Mesosphere/Lower Thermosphere 3‐Dimensional Spatially Resolved Winds Observed by Chinese Multistatic Meteor Radar Network Using the Newly Developed VVP Method

Author:

Zeng Jie12ORCID,Stober Gunter3,Yi Wen12ORCID,Xue Xianghui1245ORCID,Zhong Wei12,Reid Iain67ORCID,Adami Chris6,Ning Baiqi8,Li Guozhu8ORCID,Dou Xiankang4ORCID

Affiliation:

1. Chinese Academy of Sciences Key Laboratory of Geospace Environment Department of Geophysics and Planetary Sciences University of Science and Technology of China Hefei China

2. CAS Center for Excellence in Comparative Planetology Anhui Mengcheng Geophysics National Observation and Research Station University of Science and Technology of China Hefei China

3. Institute of Applied Physics and Oeschger Center for Climate Change Research Microwave Physics University of Bern Bern Switzerland

4. Hefei National Laboratory University of Science and Technology of China Hefei China

5. Collaborative Innovation Center of Astronautical Science and Technology Harbin China

6. ATRAD Pty Ltd. Underdale SA Australia

7. School of Physical Sciences University of Adelaide Adelaide SA Australia

8. Key Laboratory of Earth and Planetary Physics Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China

Abstract

AbstractWe present the first continuous observations of three‐dimensional spatially resolved wind fields and atmospheric motions in the mesosphere and lower thermosphere in the mid‐latitudes of the Northern Hemisphere. Our observations were performed during a 19‐month campaign from January 2022 to July 2023 and exploited the composite data from the first multistatic meteor radar system in China and an adjacent monostatic meteor radar. To retrieve the atmospheric kinetic properties, we introduce an improved volume velocity processing method including coordinate transformations and non‐linear constraints to minimize errors. The vertical winds are estimated separately from the iteration of the horizontal divergence to avoid potential biases or contamination from the horizontal winds. The winds and air motions show annual/semiannual variation characteristics within certain altitudes, usually more variable around the equinoxes. The vertical winds are basically within the magnitude of 1 m/s and are upward as expected at the mesopause during the summer, which corresponds to the adiabatic cooling.

Publisher

American Geophysical Union (AGU)

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