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Earth, Planets and Space
Fig. 6 | Earth, Planets and Space

Fig. 6

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

Fig. 6

Horizontal structures of the temperature disturbance, longitude–altitude cross section of the temperature disturbance on the equator, and longitudinal profiles of the temperature disturbance along the equator for the cases of the neutral layer thicknesses of 5 km (a, d, g), 10 km (b, e, h), and 15 km (c, f, i) (see Fig. 2). Note that regions of 3 K and above were filled with purple, and regions of − 3 K and below were filled with yellow (d, e, f)

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