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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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Tiantian Xiang,Enrique R. Vivoni,David J. Gochis
Pág. 25 - 45
Land surface conditions including soil moisture and vegetation states are expected to play important roles in the development of the daytime boundary layer and the formation of convective precipitation. For areas with an in-phase seasonality of radiation...
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Francisco José Del Toro-Guerrero, Enrique R. Vivoni, Thomas Kretzschmar, Stephen Holmes Bullock Runquist and Rogelio Vázquez-González
In this research, we examined temporal variations in soil water content (?), infiltration patterns, and potential recharge at three sites with different mountain block positions in a semiarid Mediterranean climate in Baja California, Mexico: two located ...
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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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