Simulating hydrologic and hydraulic processes throughout the Amazon River Basin

被引:120
作者
Beighley, R. E. [1 ]
Eggert, K. G. [2 ,3 ]
Dunne, T. [4 ]
He, Y. [1 ]
Gummadi, V. [1 ]
Verdin, K. L. [5 ]
机构
[1] San Diego State Univ, San Diego, CA 92182 USA
[2] Univ Calif Santa Barbara, Inst Computat Earth Syst Sci, Santa Barbara, CA 93106 USA
[3] Los Alamos Natl Lab, Div Theoret, Los Alamos, NM USA
[4] Univ Calif Santa Barbara, Donald Bren Sch Environm Sci & Management, Santa Barbara, CA 93106 USA
[5] US Geol Survey, Earth Resources Observat & Sci Ctr, Sioux Falls, SD USA
关键词
Amazon Basin; flood routing; hydrologic modelling; WATER STORAGE; VEGETATION; SOILS; MODEL;
D O I
10.1002/hyp.7252
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Presented here is a model framework based on a land surface topography that can be represented with various degrees of resolution and capable of providing representative channel/floodplain hydraulic characteristics on a daily to hourly scale. The framework integrates two models: (1) a water balance model (WBM) for the vertical fluxes and stores of water in and through the canopy and soil layers based oil the conservation of mass and energy, and (2) a routing model for the horizontal routing of surface and subsurface runoff and channel and floodplain waters based oil kinematic and diffusion wave methodologies. The WBM is driven by satellite-derived precipitation (TRMM_3B42) and air temperature (MOD08_M3). The model's use of an irregular computational grid is intended to facilitate parallel processing for applications to continental and global scales. Results are presented for the Amazon Basin over the period Jan 2001 through Dec 2005. The model is shown to capture annual runoff totals, annual peaks, seasonal patterns, and daily fluctuations over a range of spatial scales (>1,000 to <4.7M km(2)). For the period Of Study, results suggest basin-wide total water storage changes in the Amazon vary by approximately +/-5 to 10 cm, and the fractional components accounting for these changes are: root zone soil moisture (20%), Subsurface water being routed laterally to channels (40%) and channel/floodplain discharge (40%). Annual variability in monthly water storage changes by +/-2.5 cm is likely due to 0.5 to 1 month variability in the arrival of significant rainfall periods throughout the basin. Copyright (C) 2009 John Wiley & Sons, Ltd.
引用
收藏
页码:1221 / 1235
页数:15
相关论文
共 68 条
  • [1] Allen R. G., 1998, FAO Irrigation and Drainage Paper
  • [2] Tracking fresh water from space
    Alsdorf, DE
    Lettenmaier, DP
    [J]. SCIENCE, 2003, 301 (5639) : 1491 - +
  • [3] Interferometric radar measurements of water level changes on the Amazon flood plain
    Alsdorf, DE
    Melack, JM
    Dunne, T
    Mertes, LAK
    Hess, LL
    Smith, LC
    [J]. NATURE, 2000, 404 (6774) : 174 - 177
  • [4] Measuring surface water from space
    Alsdorf, Douglas E.
    Rodriguez, Ernesto
    Lettenmaier, Dennis P.
    [J]. REVIEWS OF GEOPHYSICS, 2007, 45 (02)
  • [5] Arcement G.J., 1989, United States Geological Survey Water-Supply Paper 2339, DOI DOI 10.3133/WSP2339
  • [6] Bates PD, 1997, HYDROL PROCESS, V11, P1777, DOI 10.1002/(SICI)1099-1085(199711)11:14<1777::AID-HYP543>3.0.CO
  • [7] 2-E
  • [8] Adjusting measured peak discharges from an urbanizing watershed to reflect a stationary land use signal
    Beighley, RE
    Moglen, GE
    [J]. WATER RESOURCES RESEARCH, 2003, 39 (04) : WES41 - WES411
  • [9] How far can we go in distributed hydrological modelling?
    Beven, K
    [J]. HYDROLOGY AND EARTH SYSTEM SCIENCES, 2001, 5 (01) : 1 - 12
  • [10] BLOSCHL G, 1995, HYDROL PROCESS, V9, P251, DOI 10.1002/hyp.3360090305