File:Obninsk-Collm.jpg
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(Obninsk (55°N, 37°E) and Collm (52°N, 15°E) winter MLT zonal prevailing winds as well as their differences (blue line). The zonal wind differences at this relatively short distance is correlated with stationary planetary waves (SPW) in the stratospher)
(Obninsk (55°N, 37°E) and Collm (52°N, 15°E) winter MLT zonal prevailing winds as well as their differences (blue line). The zonal wind differences at this relatively short distance is correlated with stationary planetary waves (SPW) in the stratospher)
Latest revision as of 12:49, 6 July 2010
Obninsk (55°N, 37°E) and Collm (52°N, 15°E) winter MLT zonal prevailing winds as well as their differences (blue line). The zonal wind differences at this relatively short distance is correlated with stationary planetary waves (SPW) in the stratosphere (pink line).
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| current | 12:49, 6 July 2010 |  | 1,889×1,326 (606 KB) | Jacobi (Talk | contribs) | (Obninsk (55°N, 37°E) and Collm (52°N, 15°E) winter MLT zonal prevailing winds as well as their differences (blue line). The zonal wind differences at this relatively short distance is correlated with stationary planetary waves (SPW) in the stratospher) |
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