Short vertical-wavelength inertia-gravity waves generated by a jet–front system at Arctic latitudes – VHF radar, radiosondes and numerical modelling
Inertia-gravity waves with very short vertical wavelength (λ z ≤1000 m) are a very common feature of the lowermost stratosphere as observed by the 52 MHz radar ESRAD (Esrange MST radar) in northern Scandinavia (67.88° N, 21.10° E). The waves are seen most clearly in radar-derived profiles of buoyanc...
Published in: | Atmospheric Chemistry and Physics |
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Main Authors: | , , , |
Format: | Text |
Language: | English |
Published: |
2018
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Subjects: | |
Online Access: | https://doi.org/10.5194/acp-14-6785-2014 https://www.atmos-chem-phys.net/14/6785/2014/ |