Interhemispheric Differences of Gravity Waves in the Northern and Southern Polar Middle Atmosphere Observed by the Aura Microwave Limb Sounder
Publisher DOI
Abstract
The Aura Microwave Limb Sounder (Aura/MLS) measures temperature profiles with a horizontal spacing of about 170 km along its near polar orbit. We highpass-filtered the horizontal temperature fluctuations along the suborbital track in the middle atmosphere. The characteristics of inertia gravity waves with horizontal wavelengths between 200 and 825 km are evaluated for the equatorial region (10∘ S to 10∘ N), northern polar region (70∘ N to 82∘ N), and southern polar region (70∘ S to 82∘ S) over the time interval from August 2004 to December 2021. A modulation of gravity wave activity by quasi-biennial oscillations is present in the equatorial stratosphere but not in the equatorial mesosphere. The gravity wave activity in the southern polar mesosphere is stronger by a factor of up to 2 than in the northern polar mesosphere. The seasonal variation in the vertical structure of gravity wave activity shows strong interhemispheric differences. There are double layers of enhanced gravity wave activity in the upper mesosphere over Antarctica in the summer and the winter, while the northern polar region does not show a double layer structure of gravity wave activity. In the northern polar region, upper mesospheric gravity wave activity is decreased after the onset of major sudden stratospheric warmings.
Date Issued
2026-07-03
Publication Type
Article
Language(s)
en
Journal
Atmosphere
Publisher
MDPI
ISSN
2073-4433
2073-4433
Funding(s)
Access(Rights)
open.access