Method for continously observing and determining the vertical distribution of atmospheric water vapor by using superconductive gravity
A vertically distributed and atmospheric technology, applied in the direction of measuring devices, analytical materials, climate sustainability, etc., can solve the problems of gravity without observation methods, and achieve the effect of improving time and space resolution and accuracy
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[0023] Below in conjunction with embodiment describe in detail:
[0024] 1. Step ①
[0025] The parameters of the gravity-tide model are determined by using superconducting continuous gravity observations for 30 days or more, through data preprocessing, and using a harmonic analysis program to obtain the station's gravity-tide model parameters.
[0026] 2. Step ②
[0027] Use the gravity tide model parameters to calculate the accurate sun and moon gravity and its elastic earth gravity response and ocean tide load gravity effect, that is, use the measured gravity tide model to eliminate the gravitational tide part of the superconducting gravity observation.
[0028] 3. Step ③
[0029] Obtain global gridded temperature and pressure from the web.
[0030] 4. Step ④
[0031] Using the global gridded air temperature and pressure, the atmospheric load elastic gravity response model, calculate the global atmospheric load elastic effect and the direct effect of the far region.
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