "LATM" => true ] "gratuito" => true "lecturas" => array:2 [ "total" => 2787 "formatos" => array:3 [ "EPUB" => 116 "HTML" => 2023 "PDF" => 648 ] ] "en" => array:11 [ "idiomaDefecto" => true "titulo" => "Short Baseline Calibration using GPS and EDM Observations" "tienePdf" => "en" "tieneTextoCompleto" => "en" "tieneResumen" => array:2 [ 0 => "es" 1 => "en" ] "paginas" => array:1 [ 0 => array:2 [ "paginaInicial" => "255" "paginaFinal" => "266" ] ] "contieneResumen" => array:2 [ "es" => true "en" => true ] "contieneTextoCompleto" => array:1 [ "en" => true ] "contienePdf" => array:1 [ "en" => true ] "resumenGrafico" => array:2 [ "original" => 0 "multimedia" => array:7 [ "identificador" => "fig0055" "etiqueta" => "Figure 11" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr11.jpeg" "Alto" => 1707 "Ancho" => 2273 "Tamanyo" => 335899 ] ] "descripcion" => array:1 [ "en" => "<p id="spar0065" class="elsevierStyleSimplePara elsevierViewall">Calibration baseline results from GPS and EDM.</p>" ] ] ] "autores" => array:1 [ 0 => array:2 [ "autoresLista" => "Guadalupe Esteban Vazquez Becerra, Rick A. Bennett, Mijaíl Cordero Chávez, Manuel E. Trejo Soto, José Ramón Gaxiola-Camacho" "autores" => array:5 [ 0 => array:2 [ "nombre" => "Guadalupe Esteban Vazquez" "apellidos" => "Becerra" ] 1 => array:2 [ "nombre" => "Rick A." "apellidos" => "Bennett" ] 2 => array:2 [ "nombre" => "Mijaíl Cordero" "apellidos" => "Chávez" ] 3 => array:2 [ "nombre" => "Manuel E. Trejo" "apellidos" => "Soto" ] 4 => array:2 [ "nombre" => "José Ramón" "apellidos" => "Gaxiola-Camacho" ] ] ] ] ] "idiomaDefecto" => "en" "EPUB" => "https://multimedia.elsevier.es/PublicationsMultimediaV1/item/epub/S0016716915000203?idApp=UINPBA00004N" "url" => "/00167169/0000005400000003/v2_201509120041/S0016716915000203/v2_201509120041/en/main.assets" ] "en" => array:19 [ "idiomaDefecto" => true "cabecera" => "<span class="elsevierStyleTextfn">Original paper</span>" "titulo" => "Meteoric isotopic gradient on the windward side of theSierra Madre Oriental area, Veracruz – Mexico" "tieneTextoCompleto" => true "paginas" => array:1 [ 0 => array:2 [ "paginaInicial" => "267" "paginaFinal" => "276" ] ] "autores" => array:1 [ 0 => array:4 [ "autoresLista" => "Juan Pérez Quezadas, Alejandra Cortés Silva, Salvatore Inguaggiato, María del Rocío Salas Ortega, Juan Cervantes Pérez, Victor Michael Heilweil" "autores" => array:6 [ 0 => array:4 [ "nombre" => "Juan Pérez" "apellidos" => "Quezadas" "email" => array:1 [ 0 => "pquezadas_1@hotmail.com" ] "referencia" => array:2 [ 0 => array:2 [ "etiqueta" => "<span class="elsevierStyleSup">a</span>" "identificador" => "aff0005" ] 1 => array:2 [ "etiqueta" => "<span class="elsevierStyleSup">*</span>" "identificador" => "cor0005" ] ] ] 1 => array:3 [ "nombre" => "Alejandra Cortés" "apellidos" => "Silva" "referencia" => array:1 [ 0 => array:2 [ "etiqueta" => "<span class="elsevierStyleSup">b</span>" "identificador" => "aff0010" ] ] ] 2 => array:3 [ "nombre" => "Salvatore" "apellidos" => "Inguaggiato" "referencia" => array:1 [ 0 => array:2 [ "etiqueta" => "<span class="elsevierStyleSup">c</span>" "identificador" => "aff0015" ] ] ] 3 => array:3 [ "nombre" => "María del Rocío Salas" "apellidos" => "Ortega" "referencia" => array:1 [ 0 => array:2 [ "etiqueta" => "<span class="elsevierStyleSup">d</span>" "identificador" => "aff0020" ] ] ] 4 => array:3 [ "nombre" => "Juan Cervantes" "apellidos" => "Pérez" "referencia" => array:1 [ 0 => array:2 [ "etiqueta" => "<span class="elsevierStyleSup">d</span>" "identificador" => "aff0020" ] ] ] 5 => array:3 [ "nombre" => "Victor Michael" "apellidos" => "Heilweil" "referencia" => array:1 [ 0 => array:2 [ "etiqueta" => "<span class="elsevierStyleSup">e</span>" "identificador" => "aff0025" ] ] ] ] "afiliaciones" => array:5 [ 0 => array:3 [ "entidad" => "Centro de Geociencias Universidad Nacional Autónoma de México Campus Juriquilla Querétaro, Qro., México" "etiqueta" => "a" "identificador" => "aff0005" ] 1 => array:3 [ "entidad" => "Instituto de Geofísica, Universidad Nacional Autónoma de México Ciudad Universitaria Delegación Coyoacán, 04510 México, D.F., México" "etiqueta" => "b" "identificador" => "aff0010" ] 2 => array:3 [ "entidad" => "National Institute of Geophysics and Volcanology Palermo, Italy" "etiqueta" => "c" "identificador" => "aff0015" ] 3 => array:3 [ "entidad" => "Centro de Ciencias de la Tierra Universidad Veracruzana Xalapa, Veracruz, México" "etiqueta" => "d" "identificador" => "aff0020" ] 4 => array:3 [ "entidad" => "U.S. Geological Survey-Utah Water Science Center Salt Lake City, U.S.A." "etiqueta" => "e" "identificador" => "aff0025" ] ] "correspondencia" => array:1 [ 0 => array:3 [ "identificador" => "cor0005" "etiqueta" => "⁎" "correspondencia" => "Corresponding author." ] ] ] ] "resumenGrafico" => array:2 [ "original" => 0 "multimedia" => array:7 [ "identificador" => "fig0010" "etiqueta" => "Figure 2" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr2.jpeg" "Alto" => 1387 "Ancho" => 1851 "Tamanyo" => 293907 ] ] "descripcion" => array:1 [ "en" => "<p id="spar0025" class="elsevierStyleSimplePara elsevierViewall">Displays climograms located in the town of Tembladeras, Xalapa and Veracruz, located at 3000 masl., 1400 masl, and sea level, respectively (modified from <a class="elsevierStyleCrossRef" href="#bib0110">Tejeda <span class="elsevierStyleItalic">et al</span>., 1989</a>). Precipitation at the Port of Veracruz and at Tembladeras is concentrated in the months of June to September, with magnitudes as large as 350<span class="elsevierStyleHsp" style=""></span>mm. In contrast, the majority of rainfall in Xalapa is distributed over the months of May to October, with monthly averages less than 250<span class="elsevierStyleHsp" style=""></span>mm.</p>" ] ] ] "textoCompleto" => "<span class="elsevierStyleSections"><span id="sec0005" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0025">Introduction</span><p id="par0005" class="elsevierStylePara elsevierViewall">The isotopic characterization of local rainfall in water-resource studies is very important, considering that such precipitation typically represents the primary source of recharge to groundwater systems. This isotopic signature can subsequently be used to trace groundwater flow within the aquifer. On the basis of 400 stable isotopic (δ<span class="elsevierStyleSup">2</span>H and δ<span class="elsevierStyleSup">18</span>O) samples of water (rivers, rain and snow) at different geographical locations, the linear relationship δ<span class="elsevierStyleSup">2</span>H (δD) = 8δ<span class="elsevierStyleSup">18</span>O + 10 was defined by <a class="elsevierStyleCrossRef" href="#bib0030">Craig (1961)</a> as the Global Meteoric Water Line (GMWL). <a class="elsevierStyleCrossRef" href="#bib0035">Dansgaard (1964)</a>, using data from GNIP (Global Network of Isotopes in Precipitation, 2012), found that isotopic ratios of monthly precipitation recorded at stations located in the northern continental hemisphere complied with the GMWL. Significant deviations from the GMWL line, however, were observed relative to other continents and islands. These deviations were attributed to differences in the local weather conditions and in the processes controlling precipitation. The analysis of the GNIP data for the periods 1960-1978 and 1960-1987 were reported by <a class="elsevierStyleCrossRef" href="#bib0125">Yurtsever and Gat (1981)</a> and <a class="elsevierStyleCrossRef" href="#bib0100">Rozanski <span class="elsevierStyleItalic">et al</span>. (1993)</a>, respectively. Using the same methodology described by previous authors, the IAEA (<a class="elsevierStyleCrossRef" href="#bib0070">International Atomic Energy Agency, 2005</a>) processed data from 1961 to 2000 and found that the arithmetic mean of the isotopic ratios in precipitation recorded from 410 stations distributed globally are well-described by the equation: δD = 8.07 (± 0.02) δ<span class="elsevierStyleSup">18</span>O + 9.9(± 0.1), R<span class="elsevierStyleSup">2</span> = 0.98. The deuterium excess can be described globally as d<span class="elsevierStyleInf">ex</span> δ<span class="elsevierStyleSup">2</span>H - 8δ<span class="elsevierStyleSup">18</span>O.The weighted averages of long-term precipitation for the same period (1961-2000) were calculated by GNIP from a subset of measurements during years for which more than 70% of precipitation during that year was analyzed for a given isotope (with a minimum requirement of at least one full year of data). The weighted average correlation is δD= 8.14 (± 0.02) δ<span class="elsevierStyleSup">18</span>O +10.9 (± 0.2), R<span class="elsevierStyleSup">2</span> = 0.98.