Trend analysis of watershed-scale annual and seasonal precipitation in Northern California based on dynamically downscaled future climate projections

Author:

Ishida K.12,Ercan A.3,Trinh T.1,Jang S.4,Kavvas M. L.1,Ohara N.5,Chen Z. Q.6,Kure S.7,Dib A.1

Affiliation:

1. Hydrologic Research Laboratory, Department of Civil and Environmental Engineering, University of California, Davis. One Shields Avenue, Davis, California 95616, USA

2. Present address: Faculty of Advanced Science and Technology, Kumamoto University, 2-39-1 Kurokami, Kumamoto 860-8555, Japan

3. J. Amorocho Hydraulics Laboratory, Department of Civil and Environmental Engineering, University of California, Davis. One Shields Avenue, Davis, California 95616, USA

4. Korea Institute of Water and Environment, Korea Water Resources Corporation, Daejeon 305-730, South Korea

5. Civil and Architectural Engineering, University of Wyoming, Laramie, WY 82071, USA

6. Bay Delta Office, California Department of Water Resources, Sacramento, California 95814, USA

7. Department of Environmental Engineering, Toyama Prefectural University, Toyama 939-0398, Japan

Abstract

Abstract Impact of future climate change on watershed-scale precipitation was investigated over Northern California based on future climate projections by means of the dynamical downscaling approach. Thirteen different future climate projection realizations from two general circulation models (GCMs: ECHAM5 and CCSM3) based on four emission scenarios (SRES A1B, A1FI, A2, and B1) were dynamically downscaled to 9-km resolution grids over eight watersheds in Northern California for a period of 90 water years (2010–2100). Analysis of daily precipitation over the eight watersheds showed that precipitation values obtained from dynamical downscaling of the 1981 to 1999 control runs of ECHAM5 and CCSM3 GCMs compared well with the PRISM data. Long-term future trends of annual and seasonal basin-average precipitation were investigated. Although a large variability exists for the projected annual basin-average precipitation within each of the 13 individual realizations, there was no significant long-term trend over the eight study watersheds except for the downward trend in the A1FI scenario. On the other hand, significant upward and downward trends were detected in the seasonal basin-average precipitation except in the winter months (January, February, and March). The trend analysis results in this study indicated the importance of considering seasonal variability, scenario, and model uncertainty.

Publisher

IWA Publishing

Subject

Management, Monitoring, Policy and Law,Atmospheric Science,Water Science and Technology,Global and Planetary Change

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