Abstract
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. ...
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.