</p><p id="par0010" class="elsevierStylePara elsevierViewall">There are several widely documented effects that control the spatial variation of the isotopic composition in the meteoric waters including altitude, latitude, continental, amount and season (<a class="elsevierStyleCrossRef" href="#bib0010">Clark and Fritz, 1997</a>). Of these, altitude (topography) is considered the most important factor. It has been shown that on the windward side of the mountains, the δ<span class="elsevierStyleSup">18</span>O and δD ratios of rain decrease (become isotopically depleted) with increasing altitude. This is mainly due to the combination of two factors: (1) rainfall becomes progressively depleted by the loss of isotopically heavy isotopes as rain events progress in a topographically up gradient direction and, (2) the temperature is lower and thus the condensate becomes isotopically enriched because of fractionation (<a class="elsevierStyleCrossRef" href="#bib0010">Clark and Fritz, 1997</a>). Other hydrologic factors may affect the stable isotopic signature of precipitation at windward tropical forests. <a class="elsevierStyleCrossRef" href="#bib0120">Vogelmann (1973)</a> showed that evapotranspiration in a cloud forest of eastern Mexico was subsequently recycled as fog precipitation, which could affect its isotopic content. This process of fog interception was quantified in a cloud forest of Puerto Rico (<a class="elsevierStyleCrossRef" href="#bib0065">Holwerda <span class="elsevierStyleItalic">et al</span>., 2010</a>), accounting for about 10% of the total precipitation.</p><p id="par0015" class="elsevierStylePara elsevierViewall">The objective of this study is the isotopic characterization of precipitation on the windward (Atlantic) side of the Sierra Madre Oriental in the State of Veracruz, the most populated part of the State of Veracruz. The main scope of this work is the spatial and temporal isotopic characterization of meteoric waters and their possible relationship with dominant isotopic effects in our study area. Because the isotopic meteoric line varies with region, it was important to determine a local meteoric water line. Local conditions can also be described by the vertical isotopic gradient and the deuterium excess (d<span class="elsevierStyleInf">ex</span>), which can be used assess the difference between local conditions in Veracruz compared with to the global meteoric water line δD = 8 δ<span class="elsevierStyleSup">18</span>O + 10 (<a class="elsevierStyleCrossRef" href="#bib0030">Craig, 1961</a>). In this research, we show the isotopic relationship between δ<span class="elsevierStyleSup">18</span>O‰ and δD‰ measured in the cumulative rainfall as a time series based on samples was collected during six rainy seasons (2007-2012). Importantly we evaluate the isotopic gradient along a topographic transect from sea level to an altitude of over 4000 m. This characterization will increase the understanding of important hydrological processes and will provide a foundation for future hydrological research.</p></span><span id="sec0010" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0030">Study area</span><p id="par0020" class="elsevierStylePara elsevierViewall">The 2000<span class="elsevierStyleHsp" style=""></span>km<span class="elsevierStyleSup">2</span> study area is located in the central part of the state of Veracruz, Mexico, between 2110000 and 2180000 UTM coordinates north latitude (<a class="elsevierStyleCrossRef" href="#fig0005">Figure 1</a>). Its shape is elongated in an orientation northwest to south east (approximately 90<span class="elsevierStyleHsp" style=""></span>km long) and narrower from northeast to southwest (approximately 20<span class="elsevierStyleHsp" style=""></span>km wide). It is bounded on the east by the Gulf of Mexico and to the west by the Sierra Madre Oriental. The topographic relief is variable and characterized by two main areas: a lower and flatter area located along the coast, and a higher and steeper area located along the Sierra Madre Oriental (<a class="elsevierStyleCrossRefs" href="#bib0110">Tejeda <span class="elsevierStyleItalic">et al</span>., 1989; Barradas <span class="elsevierStyleItalic">et al</span>., 2004</a>).The altitudinal gradient is extremely large rising from sea level at the Port of Veracruz to 4220 masl at the peak of the extinct Cofre de Perote volcano (cross-section A-A’ of <a class="elsevierStyleCrossRef" href="#fig0005">Figure 1</a>).The isotopic gradient and precipitation patterns in the study area are greatly influenced by this topography.</p><elsevierMultimedia ident="fig0005"></elsevierMultimedia><p id="par0025" class="elsevierStylePara elsevierViewall">The climate within the study area varies from “tropical wet-and-dry” (average annual temperature > 18<span class="elsevierStyleHsp" style=""></span>°C and more than 150<span class="elsevierStyleHsp" style=""></span>mm precipitation during the summer months) at the Port of Veracruz to “humid subtropical” (average temperature > 10<span class="elsevierStyleHsp" style=""></span>°C during the warmest months and more than 1200<span class="elsevierStyleHsp" style=""></span>mm precipitation during the rainy season) in the Sierra Madre Oriental (<a href="http://geo-mexico.com/?p=9512">http://geo-mexico.com/?p=9512</a>). The maximum monthly air temperature ranges from 12<span class="elsevierStyleHsp" style=""></span>°C at Tembladeras to 23<span class="elsevierStyleHsp" style=""></span>°C at the Port of Veracruz (<a class="elsevierStyleCrossRef" href="#fig0010">Figure 2</a>). The seasonal variation of temperature at each of the three weather stations oscillates 4, 8 and 6<span class="elsevierStyleHsp" style=""></span>°C at 3000 masl, 1400 masl, and at sea level, respectively. The primary controls on the climate within the study area are the topography and the atmospheric circulation systems prevailing during the different seasons (<a class="elsevierStyleCrossRef" href="#bib0090">Mosiño and Garcia 1973</a>). These result in the occurrence of the rainy season during the summer and autumn. Although the study area is located in the tropics, precipitation is also affected by extra-tropical (mid-latitude) phenomena. Precipitation data during 1981-2010 from three precipitation stations located along the A-A’ transect (<a class="elsevierStyleCrossRef" href="#fig0005">Figure 1</a>) at Tembladeras, Xalapa, and the Port of Veracruz (3000 m a.s.l.,1400m a.s.l., andat sea level, respectively) illustrate the strength of rainy season during the months of May through October. More than 80% of total annual rainfall occurs during these months, (<a class="elsevierStyleCrossRef" href="#fig0010">Figure 2</a>). It is also interesting that the monthly amount during the rainy season is similar for both the high-altitude station (Tembladeras) and the low-altitude station (Port of Veracruz). In contrast, precipitation at Xalapa is much less. While rainfall during the months of July and August exceeds 300<span class="elsevierStyleHsp" style=""></span>mm at both Tembladeras and the Port of Veracruz, precipitation during the same months at Xalapa is less than 200<span class="elsevierStyleHsp" style=""></span>mm. It is theorized that a local vertical circulation pattern caused by a barometric pressure anomaly causes a microclimate that brings drier air to the Xalapa area during the summer months.