Open AccessUnderstanding changes in water availability in the Rio Grande/Río Bravo del Norte basin under the influence of large‐scale circulation indices using the Noah land surface model
Author(s) -
Khedun C. Prakash,
Mishra Ashok K.,
Bolten John D.,
Beaudoing Hiroko K.,
Kaiser Ronald A.,
Giardino J. Richard,
Singh Vijay P.
Publication year - 2012
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2011jd016590
Subject(s) - environmental science , surface runoff , precipitation , climatology , pacific decadal oscillation , structural basin , climate change , water resources , drainage basin , el niño southern oscillation , hydrology (agriculture) , geography , geology , oceanography , meteorology , ecology , paleontology , cartography , geotechnical engineering , biology
Water availability plays an important role in the socio‐economic development of a region. It is however, subject to the influence of large‐scale circulation indices, resulting in periodic excesses and deficits. An assessment of the degree of correlation between climate indices and water availability, and the quantification of changes with respect to major climate events is important for long‐term water resources planning and management, especially in transboundary basins as it can help in conflict avoidance. In this study we first establish the correlation of the Pacific Decadal Oscillation (PDO) and El Niño‐Southern Oscillation (ENSO) with gauged precipitation in the Rio Grande basin, and then quantify the changes in water availability using runoff generated from the Noah land surface model. Both spatial and temporal variations are noted, with winter and spring being most influenced by conditions in the Pacific Ocean. Negative correlation is observed at the headwaters and positive correlation across the rest of the basin. The influence of individual ENSO events, classified using four different criteria, is also examined. El Niños (La Niñas) generally cause an increase (decrease) in runoff, but the pattern is not consistent; percentage change in water availability varies across events. Further, positive PDO enhances the effect of El Niño and dampens that of La Niña, but during neutral/transitioning PDO, La Niña dominates meteorological conditions. Long El Niños have more influence on water availability than short duration high intensity events. We also note that the percentage increase during El Niños significantly offsets the drought‐causing effect of La Niñas.