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CHAMP and GOCE thermospheric wind characterization with improved gas-surface interactions modelling

机译:CHAMP和GOCE热球风特征与改进的气-面相互作用模型

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The CHAMP and GOCE satellites provided high-resolution thermosphere data between 2000 and 2013, improving our knowledge of atmosphere dynamics in the thermosphere-ionosphere region. However, the currently available data sets contain inconsistencies with each other and with external data sets and models, arising to a large extent from errors in the modelling of aerodynamic forces. Improved processing of the wind data for the two satellites would benefit the further development and validation of thermosphere models and improve current understanding of atmospheric dynamics and long-term trends. The first step to remove inconsistencies has been the development of high-fidelity models of the satellite surface geometry. Next, an improved characterization of the collisions between atmospheric particles and satellite surfaces is necessary. In this article, the effect of varying the energy accommodation coefficient, which is a key parameter for describing gas-surface interactions (GSI) is investigated. For past versions of the thermosphere density and wind data from these satellites a value of the energy accommodation coefficient of alpha(E) = 0.93 was selected. The satellite accelerometer measurements, from which the thermospheric data are derived, have now been reprocessed using high-fidelity geometries and a wide range of alpha(E) values. Lowering the alpha(E) value used in the processing leads to an increase in the lift over drag ratio for those satellite panels that are inclined to the flow. This changes the direction of the modelled acceleration, and therefore the interpretation of the measured acceleration in terms of wind. The wrong choice of alpha(E) therefore leads to the introduction of satellite attitude-dependent wind errors. For the CHAMP and. GOCE satellites, we have found that values of the energy accommodation coefficient significantly lower than 0.93 (0.85 for CHAMP and 0.82 for GOCE) result in increased consistency of the wind data. A comparison between the two missions and an overview of the influence on the results of filtering for solar activity and seasonal and diurnal variations is presented. (C) 2019 COSPAR. Published by Elsevier Ltd. All rights reserved.
机译:CHAMP和GOCE卫星在2000年至2013年之间提供了高分辨率的热圈数据,从而增进了我们对热圈-电离层地区大气动力学的了解。但是,当前可用的数据集彼此之间以及与外部数据集和模型之间存在不一致,这在很大程度上是由气动力建模中的错误引起的。改进两颗卫星的风数据处理将有利于热层模型的进一步开发和验证,并增进当前对大气动力学和长期趋势的了解。消除不一致性的第一步是开发卫星表面几何形状的高保真模型。接下来,需要改善大气颗粒与卫星表面之间碰撞的特征。在本文中,研究了改变能量调节系数的影响,能量调节系数是描述气体表面相互作用(GSI)的关键参数。对于以前版本的这些卫星的热层密度和风数据,选择的能量调节系数为alpha(E)= 0.93。卫星加速度计的测量值(用于导出热层数据)现在已使用高保真几何形状和宽范围的alpha(E)值进行了重新处理。降低处理中使用的alpha(E)值会导致那些倾斜于流动的卫星面板的提升阻力比增加。这改变了建模加速度的方向,因此改变了根据风的测量加速度的解释。因此,错误选择alpha(E)会导致引入与卫星姿态有关的风向误差。对于冠军和。在GOCE卫星中,我们发现能量容纳系数的值大大低于0.93(CHAMP为0.85,GOCE为0.82)会增加风数据的一致性。介绍了两个任务之间的比较,并概述了对太阳活动以及季节和昼夜变化的滤波结果的影响。 (C)2019 COSPAR。由Elsevier Ltd.出版。保留所有权利。

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