</p><elsevierMultimedia ident="fig0010"></elsevierMultimedia><p id="par0030" class="elsevierStylePara elsevierViewall">There is also a large variability in total annual rainfall within the study area. Total annual rainfall varied from 2076 to 1206<span class="elsevierStyleHsp" style=""></span>mm at the Veracruz GNIP Station during 1962-1988. It is known that the effects of global phenomena such as El Niño - Southern Oscillation (ENSO; <a class="elsevierStyleCrossRef" href="#bib0095">Rasmusson and Wallace, 1983</a>), or La Niña (the negative phase), can result in excess rain in some parts of the state of Veracruz during the summer (<a class="elsevierStyleCrossRef" href="#bib0075">Magaña <span class="elsevierStyleItalic">et al</span>., 2003</a>). The Pacific Decadal Oscillation (PDO; <a class="elsevierStyleCrossRef" href="#bib0080">Mantua <span class="elsevierStyleItalic">et al</span>., 1997</a>), in its negative phase, can also induce excessive rain in southern portion of the state of Veracruz (<a class="elsevierStyleCrossRef" href="#bib0085">Mendez <span class="elsevierStyleItalic">et al</span>., 2010</a>). Lastly, the Atlantic Multidecadal Oscillation (AMO; <a class="elsevierStyleCrossRef" href="#bib0105">Sutton and Hodson, 2005</a>) can increase the frequency of hurricanes, causing excessive rainfall in the State of Veracruz, (<a class="elsevierStyleCrossRef" href="#bib0115">Vazquez, 2007</a>).</p><p id="par0035" class="elsevierStylePara elsevierViewall">The amount and relative δ<span class="elsevierStyleSup">18</span>O‰ isotopic composition of monthly precipitation measured by the IAEA during 1962-1988 at the Port of Veracruz (Global Network Isotopic Precipitation, 2012) is shown in <a class="elsevierStyleCrossRef" href="#fig0015">Figure 3</a>. The annual weighted isotopic composition for rainfall calculated by GNIP for the period 1962-1988 (Long Term Mean) is: δ<span class="elsevierStyleSup">18</span>O = - 4.09 ± 1.31 ‰, n = 110, and δD = - 26.8 ± 9.7 ‰, n = 78. Separately, we calculated the weighted isotopic composition of rainfall for just the rainy season (May through October) with δ<span class="elsevierStyleSup">18</span>O‰ and δD‰ of - 4.2 ‰ and - 24.2 ‰, respectively. Because these are not significant differences, it is assumed that the weighted isotopic composition precipitation during the rainy season is representative of the annual rainfall in the study area. <a class="elsevierStyleCrossRef" href="#fig0015">Figure 3</a> shows an inverse relationship between cumulative precipitation and δ<span class="elsevierStyleSup">18</span>O values. Yet during the “canicular days” (July and August), δ<span class="elsevierStyleSup">18</span>O‰ values increased by more than 1‰.</p><elsevierMultimedia ident="fig0015"></elsevierMultimedia></span><span id="sec0015" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0035">Methodology</span><p id="par0040" class="elsevierStylePara elsevierViewall">To achieve the objectives of this study, a network of temporary rain collectors were deployed along a transect from the Port of Veracuz at sea level to Cofre de Perote at 4220 mamsl. Rainfall was collected during the rainy season for a period of 6 years (2007 through 2012). Composite samples were collected at each site that included all precipitation during each rainy season (May through October). These were collected with a standard rain gauge by taking a composite sample of meteoric water over the entire rainy season.The rain gauge consists of a plastic funnel with a diameter of 40<span class="elsevierStyleHsp" style=""></span>cm connected to a storage container with sufficient capacity to store up to 5000<span class="elsevierStyleHsp" style=""></span>mm of precipitation.The containeris covered by three heat insulating materials: Poly foam, Mylar, and aluminum foil. 250<span class="elsevierStyleHsp" style=""></span>ml of inert Nujol mineral oil was added to minimize evaporation (Cortés <span class="elsevierStyleItalic">et al</span>., 2001). At the end of each rainy season, an aliquot of 60<span class="elsevierStyleHsp" style=""></span>ml of water was collected from each sample container and transferred to high density polyethylene bottles (Nalgen brand).</p><p id="par0045" class="elsevierStylePara elsevierViewall">The sites for the composite rainfall collectors were selected based on proximity to meteorological stations of the National Weather Service of Mexico that record the amount of precipitation. Before the rainy season of 2007, 11 rain gauges were installed at altitudes ranging from 8 masl at Veracruz and Antigua to 4220 masl at Cofre de Perote. These gauges were spatially distributed, as shown in <a class="elsevierStyleCrossRef" href="#fig0005">Figure 1</a>. Because of logistical problems, the network was modified every year by changing the number and location of the collectors. Seven rain gauges we installed during the rainy season of 2008, three of which were at the same sites as the previous year. Four gauges were installed during 2009, with three re-occupying previous sites. Eight gauges were installed during 2010, with four re-occupying previous sites. During both 2011 and 2012, gauges were installed at the seven sites (the same locations for both years), with three re-occupying previous sites. Over the 6-year collection period, therefore, a total of 44 collectors were utilized. The estimation of the elevation of the installed rain gauges was recorded with GPS integrated barometric altimeter (Garmin Etrex Summit brand, accuracy of ± 3 m), calibrated at sea level and compared with the topographic maps (1:50,000) published by INEGI (National Institute of Statistics, Geography and Informatics).</p><p id="par0050" class="elsevierStylePara elsevierViewall">The collected rain samples were analyzed for δ18O‰ and δD‰ at the Mass Spectrometry Laboratory (MSL) of the Institute of Geology at the National Autonomous University of Mexico (UNAM). The analytical uncertainties (1σ standard deviation) reported by the MSL-UNAM are δ<span class="elsevierStyleSup">18</span>O ∼± 0.1 ‰ and δD ∼± 1 ‰. Based on these, the estimated 1σ standard deviation for d<span class="elsevierStyleInf">ex</span> is±√[σ(δD)<span class="elsevierStyleSup">2</span> + 64 σ(δ<span class="elsevierStyleSup">18</span>O)<span class="elsevierStyleSup">2</span>], or ± 1.3 ‰. Replicate isotopic analyses were run for ten percent of samples to verify these analytical uncertainties. The reported values of δ<span class="elsevierStyleSup">18</span>O‰ and δD‰ are normalized to the international standards V-SMOW and SLAP, according to the recommendations of the IAEA, (<a class="elsevierStyleCrossRef" href="#bib0050">Gonfiantini, 1978</a>). Composite rainy season stable isotope values of samples collected at the 44 sites during this study were compared with data from the Port of Veracruz station, which was operated from 1962-1988 jointly by the Global Precipitation Isotopic Network (GPIN) and the International Atomic Energy Agency. The station has a record of 139 isotopic couples (δ<span class="elsevierStyleSup">18</span>O‰ and δD‰), 189 Tritium values, monthly precipitation, mean ambient temperature and vapor pressure (<a href="http://www.iaea.org/">www.iaea.org</a> / water, GNIP).