低层对东亚上空零星 E 层的可能控制作用

IF 2.6 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS
Hai-Sheng Zhao, Zheng-Wen Xu, Kun Xue, Jian Wu, Ya-Xin Liu, Jie Feng, Cheng Wang, Yu-Sheng Zhang, Na Li
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引用次数: 0

摘要

零星的 E 层(Es)为探索从低层大气到高层大气的耦合提供了独特的机会。研究发现,东亚是 E 层强度和发生概率最高的地区。本文利用过去 60 年中国和日本 21 个电离层探测站的长期数据,探讨了低层对 E 层的可能控制。研究发现,Es层的强度与地表大气温度、地形和海陆边界密切相关。Es层强度与地表温度的相关系数高达0.8204,与地形和海陆边界的相关系数高达0.6668。本文基于大气低层与高层之间的耦合关系,揭示了低层对东亚地区Es强度的可能控制。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Probable Controls From the Lower Layers on Sporadic E Layer Over East Asia

The sporadic E-layer (Es) exhibits unique opportunity for exploring the coupling from lower to upper atmosphere. It was found that the East Asia is with the highest intensity and occurrence probability of Es. By using the long-term data of 21 ionosonde stations in China and Japan over the past 60 yrs, this paper explores the probable control on the Es layer from the lower layers. It is found that the intensity of the Es layer is strongly correlated with the surface atmospheric temperature, terrain, and land-sea boundary. The correlation coefficient of the intensity of Es with surface temperature is as high as 0.8204, while that with the terrain and land-sea boundary is up to 0.6668. Based on the coupling between the lower and upper atmosphere, this paper reveals the probable controls from lower layers on the intensity of the Es in East Asia.

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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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