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Alexander S. Medvedev and Erdal Yiğit Thermal effects of internal gravity waves in the Martian upper atmosphere Geophysical Research Letters 39

Version of Record online: 9 MAR 2012 | DOI: 10.1029/2012GL050852

Key Points

  • Thermal effects of GWs have been parameterized in a Martian GCM
  • GWs produce a significant cooling above 100 km, well in line with observations
  • These effects are comparable with radiative effects of CO2 and must be accounted

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