</p></span><span id="sec0020" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0040">Results and discussion</span><p id="par0055" class="elsevierStylePara elsevierViewall"><a class="elsevierStyleCrossRef" href="#tbl0005">Table 1</a> shows the isotopic results of the meteoric water samples collected during 2007-2012. δ<span class="elsevierStyleSup">18</span>O ranges from - 3.3 ‰ to −15.3 ‰ and δD from −17.2 ‰ to −106.3‰.</p><elsevierMultimedia ident="tbl0005"></elsevierMultimedia><p id="par0060" class="elsevierStylePara elsevierViewall">Both isotopic ranges are large compared to the respective analytical uncertainties, ± 0.1 ‰ for δ<span class="elsevierStyleSup">18</span>O and ± 1.3 ‰ for δD. The isotopic pairs of δ<span class="elsevierStyleSup">18</span>O‰ and δ<span class="elsevierStyleSup">2</span>H‰ ranged from -3.3‰ and -17.2‰ at the Port of Veracruz (8 masl) in the rainy season of 2009 to -15.3‰ and -106.3‰ at Cofre de Perote (4200 masl) in the rainy season of 2007. These values are consistent with 2008-2010 precipitation data for Veracruz reported by Goldsmith <span class="elsevierStyleItalic">et al</span>. (2011). The deuterium excess values ranges between 7.0‰ and 17.4‰; the highest d<span class="elsevierStyleInf">ex</span> value was recorded at Cofre de Perote, indicating the largest separation from the LMWL.</p><p id="par0065" class="elsevierStylePara elsevierViewall"><a class="elsevierStyleCrossRef" href="#fig0020">Figure 4</a> shows the isotopic results for the study area, compared with the Global Meteoric Water Line, GMWL (<a class="elsevierStyleCrossRef" href="#bib0030">Craig, 1961</a>). Applying a linear regression on these results, the Local Meteoric Water Line (LMWL) for the upwind Sierra Madre Oriental study area is described by the equation δD= 7.44 δ<span class="elsevierStyleSup">18</span>O + 7.3. The deuterium excess for the more isotopically depleted samples can be seen by their slight divergence from the GMWL. This LMWL is similar to δD = 7.42 δ<span class="elsevierStyleSup">18</span>O + 7.9 for the Port of Veracruz (GNIP, 2014) but differs from another reported for the Coatepec area, also in the State of Veracruz, of δD = 8.21 δ<span class="elsevierStyleSup">18</span>O + 18.5 (<a class="elsevierStyleCrossRef" href="#bib0045">Goldsmith; 2011</a>). Our LMWL for the upwind Sierra Madre Oriental study area also differs from those reported for other parts of Mexico: δD = 7.46 δ<span class="elsevierStyleSup">18</span>O + 8.9 for the Colima Volcano area in the Mexican Pacific (<a class="elsevierStyleCrossRef" href="#bib0060">Hartsough <span class="elsevierStyleItalic">et al</span>., 2008</a>); δD = 8 δ<span class="elsevierStyleSup">18</span>O + 11 for the central highlands of Mexico (based on data collected during the same years as for the Port of Veracruz; <a class="elsevierStyleCrossRef" href="#bib0020">Cortes <span class="elsevierStyleItalic">et al</span>., 1997</a>); and δD = 7.7 δ<span class="elsevierStyleSup">18</span>O + 10.8 for the Transmexican Volcanic Belt (which is almost identical to theGMWL). These different LMLs show how the stable isotopic composition of precipitation is strongly influenced by local climatic conditions.</p><elsevierMultimedia ident="fig0020"></elsevierMultimedia><p id="par0070" class="elsevierStylePara elsevierViewall">The vertical isotopic gradient of precipitation along transect A-A’ (<a class="elsevierStyleCrossRef" href="#fig0005">figure 1</a>) of the study area was determined least squares linear regression of δ<span class="elsevierStyleSup">18</span>O versus altitude for meteoric water samples collected during 2007-2012, yielding the relation δ<span class="elsevierStyleSup">18</span>O = -2.1*Z (km) - 5.56‰; r<span class="elsevierStyleSup">2</span> = 0.87 (<a class="elsevierStyleCrossRef" href="#fig0025">Figure 5</a>a). The same vertical gradient was also found for precipitation in the Central Mexican Plateau (<a class="elsevierStyleCrossRefs" href="#bib0040">Durazo, 2008; Cortés and Durazo, 2001</a>), but with a smaller y intercept value -3.26‰. A similar vertical isotopic gradient was calculated for deuterium: δD = -15.3*Z (km) - 34.5; r<span class="elsevierStyleSup">2</span> = 0.83. In addition, an abrupt enrichment in δ<span class="elsevierStyleSup">18</span>Oand δD occurs at altitudes between 1,000 to 1,400 meters in the study area.This is may becaused by local topographic condition and/or an isotopic shift caused by tropical storms. But because this anomaly is located in an area with frequent fog, it may instead be caused by condensation processes under equilibrium isotope exchange (<a class="elsevierStyleCrossRef" href="#bib0055">Gonfiantini <span class="elsevierStyleItalic">et al</span>., 2001</a>). A third possible cause is plant evapotranspiration which, in tropical areas, may form mists and clouds that are isotopically depleted.</p><elsevierMultimedia ident="fig0025"></elsevierMultimedia><p id="par0075" class="elsevierStylePara elsevierViewall">The temporal isotopic variation at 3 sites located at different altitudes (Veracruz, Xalapa and Cofre de Perote) shows that during years characterized by heavy rainfall, the isotope composition is lighter (<a class="elsevierStyleCrossRef" href="#fig0030">figure 6</a>). This is particularly evident during 2010, the wettest year of the 6 year study due to a large number of storms in the Atlantic Ocean (five hurricanes, 13 tropical storms and one tropical depression; <a class="elsevierStyleCrossRef" href="#bib0015">CONAGUA, 2012</a>). This correlation between precipitation and isotopic depletion may be caused by cloud formation higher in the atmosphere during larger storms (<a class="elsevierStyleCrossRef" href="#bib0035">Dansgaard, 1964</a>).</p><elsevierMultimedia ident="fig0030"></elsevierMultimedia></span><span id="sec0025" class="elsevierStyleSection elsevierViewall"><span class="elsevierStyleSectionTitle" id="sect0045">Concluding Remarks</span><p id="par0080" class="elsevierStylePara elsevierViewall">The stable isotope composition of rainy season precipitation has been characterized for the windward (Atlantic) side of the Sierra Madre Oriental, located on eastern flank of the Mexican Volcanic Belt in the State of Veracruz. The cumulative rainfall during the rainy season from May to October accounts for over the 80% of the total annual rainfall in the study area. Average isotopic values were measured in 44 cumulative precipitation samples collected during the rainy seasons of 2007 through 2012 collected at altitudes ranging from 8 to 4220 masl. The results are comparable with previously reported annual weighted averages for the Port of Veracruz (GNIP, 2012), supporting the methodology of focusing only on sample collection during the rainy season. A local meteoric water line of δD= 7.44 δ<span class="elsevierStyleSup">18</span>O + 7.3 was determined from these isotopic results. In addition, calculated vertical isotopic gradients for δ<span class="elsevierStyleSup">18</span>O and δD are - 2.1 ‰ km<span class="elsevierStyleSup">-1</span> and - 15.3 ‰ km<span class="elsevierStyleSup">-1</span> respectively. These gradients are consistent with previously reported gradients in Veracruz and at similar latitudes elsewhere in central Mexico. A mid-altitude isotopic anomaly near Xalapa, however, indicates that this isotopic gradient may cause an under estimation or over estimation of the calculated altitude of precipitation in particular cases, depending on local orographic precipitation and/or extreme weather conditions. The results of this study can be utilized to improve the understanding of groundwater recharge processes. In particular, this information can be used to evaluate the source altitude of precipitation recharging aquifers in this part of eastern Mexico.