A Quantitative Calculation Method of Sea Surface Stress Induced by Rainfall
A quantitative calculation and stress technology, which is applied in design optimization/simulation, instrumentation, electrical digital data processing, etc., can solve problems such as the quantitative calculation method of rainfall-induced sea surface stress that has not yet been researched, and achieve deepening cognition and understanding, physical well-defined effects
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Embodiment 1
[0038] A method for quantitatively calculating rainfall-induced sea surface stress, specifically comprising the following steps:
[0039] (1) Collect observed or simulated wind speed data and rainfall rates;
[0040] (2) According to Calculate the boundary layer height h, and the height where the minimum value ε is located is the boundary layer height h;
[0041] (3) According to the force analysis of gravity and air resistance in the falling process of raindrops in the boundary layer, the three-dimensional motion model of raindrops with particle size D is established as follows:
[0042]
[0043] in,
[0044]
[0045] (4) Discretize the numerical value of the raindrop three-dimensional motion model equation, and obtain the numerical solution of the raindrop motion velocity:
[0046]
[0047] (5) Substituting the initial value condition in the discrete equation in the step (4), when t=0, satisfy following condition: z=h, u a = u R , v a =v R ,w T =w R ;
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Embodiment 2
[0053] In this embodiment, the calculation method of the rainfall-induced sea surface stress value is the same as that of Embodiment 1: that is, the scheme provided in Embodiment 1 is used to calculate the rainfall-induced sea surface stress value through TRMM and ERA5 data;
[0054] Such as Figure 4 As shown, this embodiment also provides the global distribution of the ratio of rainfall-induced sea surface stress to wind stress. The ratio of rainfall-induced sea surface stress to wind stress is calculated according to the following formula:
[0055]
[0056] Among them, ρ a is the atmospheric density, C d is the sea surface drag coefficient, u 10 is the wind speed at a height of 10 meters.
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