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Semi-annual oscillation of the global divergent circulation Cover

Semi-annual oscillation of the global divergent circulation

Open Access
|Jan 1992

Abstract

The multi-year outgoing long-wave radiation (OLR) and velocity potential (χ) generated from the 200-mb wind fields of the National Meteorological Center and the European Centre for Medium-Range Weather Forecasts were used to examine the structure of the semi-annual divergent circulation and its relation with tropical cumulus convection. As inferred from the semi-annual mode of the asymmetric OLR component (OLRE), the east’west differential response to the solar heating between the Asian-Australian (AA) monsoon (60°E–120°W) and the extra-AA monsoon (120°W–60°E) hemispheres sustains a distinct semi-annual mode of the asymmetric divergent circulation with a wavenumber-1 structure. This semi-annual mode of the asymmetric divergent circulation, represented by the asymmetric velocity potential (χE), develops in time coherently with the semi-annual mode of tropical cumulus convection, which indicates a faster response in the extra-AA monsoon hemisphere. That is, the negative centres of semiannual OLRE anomalies and the divergent center of the semi-annual χE field appear in the extra-AA monsoon hemisphere in April/October and in the AA-monsoon hemisphere in January/July.

Language: English
Page range: 357 - 365
Submitted on: Oct 1, 1991
Accepted on: Apr 8, 1992
Published on: Jan 1, 1992
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 1992 Tsing-Chang Chen, Kuang-Der Wu, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.