</p></span></span>" "textoCompletoSecciones" => array:1 [ "secciones" => array:11 [ 0 => array:3 [ "identificador" => "xres551704" "titulo" => "Resumen" "secciones" => array:1 [ 0 => array:1 [ "identificador" => "abst0005" ] ] ] 1 => array:2 [ "identificador" => "xpalclavsec569118" "titulo" => "Palabras clave" ] 2 => array:3 [ "identificador" => "xres551705" "titulo" => "Abstract" "secciones" => array:1 [ 0 => array:1 [ "identificador" => "abst0010" ] ] ] 3 => array:2 [ "identificador" => "xpalclavsec569119" "titulo" => "Keywords" ] 4 => array:2 [ "identificador" => "sec0005" "titulo" => "Introduction" ] 5 => array:2 [ "identificador" => "sec0010" "titulo" => "Study area" ] 6 => array:2 [ "identificador" => "sec0015" "titulo" => "Methodology" ] 7 => array:2 [ "identificador" => "sec0020" "titulo" => "Results and discussion" ] 8 => array:2 [ "identificador" => "sec0025" "titulo" => "Concluding Remarks" ] 9 => array:2 [ "identificador" => "xack186045" "titulo" => "Acknowledgment" ] 10 => array:1 [ "titulo" => "References" ] ] ] "pdfFichero" => "main.pdf" "tienePdf" => true "fechaRecibido" => "2014-04-01" "fechaAceptado" => "2015-01-13" "PalabrasClave" => array:2 [ "es" => array:1 [ 0 => array:4 [ "clase" => "keyword" "titulo" => "Palabras clave" "identificador" => "xpalclavsec569118" "palabras" => array:5 [ 0 => "Isótopos estables" 1 => "gradiente isotópico" 2 => "Veracruz México" 3 => "composición isotópica" 4 => "precipitación." ] ] ] "en" => array:1 [ 0 => array:4 [ "clase" => "keyword" "titulo" => "Keywords" "identificador" => "xpalclavsec569119" "palabras" => array:6 [ 0 => "Stable isotopes" 1 => "isotopic gradient" 2 => "Veracruz" 3 => "México" 4 => "isotopic composition" 5 => "precipitation." ] ] ] ] "tieneResumen" => true "resumen" => array:2 [ "es" => array:2 [ "titulo" => "Resumen" "resumen" => "<span id="abst0005" class="elsevierStyleSection elsevierViewall"><p id="spar0005" class="elsevierStyleSimplePara elsevierViewall">Se caracterizó la composición isotópica δ<span class="elsevierStyleSup">18</span>O ‰ y δD‰, del agua meteórica en el flanco oriental de la Faja Volcánica Transmexicana, sobre un transecto de 90<span class="elsevierStyleHsp" style=""></span>km que parte de nivel de mar hasta 4220 msnm. Las muestras de lluvia fueron colectadas, durante los años 2007 a 2012, en temporada de lluvia (mayo a Octubre). Se obtuvo una Línea Meteórica Local (LML) bajo una regresión lineal la cual queda descrita por δD = 7.4 δ<span class="elsevierStyleSup">18</span>O + 7.3, R<span class="elsevierStyleSup">2</span> = 0.99. Esta línea tiende a separarse de la Línea Meteórica Mundial (LMM) donde la precipitación ocurre a altitudes mayores a 3000 msnm, debido a un enriquecimiento en Deuterio. El resultado obtenido en esta investigación fue comparado con los datos isotópicos, colectados en el Puerto de Veracruz, extraídos de la base de datos de la Red Mundial de Isótopos en Precipitación. El gradiente altitudinal de δ<span class="elsevierStyleSup">18</span>O, es descrito por una regresión lineal δ<span class="elsevierStyleSup">18</span>O = - 2.1 (Z km) - 5.56, R<span class="elsevierStyleSup">2</span> = 0.86, la cual implica un gradiente vertical de -0.21 ‰/ 100m. Finalmente, el registro isotópico en agua meteórica durante los años de observación en esta investigación muestra un enriquecimiento en δ<span class="elsevierStyleSup">18</span>O y δD a una altitud aproximada de 1400 msnm, probablemente influenciado por la topografía y/o relacionado por efectos isotópicos de tormentas tropicales, típicas de estas latitudes. Esta caracterización aumentará la comprensión de importantes procesos hidrológicos y proporcionará la base para futuras investigaciones hidrológicas.</p></span>" ] "en" => array:2 [ "titulo" => "Abstract" "resumen" => "<span id="abst0010" class="elsevierStyleSection elsevierViewall"><p id="spar0010" class="elsevierStyleSimplePara elsevierViewall">The isotopic composition (δ<span class="elsevierStyleSup">18</span>O, δD‰) of precipitation in the windward side of the Sierra Madre Oriental on the eastern flank of the Mexican Volcanic Belt was characterized along a 90<span class="elsevierStyleHsp" style=""></span>km transect from sea level up to an altitude of 4220 meters. Rain samples were collected during the rainy season (May through October) from 2007 through 2012. The Local Meteoric Water Line (LMWL), determined with linear regression of isotope results, is δD = 7.44 δ<span class="elsevierStyleSup">18</span>O + 7.3, R<span class="elsevierStyleSup">2</span> = 0.99. This line departs from the Global Meteoric Water Line (GMWL) for precipitation at altitudes greater than 3000 masl due to deuterium enrichment processes. The results obtained in this research were compared with isotopic data of the Global Network of Isotopes Precipitation (GNIP) data base from the port of Veracruz. The altitude (Z) gradient of δ<span class="elsevierStyleSup">18</span>O was also determined by the linear regression of precipitation data, resulting in the relation δ<span class="elsevierStyleSup">18</span>O = -2.1Z - 5.56, R<span class="elsevierStyleSup">2</span> = 0.86, where Z is altitude in kilometers.This implies a δ<span class="elsevierStyleSup">18</span>O vertical gradient of -0.21 ‰/ 100 m, which falls within the normal range described in the literature for tropical areas. Finally, the isotopic record of meteoric waters during the years of observation shows anomalous enrichment in δ<span class="elsevierStyleSup">18</span>O and δD at an altitude of about 1400 m, probably influenced by the local topography and/or an isotope effect related to tropical storms typical of this latitude. This characterization will increase the understanding of important hydrological processes and will provide a foundation for future hydrological research.</p></span>" ] ] "multimedia" => array:7 [ 0 => array:7 [ "identificador" => "fig0005" "etiqueta" => "Figure 1" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr1.jpeg" "Alto" => 1188 "Ancho" => 1872 "Tamanyo" => 225207 ] ] "descripcion" => array:1 [ "en" => "<p id="spar0020" class="elsevierStyleSimplePara elsevierViewall">Geographyc map and topographic section of the up wind Sierra Madre Oriental study area from Cofre de Perote (A) to Veracruz (A’); location of precipitation stations shown by black triangles.</p>" ] ] 1 => array:7 [ "identificador" => "fig0010" "etiqueta" => "Figure 2" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr2.jpeg" "Alto" => 1387 "Ancho" => 1851 "Tamanyo" => 293907 ] ] "descripcion" => array:1 [ "en" => "<p id="spar0025" class="elsevierStyleSimplePara elsevierViewall">Displays climograms located in the town of Tembladeras, Xalapa and Veracruz, located at 3000 masl., 1400 masl, and sea level, respectively (modified from <a class="elsevierStyleCrossRef" href="#bib0110">Tejeda <span class="elsevierStyleItalic">et al</span>., 1989</a>). Precipitation at the Port of Veracruz and at Tembladeras is concentrated in the months of June to September, with magnitudes as large as 350<span class="elsevierStyleHsp" style=""></span>mm. In contrast, the majority of rainfall in Xalapa is distributed over the months of May to October, with monthly averages less than 250<span class="elsevierStyleHsp" style=""></span>mm.</p>" ] ] 2 => array:7 [ "identificador" => "fig0015" "etiqueta" => "Figure 3" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr3.jpeg" "Alto" => 872 "Ancho" => 1376 "Tamanyo" => 115560 ] ] "descripcion" => array:1 [ "en" => "<p id="spar0030" class="elsevierStyleSimplePara elsevierViewall">Monthly arithmetic average of δ<span class="elsevierStyleSup">18</span>O‰ and monthly precipitation average (mm) accumulated from 1962 to 1988. Source: GNIP, IAEA, <span class="elsevierStyleInterRef" id="intr0005" href="http://www-naweb.iaea.org/napc/ih/IHS_resources_gnip">http://www-naweb.iaea.org/napc/ih/IHS_resources_gnip</span>. html.