A Statistical Study of Space Hurricanes in the Southern Hemisphere

Author:

Lu Sheng1,Xing Zan‐Yang1ORCID,Zhang Qing‐He12ORCID,Zhang Yong‐Liang3ORCID,Yang Hui‐Gen14ORCID,Oksavik Kjellmar56ORCID,Lyons L. R.7ORCID,Lockwood Michael8ORCID,Ma Yu‐Zhang1ORCID,Wang Xiang‐Yu1,Deng Zhong‐Xin9,Xu Tong9ORCID,Li Guo‐Jun10,Wang Yong1ORCID,Zhang Duan1ORCID

Affiliation:

1. Shandong Provincial Key Laboratory of Optical Astronomy and Solar‐Terrestrial Environment Institute of Space Sciences Shandong University Weihai China

2. State Key Laboratory of Space Weather National Space Science Center Chinese Academy of Sciences Beijing China

3. Applied Physics Laboratory The Johns Hopkins University Laurel MD USA

4. Polar Research Institute of China Shanghai China

5. Department of Physics and Technology University of Bergen Bergen Norway

6. Arctic Geophysics University Centre in Svalbard Longyearbyen Norway

7. Department of Atmospheric and Oceanic Sciences University of California Los Angeles Los Angeles CA USA

8. Department of Meteorology University of Reading Reading UK

9. China Research Institute of Radiowave Propagation Qingdao China

10. Lab of BLOS Reliable Information Transmission Chongqing University of Posts and Telecommunications Chongqing China

Abstract

AbstractThe space hurricane is a large‐scale three‐dimensional magnetic vortex structure that can cause massive local energy injections in the polar cap. By analyzing Defense Meteorological Satellite Program (DMSP) F16–F19 satellite observations from 2005 to 2016, we found that the Southern Hemisphere space hurricane mainly occurs in summer under negative By dominated northward interplanetary magnetic field (IMF) conditions. In particular, the space hurricanes are more likely to occur in the dayside polar cap at magnetic latitude greater than 80°. The characteristics for the Southern Hemisphere are basically consistent with the characteristics of space hurricanes in the Northern Hemisphere. The different dependences of By component in different hemispheres supports the high‐latitude lobe reconnection as the formation mechanism. Plasma data from DMSP satellites in both hemispheres show that the appearance of the space hurricane greatly enhances the convection in the polar cap and the electron density on its dawn side. Within the space hurricane, electron temperatures typically increase significantly, accompanied by strong upward field‐aligned currents and electron precipitation. These results give us a better understanding of the solar wind‐magnetosphere‐polar ionosphere coupling process under northward IMF conditions.

Funder

National Natural Science Foundation of China

China Postdoctoral Science Foundation

Publisher

American Geophysical Union (AGU)

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