Winter Climatology of Short-Period Mesospheric Gravity Waves Over Alaska

Momentum deposition by short-period (<1 h) gravity waves is known to play a major role in the global circulation in the mesosphere and lower thermosphere (MLT) region ~80-100 km (e.g. Fritts and Alexander, 2003). Observations of these waves over the Arctic region are few and their impact on the A...

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Bibliographic Details
Main Authors: Negale, Michael, Nielsen, Kim, Taylor, Michael J., Pautet, Dominique
Format: Text
Language:unknown
Published: Hosted by Utah State University Libraries 2013
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Online Access:https://digitalcommons.usu.edu/phys_stures/25
https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=1018&context=phys_stures
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Summary:Momentum deposition by short-period (<1 h) gravity waves is known to play a major role in the global circulation in the mesosphere and lower thermosphere (MLT) region ~80-100 km (e.g. Fritts and Alexander, 2003). Observations of these waves over the Arctic region are few and their impact on the Arctic MLT region is of high interest, but has yet to be determined. The Mesospheric Airglow Imaging and Dynamics (MAID) project was initiated in January 2011 to investigate short-period gravity wave dynamics over central Alaska. In this poster, we focus on quantifying the climatology of short-period gravity waves during two winter seasons (2011-2012) over central Alaska