Calibration of Land-Use-Dependent Evaporation Parameters in Distributed Hydrological Models Using MODIS Evaporation Time Series Data

被引:1
|
作者
Casper, Markus C. [1 ]
Salm, Zoe [1 ]
Gronz, Oliver [1 ]
Hutengs, Christopher [2 ,3 ]
Mohajerani, Hadis [1 ]
Vohland, Michael [2 ,3 ]
机构
[1] Univ Trier, Phys Geog, D-54286 Trier, Germany
[2] Univ Leipzig, Inst Geog Geoinformat & Remote Sensing, D-04109 Leipzig, Germany
[3] Univ Leipzig, Remote Sensing Ctr Earth Syst Res, D-04109 Leipzig, Germany
关键词
spatio-temporal ETa patterns; MODIS ETa; vegetation-related evaporation parameters; land-use-specific manual ETa calibration; LANDSAT-based validation; spatial efficiency metric; PEDOTRANSFER FUNCTIONS; HYDRAULIC-PROPERTIES; SURFACE-RESISTANCE; CANOPY RESISTANCE; EVAPOTRANSPIRATION; PERFORMANCE; METHODOLOGY; FEEDBACKS; ARCHIVE; SOILS;
D O I
10.3390/hydrology10120216
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
The land-use-specific calibration of evapotranspiration parameters in hydrologic modeling is challenging due to the lack of appropriate reference data. We present a MODIS-based calibration approach of vegetation-related evaporation parameters for two mesoscale catchments in western Germany with the physically based distributed hydrological model WaSiM-ETH. Time series of land-use-specific actual evapotranspiration (ETa) patterns were generated from MOD16A2 evapotranspiration and CORINE land-cover data from homogeneous image pixels for the major land-cover types in the region. Manual calibration was then carried out for 1D single-cell models, each representing a specific land-use type based on aggregated 11-year mean ETa values using SKout and PBIAS as objective functions (SKout > 0.8, |PBIAS| < 5%). The spatio-temporal evaluation on the catchment scale was conducted by comparing the simulated ETa pattern to six daily ETa grids derived from LANDSAT data. The results show a clear overall improvement in the SPAEF (spatial efficiency metric) for most land-use types, with some deficiencies for two scenes in spring and late summer due to phenological variation and a particularly dry hydrological system state, respectively. The presented method demonstrates a significant improvement in the simulation of ETa regarding both time and spatial scale.
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页数:23
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