</p>" ] ] 3 => array:7 [ "identificador" => "fig0020" "etiqueta" => "Figure 4" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr4.jpeg" "Alto" => 969 "Ancho" => 1479 "Tamanyo" => 130643 ] ] "descripcion" => array:1 [ "en" => "<p id="spar0035" class="elsevierStyleSimplePara elsevierViewall">δ<span class="elsevierStyleSup">18</span>O‰ and δ<span class="elsevierStyleSup">2</span>H‰ of precipitation samples collected 2007 through 2012 and the resulting linear regression (Local Meteoric Water Line, LML) for the upwind Sierra Madre Oriental study area, compared with the Global Meteoric Line (GML).</p>" ] ] 4 => array:7 [ "identificador" => "fig0025" "etiqueta" => "Figure 5" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr5.jpeg" "Alto" => 1702 "Ancho" => 1207 "Tamanyo" => 171220 ] ] "descripcion" => array:1 [ "en" => "<p id="spar0040" class="elsevierStyleSimplePara elsevierViewall">Vertical isotopic gradient of (a) δ<span class="elsevierStyleSup">18</span>O‰ and (b) δD during the rainy season.</p>" ] ] 5 => array:7 [ "identificador" => "fig0030" "etiqueta" => "Figure 6" "tipo" => "MULTIMEDIAFIGURA" "mostrarFloat" => true "mostrarDisplay" => false "figura" => array:1 [ 0 => array:4 [ "imagen" => "gr6.jpeg" "Alto" => 928 "Ancho" => 1448 "Tamanyo" => 82722 ] ] "descripcion" => array:1 [ "en" => "<p id="spar0045" class="elsevierStyleSimplePara elsevierViewall">Temporal behavior of δ<span class="elsevierStyleSup">18</span>O‰, for meteoric water samples from 2007 to 2012, at three different altitudes: Veracruz, Xalapa, and Cofre de Perote at 8, 1448 and 4220 masl, respectively.</p>" ] ] 6 => array:7 [ "identificador" => "tbl0005" "etiqueta" => "Table 1" "tipo" => "MULTIMEDIATABLA" "mostrarFloat" => true "mostrarDisplay" => false "tabla" => array:1 [ "tablatextoimagen" => array:1 [ 0 => array:2 [ "tabla" => array:1 [ 0 => """ <table border="0" frame="\n \t\t\t\t\tvoid\n \t\t\t\t" class=""><thead title="thead"><tr title="table-row"><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">Name</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">Altitude</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">2007</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">2008</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">2009</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">2010</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">2011</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">2012</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th></tr><tr title="table-row"><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">(m a.s.l.)</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col">δ<span class="elsevierStyleSup"><span class="elsevierStyleBold">18</span></span><span class="elsevierStyleBold">O‰</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">δ</span><span class="elsevierStyleSup"><span class="elsevierStyleBold">2</span></span><span class="elsevierStyleBold">H‰</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">d-</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">δ</span><span class="elsevierStyleSup"><span class="elsevierStyleBold">18</span></span><span class="elsevierStyleBold">O‰</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">δ</span><span class="elsevierStyleSup"><span class="elsevierStyleBold">2</span></span><span class="elsevierStyleBold">H‰</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">d-</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">δ</span><span class="elsevierStyleSup"><span class="elsevierStyleBold">18</span></span><span class="elsevierStyleBold">O‰</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">δ</span><span class="elsevierStyleSup"><span class="elsevierStyleBold">2</span></span><span class="elsevierStyleBold">H‰</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">d-</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">δ</span><span class="elsevierStyleSup"><span class="elsevierStyleBold">18</span></span><span class="elsevierStyleBold">O‰</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">δ</span><span class="elsevierStyleSup"><span class="elsevierStyleBold">2</span></span><span class="elsevierStyleBold">H‰</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">d-</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">δ</span><span class="elsevierStyleSup"><span class="elsevierStyleBold">18</span></span><span class="elsevierStyleBold">O‰</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">δ</span><span class="elsevierStyleSup"><span class="elsevierStyleBold">2</span></span><span class="elsevierStyleBold">H‰</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">d-</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">δ</span><span class="elsevierStyleSup"><span class="elsevierStyleBold">18</span></span><span class="elsevierStyleBold">O‰</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">δ</span><span class="elsevierStyleSup"><span class="elsevierStyleBold">2</span></span><span class="elsevierStyleBold">H‰</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">d-</span> \t\t\t\t\t\t\n \t\t\t\t</th></tr><tr title="table-row"><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">excess</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">excess</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">excess</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">excess</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">excess</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col"><span class="elsevierStyleBold">excess</span> \t\t\t\t\t\t\n \t\t\t\t</th></tr><tr title="table-row"><th class="td" title="table-head " align="" valign="top" scope="col" style="border-bottom: 2px solid black"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col" style="border-bottom: 2px solid black"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col" style="border-bottom: 2px solid black"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col" style="border-bottom: 2px solid black"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col" style="border-bottom: 2px solid black"><span class="elsevierStyleBold">[‰]</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col" style="border-bottom: 2px solid black"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col" style="border-bottom: 2px solid black"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col" style="border-bottom: 2px solid black"><span class="elsevierStyleBold">[‰]</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col" style="border-bottom: 2px solid black"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col" style="border-bottom: 2px solid black"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col" style="border-bottom: 2px solid black"><span class="elsevierStyleBold">[‰]</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col" style="border-bottom: 2px solid black"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col" style="border-bottom: 2px solid black"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col" style="border-bottom: 2px solid black"><span class="elsevierStyleBold">[‰]</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col" style="border-bottom: 2px solid black"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col" style="border-bottom: 2px solid black"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col" style="border-bottom: 2px solid black"><span class="elsevierStyleBold">[‰]</span> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col" style="border-bottom: 2px solid black"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="" valign="top" scope="col" style="border-bottom: 2px solid black"> \t\t\t\t\t\t\n \t\t\t\t</th><th class="td" title="table-head " align="left" valign="top" scope="col" style="border-bottom: 2px solid black"><span class="elsevierStyleBold">[‰]</span> \t\t\t\t\t\t\n \t\t\t\t</th></tr></thead><tbody title="tbody"><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Cofre de Perote \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">4220 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-15.3 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-106.3 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">15.