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机构地区:[1]Henan Engineering Laboratory for Big Data Statistical Analysis and Optimal Control,School of Mathematics and Information Sciences,Henan Normal University,Xinxiang Henan 453007,China [2]State Key Laboratory of Space Weather,Center for Space Science and Applied Research,Chinese Academy of Sciences,Beijing 100190,China [3]School of Astronomyand Space Science,University of the Chinese Academy of Science,Beijing 100049,China [4]Catholic University of America,Washington,DC 20064,USA [5]National Aeronautics and Space Administration(NASA)Goddard Space Flight Center,Greenbelt,MD 20771,USA
出 处:《Earth and Planetary Physics》2020年第5期504-512,共9页地球与行星物理(英文版)
基 金:This work was supported by the National Natural Science Foundation of China(grants 41831073 and 41874182).
摘 要:The global atmospheric static stability(N2)in the middle atmosphere and its relation to gravity waves(GWs)were investigated by using the temperature profiles measured by the Sounding of the Atmosphere using Broadband Emission Radiometry(SABER)instrument from 2002 to 2018.At low latitudes,a layer with enhanced N2 occurs at an altitude of^20 km and exhibits annual oscillations caused by tropopause inversion layers.Above an altitude of^70 km,enhanced N2 exhibits semiannual oscillations at low latitudes caused by the mesosphere inversion layers and annual oscillations at high latitudes resulting from the downward shift of the summer mesopause.The correlation coefficients between N2 and GW amplitudes can be larger than 0.8 at latitudes poleward of^40°N/S.This observation provides factual evidence that a large N2 supports large-amplitude GWs and indicates that N2 plays a dominant role in maintaining GWs at least at high latitudes of the middle atmosphere.This evidence also partially explains the previous results regarding the phase changes of annual oscillations of GWs at high latitudes.
关 键 词:atmospheric static stability gravity waves annual oscillation semiannual oscillation MESOPAUSE
分 类 号:P433[天文地球—大气科学及气象学]
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