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vertically polarized microwave radiation at 12 channels and six frequencies ranging from 6.9 to 89.0 GHz. Its observations at moderately low frequencies are very sensitive to land water in various forms, such as soil moisture, vegetation water content, and snow, and are little affected by atmosphere conditions. AMSR-E was launched in June 2002 and functioned well until October 2011. During this period, TGD experienced two impounding stages: the initial stage of impoundment with a water level increasing
vertically polarized microwave radiation at 12 channels and six frequencies ranging from 6.9 to 89.0 GHz. Its observations at moderately low frequencies are very sensitive to land water in various forms, such as soil moisture, vegetation water content, and snow, and are little affected by atmosphere conditions. AMSR-E was launched in June 2002 and functioned well until October 2011. During this period, TGD experienced two impounding stages: the initial stage of impoundment with a water level increasing
dataset that can be developed from a hydrologic model, dam break model, or observations. The source location of the input hydrograph must be defined. When simulating floods in urban areas, Flood2D-GPU can represent the geometric features such as levees on the DEM by GIS-based preprocessing. Figure 5 presents a schematic view of artificially “burning” (i.e., after GIS-based preprocessing) the levees along the river ( Figure 5b ) to realistically represent the floods in the floodplain. To represent
dataset that can be developed from a hydrologic model, dam break model, or observations. The source location of the input hydrograph must be defined. When simulating floods in urban areas, Flood2D-GPU can represent the geometric features such as levees on the DEM by GIS-based preprocessing. Figure 5 presents a schematic view of artificially “burning” (i.e., after GIS-based preprocessing) the levees along the river ( Figure 5b ) to realistically represent the floods in the floodplain. To represent
