首页 | 本学科首页   官方微博 | 高级检索  
     检索      


Physically based maximum precipitation estimation under future climate change conditions
Authors:Kei Ishida  M Levent Kavvas  Z Q Richard Chen  Alain Dib  Andres J Diaz  Michael L Anderson  Toan Trinh
Institution:1. Hydrologic Research Laboratory, Department of Civil and Environmental Engineering, University of California, Davis, Davis, CaliforniaPresent Address Kei Ishida, Graduate School of Science and Technology, Kumamoto University, 2‐39‐1 7 Kurokami, Kumamoto 860‐8555, Japan.;2. Hydrologic Research Laboratory, Department of Civil and Environmental Engineering, University of California, Davis, Davis, California;3. Bay Delta Office, California Department of Water Resources, Sacramento, California;4. California Department of Water Resources, Sacramento, California
Abstract:Estimation of the extreme precipitation over a target watershed under a changing climate would be necessary to design safe large hydraulic structures. For this purpose, the maximum precipitation (MP) estimation approach was applied to the American River Watershed (ARW) in Northern California under several future climate conditions over 90 water years (2010–2099). These future climate conditions were obtained using 13 future climate projections from two general circulation models (ECHAM5 and CCSM3) based on four future climate scenarios (Special Report on Emissions Scenarios: A1B, A1FI, A2, and B1). A total of 1,170 future projected severe storm events (90 years × 13 projections) were selected with respect to the 72‐hr basin‐average precipitation over the ARW. The 72‐hr basin‐average precipitation for each of the selected severe storm events was maximized over the ARW by horizontally shifting the atmospheric boundary conditions of a regional atmospheric model in order to optimize the path of the storm system that corresponded to the particular event. After maximization, the MP estimates, which are the largest precipitation depths among the maximized results, were obtained as 836.7 mm for the early half‐century period (2010–2054) and 1,056.5 mm for the late half‐century period (2055–2099).
Keywords:
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号