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Earth, Planets and Space
Fig. 5 | Earth, Planets and Space

Fig. 5

From: Influence of the cloud-level neutral layer on the vertical propagation of topographically generated gravity waves on Venus

Fig. 5

a Longitude–altitude cross section of the temperature disturbance on the equator for the nominal case shown in Fig. 2. The zonal wind direction is right to left. b Vertical profile of the temperature disturbance just above the position of the wave forcing. Note that regions of 3 K and above were filled with purple, and regions of − 3 K and below were filled with yellow (a)

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