loading page

Mesospheric Mountain Wave Activity in the Lee of the Southern Andes
  • +4
  • Pierre-Dominique Pautet,
  • Michael J. Taylor,
  • David C. Fritts,
  • Diego Janches,
  • Natalie Kaifler,
  • Andreas Dörnbrack,
  • Jose Luis Hormaechea
Pierre-Dominique Pautet
Utah State Uiversity

Corresponding Author:[email protected]

Author Profile
Michael J. Taylor
Utah State University
Author Profile
David C. Fritts
GATS
Author Profile
Diego Janches
National Aeronautics and Space Administration (NASA)
Author Profile
Natalie Kaifler
Institute of Atmospheric Physics, German Aerospace Center
Author Profile
Andreas Dörnbrack
DLR
Author Profile
Jose Luis Hormaechea
Facultad de Ciencias Astronomicas y Geofisicas UNLP
Author Profile

Abstract

Gravity waves (GWs) generated by orographic forcing, also known as mountain waves (MWs) have been studied for decades. First measured in the troposphere, then in the stratosphere, they were only imaged at mesospheric altitude in 2008. Their characteristics have been investigated during several recent observation campaigns, but many questions remain concerning their impacts on the upper atmosphere, and the effects of the background environment on their deep propagation.
An Advanced Mesospheric Temperature Mapper (AMTM) and the Southern Argentina Agile MEteor Radar (SAAMER) have been operated simultaneously during the Austral winter 2018 from Rio Grande, Argentina (53.8°S). This site is located near the tip of South America, in the lee of the Andes Mountains, a region considered the largest MW hotspot on Earth.
New AMTM image data obtained during a 6-month period show almost 100 occurrences of MW signatures penetrating into the upper mesosphere. They are visible ~30% of time at the height of the winter season (mid-May to mid-July). Their intermittency is highly correlated with the zonal wind controlled by the semi-diurnal tide, revealing the direct effect of the atmospheric background on MW penetration into the Mesosphere Lower Thermosphere (MLT, altitude 80-100 km). Measurements of their momentum fluxes (MF) were determined to reach very large values (average ~250 m/s), providing strong evidence of the importance and impacts of small-scale gravity waves at mesospheric altitudes.
16 Apr 2021Published in Journal of Geophysical Research: Atmospheres volume 126 issue 7. 10.1029/2020JD033268