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At altitudes 90 150 km the Venusian air moves from the dayside to nightside of the planet, with upwelling over sunlit hemisphere and downwelling over dark hemisphere.
The delay in arrival of the upwelling over KTB is about 20 min, relative to its appearance over CPN.
In this scenario, the telling feature would be a delay in appearance of the upwelling over KTB, relative to its appearance over CPN.
Referring back to Fig. 12, we have marked the mean time of appearance of the upwelling over CPN with a labeled arrow.
Noting that the upwelling over CPN on M27 took 2 h to drift to BCL, we suggest that our extreme events are related to deep upwelling events and OGC paths with long persistence.
We note that the onsets of RSF, around the times of appearance of presumably the same upwelling, over CPN, KTB, and BCL, clearly strengthen the evidence in support of this hypothesis.
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Upwelling growth over KWA was accompanied by strong RSF.
These zones of strong upwelling extend over several hundred kilometres and are driven by the interaction of the eastward-flowing Antarctic Circumpolar Current with large-scale bathymetric features: the South-East Indian Ridge (140°E), and the Pacific-Antarctic Ridge (east of 165°E).
Pteropods and other plankton congregate over upwelling spots because they are good sources of nutrients and food.
The continent of Africa has moved and rotated just slightly over the intervening millions of years, shifting the relative location of the upwelling.
These authors compared the diversity and trophic structure of intertidal assemblages over a large number of sites in four geographic regions influenced by upwelling.
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