A General Hydrologic Simulation Method Using Remote Sensing Evaporation Directly
A hydrological model and remote sensing technology, applied in the field of hydrological research, can solve the problems of not forming, not considering the uncertainty of hydrological simulation, not being widely used, etc., to achieve the effect of reducing uncertainty
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Embodiment 1
[0028] This embodiment is a general hydrological simulation method that directly uses remote sensing evaporation. The process is as follows figure 1 Shown.
[0029] Taking the hydrological simulation of A watershed as an application example, according to figure 1 The shown watershed hydrological simulation method process is an example of daily-scale hydrological simulation to illustrate the hydrological simulation process of this embodiment.
Embodiment 2
[0052] This embodiment is an improvement of the first embodiment, and is a refinement of the hydrological model of the studied river basin in the first embodiment. The hydrological model of the studied basin described in this embodiment is the three-water source Xin'anjiang model or the SWAT model.
[0053] In the Xinanjiang model, the model process is as figure 2 As shown, the soil layer is divided into three layers according to the unevenness of the vertical distribution of the soil, and the three-layer evapotranspiration model is used to calculate the evapotranspiration. Calculated as follows:
[0054] WM=UM+LM+DM (2.2)
[0055] W=WU+WL+WD (2.3)
[0056] E=EU+EL+ED (2.4)
[0057] Where: W is the total tension water storage capacity, mm; WU is the upper tension water storage capacity, mm; WL is the lower tension water storage capacity, mm; WD is the deep tension water storage capacity, mm; E is the total evaporation capacity , Mm; EU is the upper layer evapotranspiration mm; EL i...
Embodiment 3
[0068] This embodiment is an improvement of the above embodiment, and is a refinement of the simulation process of the above embodiment regarding the reasonable evaporation simulation result. The simulation process with reasonable evaporation simulation results in this embodiment refers to: NSE E > 0.3 evaporation simulation process.
[0069] The value range of the Nash efficiency coefficient NSE is (-∞, 1), but the meaningful range should be positive and the closer to 1, the higher the simulation accuracy. Generally, in hydrological simulation, the condition that the simulation result is reasonable is set as NSE greater than a certain threshold (such as 0.3 here, 0.5, 0.6, etc.), and the selection of the threshold should be determined according to the specific situation.
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