TECHNICAL PAPERS
Nov 15, 2011

Coupled Regional Hydroclimate Model and Its Application to the Tigris-Euphrates Basin

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Publication: Journal of Hydrologic Engineering
Volume 16, Issue 12

Abstract

To establish a basinwide water management plan for the Tigris-Euphrates (TE) watershed, it is necessary to perform rigorous water balance studies of the whole watershed—at least for critical historical drought and flood conditions and under various water resources development scenarios. Water-balance studies over the watershed require climatic and hydrologic data sets, corresponding to historical critical flood and drought periods, at fine time and spatial grid resolutions provide the necessary hydroclimatic information. The Regional Hydroclimate Model of the Tigris-Euphrates (RegHCM-TE) and the associated geographic information system (GIS) were developed to downscale large-scale atmospheric data sets over the TE watershed and to reconstruct the aforementioned climatic and land hydrologic data sets at fine spatial and time increments. In RegHCM-TE, the earth system over the TE watershed is modeled as a fully coupled system of atmospheric processes aloft coupled with the atmospheric boundary layer, land-surface processes, surface and subsurface hydrologic processes, and the interactions among the various hydrologic and atmospheric processes. The parameters of the model are estimated by using existing global and local GIS data. By using the large-scale global historical atmospheric databases as its initial and boundary conditions, RegHCM-TE has been used to reconstruct historical hydroclimate data at a grid size of 15 km over the TE watershed, for which only very sparse hydrologic observations were available. RegHCM-TE and its model validation are described in this paper.

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Information & Authors

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Go to Journal of Hydrologic Engineering
Journal of Hydrologic Engineering
Volume 16Issue 12December 2011
Pages: 1059 - 1070

History

Received: Oct 14, 2009
Accepted: Dec 28, 2010
Published online: Nov 15, 2011
Published in print: Dec 1, 2011

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Authors

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Z. Q. Richard Chen, M.ASCE [email protected]
Water Resources Engineer, California Dept. of Water Resources, 1416 9th St., Sacramento, CA 95814. E-mail: [email protected]
M. L. Kavvas, F.ASCE [email protected]
Professor, Hydrologic Research Laboratory, Dept. of Civil and Environmental Engineering, Univ. of California, Davis, CA 95616. E-mail: [email protected]
N. Ohara, A.M.ASCE [email protected]
Assistant Development Engineer, Hydrologic Research Laboratory, Dept. of Civil and Environmental Engineering, Univ. of California, Davis, CA 95616 (corresponding author). E-mail: [email protected]
M. L. Anderson, M.ASCE [email protected]
State Climatologist, California Dept. of Water Resources, 3310 El Camino Ave., Suite 200, Sacramento, CA 95821-9000. E-mail: [email protected]
J. Yoon
Associate Professor, Dept. of Environmental Engineering, Korea Univ., Jochiwon, Chungnam 339-700, South Korea.

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