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Retrieval of water vapor profile in the mesosphere from satellite ozone and hydroxyl measurements by the basic dynamic model of mesospheric photochemical system

机译:通过中层光化学系统的基本动力学模型,从卫星臭氧和羟基的测量值反演中层水汽剖面

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摘要

We propose an indirect method for retrieving a number of significant minorgas constituents of the atmosphere. The technique is based on the use ofso-called basic dynamic models of atmospheric photochemical systemssimplified mathematically correctly in a special manner. It is applied to amesospheric system describing day evolution of key minor gas constituents atthese heights. We take as initial data experimental data of theCRISTA-MAHRSI satellite campaign of August 1997 during which ozone andhydroxyl (O and OH) concentrations were measured simultaneously. It isdemonstrated that the use of the basic dynamic model allows retrieval ofvertical distribution (within the 53–85 km range of heights) of water vaporconcentration that is one of the control parameters of the mesosphericphotochemistry.
机译:我们提出了一种间接方法来检索大气中许多重要的次要气体成分。该技术基于使用大气光化学系统的所谓基本动力学模型,该模型以特殊方式在数学上正确地简化了。它被用于描述这些高度关键次要气体成分的日演变的流层系统。我们将1997年8月的CRISTA-MAHRSI​​卫星运动的实验数据作为初始数据,在此期间同时测量了臭氧和羟基(O和OH)的浓度。可以证明,使用基本动力学模型可以检索水蒸气浓度的垂直分布(在53-85 km的高度范围内),而水蒸气浓度是中层光化学控制参数之一。

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