Saturday, 3 April 1999: 10:30 AM
The science of Southern Hemisphere meteorology has grown substantially
since the first Conference on this subject held in Sao Jose dos Campos in
1983. The formation of the AMS Committee on Southern Hemisphere meteorology
was founded upon the expectation that elements of austral weather may differ
substantially from those found in the northern hemisphere. The intervening
years have vindicated this expectation in a series of remarkable discoveries
showing the truly unique character of the austral weather patterns. Perhaps
the most stunning discovery was the ozone hole, which was first documented
several years after the Sao Jose Conference, and led to contributions by
future nobel laureates in subsequent related conferences in Buenos Aires.
More recently, enhanced monitoring at the Andean Bolivian foothills has
displayed a very prominent low-level jet that has some distinctive features
with respect to low-level-jets in other parts of the world. This research
and recent research on the ozone hole will be updated in other talks. The
purpose of this presentation is to describe the increased understanding of
intra-seasonal oscillations of the South Atlantic Convergence Zone (SACZ).
This feature was only being discovered around the time that the committee
on Southern Hemisphere meteorology was established, and has now been much
more extensively studied. We review background literature that describes
the relation of the SACZ to South American flood and drought, to Northern
Hemisphere predictability, and to the dynamical structure of the Southern
Hemisphere weather patterns.
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