The Two-Dimensional Evolution of Thermospheric n-ary sumation O/N2Response to Weak Geomagnetic Activity During Solar-Minimum Observed by GOLD

被引:76
作者
Cai, Xuguang [1 ]
Burns, Alan G. [1 ]
Wang, Wenbin [1 ]
Qian, Liying [1 ]
Solomon, Stanley C. [1 ]
Eastes, Richard W. [2 ]
Pedatella, Nicholas [1 ]
Daniell, Robert E. [3 ]
McClintock, William E. [2 ]
机构
[1] Natl Ctr Atmospher Res, High Altitude Observ, Pob 3000, Boulder, CO 80307 USA
[2] Univ Colorado, Lab Atmospher & Space Phys, Boulder, CO 80309 USA
[3] Ionospher Phys, Stoughton, MA USA
基金
美国国家科学基金会;
关键词
O; N-2 column density ratio; thermosphere composition; weak geomagnetic activity; IONOSPHERIC STORMS; UPPER-ATMOSPHERE; PERTURBATIONS; MIDDLE;
D O I
10.1029/2020GL088838
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
We conduct observational and modeling studies of thermospheric composition responses to weak geomagnetic activity (nongeomagnetic storms). We found that the thermospheric O and N(2)column density ratio ( n-ary sumation O/N-2) in part of the Northern Hemisphere measured by Global-scale Observations of the Limb and Disk (GOLD) exhibited large and long-lived depletions during weak geomagnetic activity in May and June 2019. The depletions reached 30% of quiet time values, extended equatorward to 10 degrees N and lasted more than 10 hr. Furthermore, numerical simulation results are similar to these observations and indicate that the n-ary sumation O/N(2)depletions were pushed westward by zonal winds. The n-ary sumation O/N(2)evolution during weak geomagnetic activity suggests that the formation mechanism of the n-ary sumation O/N(2)depletions is similar to that during a geomagnetic storm. The effects of weak geomagnetic activity are often ignored but, in fact, are important for understanding thermosphere neutral composition variability and hence the state of the thermosphere-ionosphere system.
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页数:9
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