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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 111,
D15104,
doi:10.1029/2005JD006724,
2006
Extreme wet years over southern Africa: Role of Indian Ocean sea surface temperatures
Richard Washington
Climate Research Lab, Oxford University Centre for the Environment, University of Oxford, Oxford, UK
Anthony Preston
Climate Research Lab, Oxford University Centre for the Environment, University of Oxford, Oxford, UK
Abstract
Southern Africa is a predominantly semiarid region with a high degree of interannual rainfall variability. Although much of
the recent climate research has focused on the causes of drought events, the region has also experienced extremes of above
average rainfall, the most recent examples being the major flooding episodes that devastated Mozambique during 2000 and 2001.
This paper investigates extremely wet years over southern Africa during the twentieth century. Focusing on the two most extreme
years, 1974 and 1976, we show that while ENSO serves as an important control on rainfall variability, a specific pattern of
SSTs in the SW Indian Ocean, with warm anomalies in the subtropical SW Indian Ocean and cool anomalies in the northern SW
Indian Ocean that is statistically independent of ENSO, plays a crucial role in generating extreme conditions. To do this,
we use a series of multimodel experiments, to demonstrate first the importance of global sea surface temperatures. Through
additional idealized experiments with HadAM3, we then isolate the role of SST anomalies in the Indian Ocean. The anomalies
are based on the observed SSTs with the ENSO signal linearly removed. The critical influence is tied to cold SST anomalies
in the Mascarene region which induce an anomalous anticyclonic circulation driving an anomalous low-level easterly moisture
flux along 10–20°S into eastern southern Africa. This results in enhanced moist convective uplift, conducive to enhanced rainfall,
over a large part of southern Africa. Near surface humidity and 500-hPa omega fields extend from eastern southern Africa into
the Agulhas region in a tropical-temperate cloud band like structure. The similarity between the reanalysis fields for the
extreme years and the model experiments is striking.
Received 30
September
2005;
accepted 2
May
2006;
published 8
August
2006.
Keywords: southern Africa;
extreme rains;
Indian Ocean SST.
Index Terms: 3305 Atmospheric Processes: Climate change and variability (1616, 1635, 3309, 4215, 4513); 1626 Global Change: Global climate models (3337, 4928); 0312 Atmospheric Composition and Structure: Air/sea constituent fluxes (3339, 4504); 1854 Hydrology: Precipitation (3354).
Read Full Article (file size: 975813 bytes) Cited by
Citation: Washington, R., and A. Preston
(2006),
Extreme wet years over southern Africa: Role of Indian Ocean sea surface temperatures,
J. Geophys. Res.,
111,
D15104,
doi:10.1029/2005JD006724.
Copyright 2006 by the American Geophysical Union.
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