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

Inactive Publication Date: 2009-09-09
INST OF GEODESY & GEOPHYSICS CHINESE ACADEMY OF SCI
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AI Technical Summary

Problems solved by technology

The total vertical air mass can be obtained from atmospheric pressure observations, but there is no direct and ready-made observation method for the gravitational force of the air mass near the station to the station

Method used

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  • Method for continously observing and determining the vertical distribution of atmospheric water vapor by using superconductive gravity
  • Method for continously observing and determining the vertical distribution of atmospheric water vapor by using superconductive gravity
  • Method for continously observing and determining the vertical distribution of atmospheric water vapor by using superconductive gravity

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Embodiment Construction

[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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Abstract

The invention discloses a method for continously observing and determining the vertical distribution of atmospheric water vapor by using superconductive gravity and relates to a method for determining the vertical distribution of the atmospheric water vapor. The method comprehensively uses earth tide theory, observation technology, atmosphere load gravity correction theory and simulates global surface pressure temperature observation data and the like which eliminate other phenomena except that the atmosphere acts on the gravity on the station above 50 kilometers away from the surface of the ground point of an observation station, to obtain ground point gravitation which the atmosphere in an area acts on; and then atmosphere vertical water vapor is inversed. The method is a fire-new method, is added with a new observation means, and can increase the observation time and spatial resolution of the atmosphere vertical water vapor. Combined with the observation of the wind speed and wind direction, the method can be used for observing three-dimensional water vapor distribution and increases the accuracy of weather forecast.

Description

technical field [0001] The invention relates to a method for determining the vertical distribution of atmospheric water vapor, in particular to a method for determining the vertical distribution of atmospheric water vapor by using superconducting gravity continuous observation. Background technique [0002] The water vapor content in the air is an important parameter in meteorology, especially weather such as precipitation and snow is closely related to production, life and military operations, and the accuracy of forecasting is particularly important. For a long time, the observation of water vapor distribution in space has mainly relied on sounding balloons and water vapor radiometers. The spatial and temporal density distribution of the data is very limited. People have been trying to improve the observation of water vapor content in space, and have spared no expense in researching ground-based and space-based meteorological element observation technologies, such as wate...

Claims

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Application Information

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Patent Type & Authority Applications(China)
IPC IPC(8): G01N33/00
CPCY02A90/10
Inventor 罗少聪周百力
Owner INST OF GEODESY & GEOPHYSICS CHINESE ACADEMY OF SCI
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