Case Studies of a MODIS-Based Potential Evapotranspiration Input to the Sacramento Soil Moisture Accounting Model

被引:11
作者
Bowman, Angela L. [1 ]
Franz, Kristie J. [1 ]
Hogue, Terri S. [2 ]
机构
[1] Iowa State Univ, Dept Geol & Atmospher Sci, Ames, IA 50011 USA
[2] Colorado Sch Mines, Dept Civil & Environm Engn, Golden, CO 80401 USA
基金
美国国家航空航天局;
关键词
RAINFALL-RUNOFF MODEL; EVAPORATION; SATELLITE;
D O I
10.1175/JHM-D-16-0214.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A satellite-based potential evapotranspiration (PET) estimate derived from Moderate Resolution Imaging Spectroradiometer (MODIS) observations was tested for input to the spatially lumped and gridded Sacramento Soil Moisture Accounting (SAC-SMA) model. The 15 forecast points within the National Weather Service (NWS) North Central River Forecast Center (NCRFC) forecasting region were the basis for this analysis. Through a series of case studies, the MODIS-derived PET estimate (M-PET) was evaluated for input to the SAC-SMA model by comparing streamfiow simulations with those from traditional SAC-SMA evapotranspiration (ET) demand. Two prior studies have evaluated the M-PET data 1) to compute new long-term average ET demand values and 2) to input a time series (i.e., daily time-varying PET) to the NWS Hydrology Laboratory Research Distributed Hydrologic Model (HL-RDHM), a spatially distributed version of the SAC-SMA model. This current paper presents results from a third test in which the M-PET time series is input to the lumped SAC-SMA model. In all cases, evaluation is between the M-PET data and the long-term average values used by the NWS. Similar to prior studies, results of the current analysis are mixed with improved model evaluation statistics for 4 of 15 basins tested. Of the three cases, using the time-varying M-PET as input to the distributed SAC-SMA model led to the most promising results, with model simulations that are at least as good as those when using the SAC-SMA ET demand. Analyses of the model-simulated ET suggest that the time-varying M-PET input may produce a more physically realistic representation of ET processes in both the lumped and distributed versions of the SAC-SMA model.
引用
收藏
页码:151 / 158
页数:8
相关论文
共 24 条
[1]  
Anderson E., 2002, CALIBRATION CONCEPTU
[2]  
[Anonymous], 33 NOAA NWS
[3]   ASSESSING SATELLITE AND GROUND-BASED POTENTIAL EVAPOTRANSPIRATION FOR HYDROLOGIC APPLICATIONS IN THE COLORADO RIVER BASIN [J].
Barik, Muhammad G. ;
Hogue, Terri S. ;
Franz, Kristie J. ;
Kinoshita, Alicia M. .
JOURNAL OF THE AMERICAN WATER RESOURCES ASSOCIATION, 2016, 52 (01) :48-66
[4]   MODIS-Based Potential Evapotranspiration Demand Curves for the Sacramento Soil Moisture Accounting Model [J].
Bowman, Angela L. ;
Franz, Kristie J. ;
Hogue, Terri S. ;
Kinoshita, Alicia M. .
JOURNAL OF HYDROLOGIC ENGINEERING, 2016, 21 (01)
[5]  
Burnash R. J. C., 1995, Computer models of watershed hydrology., P311
[6]  
Ferral R. L., 1973, GEN STREAMFLOW SIMUL
[7]   Assessment of the validity of using mean potential evaporation in computations of the long-term soil water balance [J].
Fowler, A .
JOURNAL OF HYDROLOGY, 2002, 256 (3-4) :248-263
[8]   Evaluating model performance and parameter behavior for varying levels of land surface model complexity [J].
Hogue, Terri S. ;
Bastidas, Luis A. ;
Gupta, Hoshin V. ;
Sorooshian, Soroosh .
WATER RESOURCES RESEARCH, 2006, 42 (08)
[9]  
Hogue TS, 2000, J HYDROMETEOROL, V1, P524, DOI 10.1175/1525-7541(2000)001<0524:AMACSF>2.0.CO
[10]  
2