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-14.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-101.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">17.4 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-12.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-87.2 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">15.7 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-14.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-102.3 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">16.8 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-13.4 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-90.2 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">17.4 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-14.6 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-101.8 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">15.2 \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Tembladeras \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">3081 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-13 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-90.8 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">13.3 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-12.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-87.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">12.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Pocitos \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">2464 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-9.1 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-57.7 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">15.2 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Las Vigas \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">2442 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-12.2 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-84.6 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">13.0 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Loma de Tablas \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">2275 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-8.7 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-53.7 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">15.7 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-9.6 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-63.2 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">13.8 \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Ixhuacán \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">1690 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-6.4 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-44.0 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">7.0 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Xalapa \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">1448 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-7.3 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-45.4 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">13.4 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-8.0 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-50.4 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">13.7 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-9.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-65.4 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">10.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-5.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-33.1 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">14.4 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-7.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-50.3 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">13.3 \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Totutla \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">1374 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-10.1 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-67.4 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">13.0 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Xico \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">1354 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-7.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-50.4 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">13.0 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Coatepec \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">1189 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-6.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-43.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">11.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Alto Lucero \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">1078 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-7.3 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-47.4 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">11.1 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-8.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-56.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">10.7 \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Dos Ríos \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">950 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-8.6 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-57.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">11.0 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-63.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">8.1 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Loma de Rogel \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">710 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-9.2 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-65 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">8.2 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">La Reforma \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">691 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-6.7 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-42.2 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">11.7 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-7.3 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-48.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">9.8 \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Cerro Gordo \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">601 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-7.7 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-51.3 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">10.4 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Carrizal \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">441 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-6.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-46.3 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">8.8 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">La Cumbre \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">375 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-5.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-36.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">10.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-8.2 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-55.1 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">10.