Persistent Layers of Enhanced Gravity Wave Dissipation in the Upper Mesosphere Revealed From SABER Observations

Xiao Liu, Jiyao Xu, Jia Yue, Masaru Kogure

研究成果: ジャーナルへの寄稿学術誌査読

4 被引用数 (Scopus)

抄録

Dissipation of gravity waves (GWs) and resultant momentum flux deposition and eddy diffusion significantly influence the atmospheric structure and circulation. Using the temperature profiles measured by the SABER instrument (2002–2021), we derive the global GW action and its scale height (HAm). Comparing to the background scale height (H), we identify a persistent layer of enhanced GW dissipation (HAm/H > 2) in the upper mesosphere. The enhanced dissipation is primarily centered at 80–85 km with a vertical range of ∼8–20 km. At middle and high latitudes, the enhanced dissipation extends down to ∼60 km and is located above the eastward (westward) wind peak in winter (summer). At low latitudes, enhanced dissipation occurs around the wind reversals. The possible mechanisms of enhanced dissipation include wave refraction, wind filtering, and reduced static stability. The persistent layer of enhanced dissipation identified here provide observational evidence for GW dissipation constrains in models.

本文言語英語
論文番号e2021GL097038
ジャーナルGeophysical Research Letters
49
5
DOI
出版ステータス出版済み - 3月 16 2022

!!!All Science Journal Classification (ASJC) codes

  • 地球物理学
  • 地球惑星科学一般

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