修正的CTIP模型及其与DMSP卫星数据的比较

Christopher R. Wilford, R. Moffett, J. M. Rees, R. Heelis
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引用次数: 2

摘要

热层-电离层-等离子体层(CTIP)耦合模型是一个三维模型,通过求解连续性、动量和能量平衡方程来计算离子和电子浓度、温度和场向速度。谢菲尔德大学版本的CTIP模型已经被修改,以包括第三个原子离子,He+。来自国防气象卫星计划(DMSP)的数据用于比较和验证改进的CTIP模型的结果。修改后的CTIP模型再现了He+分布,如数据所示。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A modified CTIP model and comparisons with DMSP satellite data
The coupled thermosphere–ionosphere–plasmasphere (CTIP) model is a three–dimensional model that solves equations of continuity, momentum and energy balance to calculate ion and electron concentrations, temperatures and field–aligned velocities. The University of Sheffield version of the CTIP model has been modified in order to include a third atomic ion, He+. Data from the Defense Meteorological Satellite Program (DMSP) are used to compare and validate the results from the modified CTIP model. The modified CTIP model is shown to reproduce He+ distributions as seen in the data.
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