热层分子氧及其与太阳活动的关系

IF 2.9 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS Journal of Geophysical Research: Space Physics Pub Date : 2025-02-02 DOI:10.1029/2024JA033224
K. R. Greer, M. Jones Jr, J. Lumpe, R. Eastes, F. Laskar, E. Smith, M. Snow, W. E. McClintock
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摘要

全球尺度翼盘观测(Global-scale Observations of Limb and Disk, GOLD)任务的观测为地球中低热层(120-200 km)的分子氧分布提供了新的遥感数据来源。GOLD O2观测表明,在170公里处,随着太阳活动的增加,分子氧密度增加,太阳射电通量F10.7值在60至~ 120太阳通量单位(sfu)之间。在与太阳极紫外线辐照度QEUV在1和~ 2.25 erg cm−2 s−1之间的比较中也可以看到这一点。然而,经验质谱非相干散射雷达2.0 (MSIS 2.0)模型高估了在这些低太阳活动水平下170公里处的O2密度,并预测在~ 120 sfu以下,密度随着太阳通量的增加而降低。额外的数据集证实了对氧的GOLD观测及其与太阳活动的关系。准确测定和预测O2对于准确模拟电离层中的等离子体密度和中低热层中的热层密度至关重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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On Thermospheric Molecular Oxygen and Its Relationship to Solar Activity

Observations from the Global-scale Observations of Limb and Disk (GOLD) mission have provided a new remote-sensing data source of molecular oxygen profiles in Earth's lower-to-middle thermosphere (120–200 km). GOLD O2 observations indicate increasing densities of molecular oxygen at 170 km with rising solar activity between solar radio flux F10.7 values of 60 and ∼120 solar flux units (sfu). This is also seen in comparisons with solar extreme ultraviolet irradiance QEUV between 1 and ∼2.25 erg cm−2 s−1. However, the empirical Mass Spectrometer Incoherent Scatter radar 2.0 (MSIS 2.0) model overestimates O2 densities at 170 km at these low levels of solar activity and predicts a decreasing density with increasing solar flux below ∼120 sfu. Additional data sets validate GOLD observations of O2 and their relationship with solar activity. Accurately determining and forecasting O2 is critical for accurately modeling plasma densities in the ionosphere and thermospheric density in the lower-to-middle thermosphere.

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来源期刊
Journal of Geophysical Research: Space Physics
Journal of Geophysical Research: Space Physics Earth and Planetary Sciences-Geophysics
CiteScore
5.30
自引率
35.70%
发文量
570
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