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Main Library
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Observations of Stratospheric Gravity Waves Over Europe on 12 January 2016: The Role of the Polar Night Jet.
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- Author(s): Bossert, Katrina; Vadas, Sharon L.; Hoffmann, Lars; Becker, Erich; Harvey, V. Lynn; Bramberger, Martina
- Source:
Journal of Geophysical Research. Atmospheres; 11/16/2020, Vol. 125 Issue 21, p1-14, 14p- Subject Terms:
- Source:
- Additional Information
- Subject Terms:
- Abstract: Observations during 12 January 2016 revealed a series of events of significant gravity wave (GW) activity over Europe. Analysis of derived temperatures from the Atmospheric InfraRed Sounder (AIRS) provides insight into the sources of these GWs, and include a new observation of stratosphere polar night jet (PNJ) generated GWs. Mountain waves were present during this time as well over the French Alps and the Carpathian Mountains and had maximum temperature perturbations, T′, as large as 27 K over the French Alps. Further investigation of the mountain waves that demonstrated their presence in the stratosphere was determined not only by stratospheric conditions but also by strong winds in the troposphere and at the surface. GWs generated in the stratosphere by the PNJ had maximum T′ of 7 K. These observations demonstrate multiple sources of GWs during a dynamically active period and implicate the role of the PNJ in both the vertical propagation of GWs generated in the troposphere and the generation of GWs from the PNJ itself. Key Points: AIRS observations demonstrate the presence of gravity waves generated by the polar night jetDownward propagating gravity waves were observed at altitudes below the polar night jetThe polar night jet plays an important role in the growth of mountain waves in the stratosphere [ABSTRACT FROM AUTHOR]
- Abstract: Copyright of Journal of Geophysical Research. Atmospheres is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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