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Tonantzin Tarin,Enrico A. Yepez,Jaime Garatuza-Payan,Julio C. Rodriguez,Luis A. Méndez-Barroso,Christopher J. Watts,Enrique R. Vivoni
Pág. 319 - 335
Evapotranspiration is the second largest component of the hydrological cycle after rainfall precipitation in semiarid regions such as northwestern Mexico. In this study, we partitioned the evapotranspiration (ET) flux using stable isotopes of water in th...
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Rodrigo Vargas,Enrico Yépez,José Luis Andrade,Gregorio Ángeles,Tulio Arredondo,Alejandro Castellanos,Josué Delgado,Jaime Garatuza-Payan,Eugenia González del Castillo,Walter Oechel,Arturo Sánchez-Azofeifa,Erik Velasco,Enrique Vivoni,Christopher Watts
Understanding ecosystem processes from a functional point of view is essential to study relationships among climate variability, biogeochemical cycles, and surface-atmosphere interactions. Increasingly during the last decades, the eddy covariance (EC) me...
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