Venezuelan Rain Systems and the General Circulation of the Summer Tropics II: Relations between Low and High Latitudes

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Abstract
The question, Why are there discrete synoptic weather systems in the tropics without a basic current that can become baroclinically unstable, is considered. Release of kinetic energy through vertical circulations and maintenance of the surface flow against friction by mean values indicate that existence of a simple general circulation cell should be possible. But, in the descending branch the requisite poleward temperature gradient cannot be maintained with radiation cooling. An additional mechanism for heat removal must be sought. Extratropical troughs extending deep into the tropics may provide such a mechanism. At first their role in setting off tropical rain areas is investigated dynamically. It is found that a large imbalance of forces develops in the northerly current on the western side of the troughs which causes the equator-bound air to turn sharply clockwise. Absolute vorticity approaches zero and intense high-tropospheric divergence is initiated acting as a siphon on the lower layers. ... Abstract The question, Why are there discrete synoptic weather systems in the tropics without a basic current that can become baroclinically unstable, is considered. Release of kinetic energy through vertical circulations and maintenance of the surface flow against friction by mean values indicate that existence of a simple general circulation cell should be possible. But, in the descending branch the requisite poleward temperature gradient cannot be maintained with radiation cooling. An additional mechanism for heat removal must be sought. Extratropical troughs extending deep into the tropics may provide such a mechanism. At first their role in setting off tropical rain areas is investigated dynamically. It is found that a large imbalance of forces develops in the northerly current on the western side of the troughs which causes the equator-bound air to turn sharply clockwise. Absolute vorticity approaches zero and intense high-tropospheric divergence is initiated acting as a siphon on the lower layers. ...

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