金星全球电离层-热层模型(V-GITM):热层和电离层耦合模型

IF 3.9 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS
Brandon M. Ponder, Aaron J. Ridley, Stephen W. Bougher, David Pawlowski, Amanda Brecht
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引用次数: 0

摘要

本文介绍了新的金星全球电离层-热层模型(V-GITM),该模型将陆地全球电离层-热层模型框架与金星特定参数、离子中性化学和辐射过程相结合,以模拟 70 至 170 公里金星大气层的温度、组成和动力学结构方面的一些可观测特征。大气过程是根据以前的金星全球大气环流模型所使用的公式计算的,其中还包括一些增强功能,如改进的水平和垂直动量方程以及跟踪放热化学反应。明确求解动量方程可以探索其对昼夜结构的动态影响。此外,V-GITM 使用放热化学反应而不是强热效率,既考虑了太阳 EUV 导致的加热,又产生了与经验模型相当的温度。V-GITM 的中性温度和中性离子密度与 "金星先锋 "和 "金星快车 "获得的高层大气测量数据进行了比较。V-GITM 显示了穿过云顶到中间热层的不对称水平风速,并解释了维持风结构的机制。此外,V-GITM 还产生了合理的日侧离子密度,并表明中性风可以通过实验将 O 2 + ${\mathrm{O}}_{2}^{+}$ 带到夜侧。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

The Venus Global Ionosphere-Thermosphere Model (V-GITM): A Coupled Thermosphere and Ionosphere Formulation

The Venus Global Ionosphere-Thermosphere Model (V-GITM): A Coupled Thermosphere and Ionosphere Formulation

This paper introduces the new Venus global ionosphere-thermosphere model (V-GITM) which incorporates the terrestrial GITM framework with Venus-specific parameters, ion-neutral chemistry, and radiative processes in order to simulate some of the observable features regarding the temperatures, composition, and dynamical structure of the Venus atmosphere from 70 to 170 km. Atmospheric processes are included based upon formulations used in previous Venus GCMs, several augmentations exist, such as improved horizontal and vertical momentum equations and tracking exothermic chemistry. Explicitly solving the momentum equations allows for the exploration of its dynamical effects on the day-night structure. In addition, V-GITM's use of exothermic chemistry instead of a strong heating efficiency accounts for the heating due to the solar EUV while producing comparable temperatures to empirical models. V-GITM neutral temperatures and neutral-ion densities are compared to upper atmosphere measurements obtained from Pioneer Venus and Venus Express. V-GITM demonstrates asymmetric horizontal wind velocities through the cloud tops to the middle thermosphere and explains the mechanisms for sustaining the wind structure. In addition, V-GITM produces reasonable dayside ion densities and shows that the neutral winds can carry the ions to the nightside via an experiment advecting O 2 + ${\mathrm{O}}_{2}^{+}$ .

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来源期刊
Journal of Geophysical Research: Planets
Journal of Geophysical Research: Planets Earth and Planetary Sciences-Earth and Planetary Sciences (miscellaneous)
CiteScore
8.00
自引率
27.10%
发文量
254
期刊介绍: The Journal of Geophysical Research Planets is dedicated to the publication of new and original research in the broad field of planetary science. Manuscripts concerning planetary geology, geophysics, geochemistry, atmospheres, and dynamics are appropriate for the journal when they increase knowledge about the processes that affect Solar System objects. Manuscripts concerning other planetary systems, exoplanets or Earth are welcome when presented in a comparative planetology perspective. Studies in the field of astrobiology will be considered when they have immediate consequences for the interpretation of planetary data. JGR: Planets does not publish manuscripts that deal with future missions and instrumentation, nor those that are primarily of an engineering interest. Instrument, calibration or data processing papers may be appropriate for the journal, but only when accompanied by scientific analysis and interpretation that increases understanding of the studied object. A manuscript that describes a new method or technique would be acceptable for JGR: Planets if it contained new and relevant scientific results obtained using the method. Review articles are generally not appropriate for JGR: Planets, but they may be considered if they form an integral part of a special issue.
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