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José P. Vega-Camarena, Luis Brito-Castillo, Luis F. Pineda-Martínez and Luis M. Farfán
In the warm season, El Niño/Southern Oscillation (ENSO) causes periods with more rain in Northern Mexico during its positive phase, while less rainfall is recorded in the southern regions during the negative phase. This research study evaluates the varia...
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Elena Kalmykova and Sergei Lazarev
Purpose of the study: to substantiate the prospects of using various species, varieties and forms of the genus Robinia in protective afforestation and landscaping of settlements in dry-steppe and semi-desert zones of southern Russia. It is established th...
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Corrie Monteverde, Fernando De Sales and Charles Jones
The Brazilian Amazon provides important hydrological cycle functions, including precipitation regimes that bring water to the people and environment and are critical to moisture recycling and transport, and represents an important variable for climate mo...
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Eylon Shamir, Elia M. Tapia-Villaseñor, Mary-Belle Cruz-Ayala and Sharon B. Megdal
In the parched Upper Santa Cruz River Basin (USCRB), a binational USA?Mexico basin, the water resources depend on rainfall-triggered infrequent flow events in ephemeral channels to recharge its storage-limited aquifers. In-situ data from the basin highli...
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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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Thang M. Luong, Christopher L. Castro, Truong M. Nguyen, William W. Cassell and Hsin-I Chang
A commonly noted problem in the simulation of warm season convection in the North American monsoon region has been the inability of atmospheric models at the meso-ß scales (10 s to 100 s of kilometers) to simulate organized convection, principally mesosc...
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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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Shangfeng Chen, Bin Yu, Wen Chen and Renguang Wu
The El Niño–Southern Oscillation (ENSO) is the strongest interannual air–sea coupled variability mode in the tropics, and substantially impacts the global weather and climate. Hence, it is important to improve our understanding of the ...
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The global distribution, seasonal evolution, and underlying mechanisms for the climatological midsummer drought (MSD) are investigated using a suite of relatively high spatial and temporal resolution station observations and reanalysis data with particul...
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A. VALDÉS-MANZANILLA,V. L. BARRADAS MIRANDA
This work examines Mesoscale Convective Systems (MCS) observed during the North American Monsoon Experiment (NAME), using data of deployed instruments in Northwest Mexico like weather radar, atmospheric soundings and weather satellite. Satellite infrared...
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