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Actopan \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">268 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-5.4 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-34.3 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">8.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-7.4 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-48.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">10.1 \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Rinconada \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">263 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-7.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-51.1 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">8.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Buena Vista \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">199 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-6.8 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-42.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">11.6 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Tamarindo \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">140 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-5.7 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-34.3 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">11.6 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Paso de Ovejas \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">30 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-6.6 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-42.1 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">10.7 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">Veracruz \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">8 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-4.8 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-25.7 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">12.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-3.3 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-17.2 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">9.3 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-6.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-42.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">9.4 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-4.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-24.0 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">12.0 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-4.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-28.9 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">10.1 \t\t\t\t\t\t\n \t\t\t\t</td></tr><tr title="table-row"><td class="td" title="table-entry " align="left" valign="top">La Antigua \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">8 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-7.3 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">-48.6 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="left" valign="top">9.5 \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td><td class="td" title="table-entry " align="" valign="top"> \t\t\t\t\t\t\n \t\t\t\t</td></tr></tbody></table> """ ] "imagenFichero" => array:1 [ 0 => "xTab890456.png" ] ] ] ] "descripcion" => array:1 [ "en" => "<p id="spar0015" class="elsevierStyleSimplePara elsevierViewall">Stable isotope ratios δ<span class="elsevierStyleSup">18</span>O‰ and δD‰ vs V-SMOW of accumulated rainfall in the upwind Sierra Madre Oriental study area, during the rainy seasons from 2007 through 2012.</p>" ] 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Special thanks to all the students and people from different communities who participated in the placement and sampling of precipitationcollectors.</p>" "vista" => "all" ] ] ] "idiomaDefecto" => "en" "url" => "/00167169/0000005400000003/v2_201509120041/S0016716915000240/v2_201509120041/en/main.assets" "Apartado" => array:4 [ "identificador" => "40021" "tipo" => "SECCION" "en" => array:2 [ "titulo" => "Articles" "idiomaDefecto" => true ] "idiomaDefecto" => "en" ] "PDF" => "https://static.elsevier.es/multimedia/00167169/0000005400000003/v2_201509120041/S0016716915000240/v2_201509120041/en/main.pdf?idApp=UINPBA00004N&text.app=https://www.elsevier.es/" "EPUB" => "https://multimedia.elsevier.es/PublicationsMultimediaV1/item/epub/S0016716915000240?idApp=UINPBA00004N" ]
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2024 October | 33 | 14 | 47 |
2024 September | 49 | 6 | 55 |
2024 August | 27 | 7 | 34 |
2024 July | 14 | 4 | 18 |
2024 June | 17 | 2 | 19 |
2024 May | 22 | 7 | 29 |
2024 April | 21 | 6 | 27 |
2024 March | 32 | 9 | 41 |
2024 February | 41 | 5 | 46 |
2024 January | 23 | 4 | 27 |
2023 December | 21 | 9 | 30 |
2023 November | 36 | 7 | 43 |
2023 October | 45 | 7 | 52 |
2023 September | 41 | 7 | 48 |
2023 August | 15 | 3 | 18 |
2023 July | 24 | 5 | 29 |
2023 June | 16 | 4 | 20 |
2023 May | 56 | 4 | 60 |
2023 April | 27 | 0 | 27 |
2023 March | 22 | 6 | 28 |
2023 February | 27 | 7 | 34 |
2023 January | 38 | 7 | 45 |
2022 December | 31 | 9 | 40 |
2022 November | 30 | 18 | 48 |
2022 October | 31 | 19 | 50 |
2022 September | 28 | 12 | 40 |
2022 August | 29 | 7 | 36 |
2022 July | 22 | 9 | 31 |
2022 June | 32 | 14 | 46 |
2022 May | 27 | 8 | 35 |
2022 April | 26 | 9 | 35 |
2022 March | 39 | 16 | 55 |
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2022 January | 42 | 10 | 52 |
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2021 October | 29 | 18 | 47 |
2021 September | 17 | 16 | 33 |
2021 August | 38 | 6 | 44 |
2021 July | 26 | 15 | 41 |
2021 June | 36 | 9 | 45 |
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2021 March | 52 | 20 | 72 |
2021 February | 22 | 14 | 36 |
2021 January | 31 | 10 | 41 |
2020 December | 26 | 9 | 35 |
2020 November | 33 | 4 | 37 |
2020 October | 32 | 7 | 39 |
2020 September | 33 | 13 | 46 |
2020 August | 30 | 11 | 41 |
2020 July | 23 | 9 | 32 |
2020 June | 24 | 2 | 26 |
2020 May | 33 | 13 | 46 |
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2020 March | 32 | 7 | 39 |
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2019 December | 29 | 11 | 40 |
2019 November | 28 | 8 | 36 |
2019 October | 36 | 6 | 42 |
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2019 August | 26 | 8 | 34 |
2019 July | 32 | 16 | 48 |
2019 June | 66 | 18 | 84 |
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2019 March | 22 | 3 | 25 |
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2019 January | 14 | 6 | 20 |
2018 December | 12 | 1 | 13 |
2018 November | 26 | 5 | 31 |
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2018 September | 17 | 7 | 24 |
2018 August | 23 | 6 | 29 |
2018 July | 15 | 6 | 21 |
2018 June | 24 | 6 | 30 |
2018 May | 27 | 8 | 35 |
2018 April | 20 | 6 | 26 |
2018 March | 17 | 2 | 19 |
2018 February | 22 | 8 | 30 |
2018 January | 28 | 5 | 33 |
2017 December | 18 | 1 | 19 |
2017 November | 22 | 4 | 26 |
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2017 September | 21 | 9 | 30 |
2017 August | 19 | 10 | 29 |
2017 July | 9 | 4 | 13 |
2017 June | 54 | 3 | 57 |
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2017 April | 28 | 3 | 31 |
2017 March | 25 | 35 | 60 |
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2017 January | 14 | 1 | 15 |
2016 December | 15 | 8 | 23 |
2016 November | 28 | 7 | 35 |
2016 October | 28 | 8 | 36 |
2016 September | 32 | 7 | 39 |
2016 August | 30 | 2 | 32 |
2016 July | 25 | 1 | 26 |
2016 June | 24 | 16 | 40 |
2016 May | 22 | 18 | 40 |
2016 April | 20 | 22 | 42 |
2016 March | 28 | 19 | 47 |
2016 February | 24 | 21 | 45 |
2016 January | 22 | 16 | 38 |
2015 December | 22 | 17 | 39 |
2015 November | 16 | 18 | 34 |
2015 October | 23 | 22 | 45 |
2015 September | 10 | 7 | 17 |