Zonal Circulations over the Equatorial Indian Ocean

The NCEP–NCAR 1958–97 upper-air dataset and surface observations have been analyzed for evidence of zonal–vertical circulations along the Indian Ocean equator and their role in climatic variability. The long-term mean upper-tropospheric circulation is dominated in boreal winter by divergent outflow...

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Bibliographic Details
Published inJournal of climate Vol. 13; no. 15; pp. 2746 - 2756
Main Author Hastenrath, Stefan
Format Journal Article
LanguageEnglish
Published Boston, MA American Meteorological Society 01.08.2000
Subjects
Atmospheric circulation
Atmospheric pressure
Climate
Coasts
Datasets
Earth, ocean, space
Equator
Exact sciences and technology
External geophysics
General circulation. Atmospheric waves
Marine
Meteorology
Oceans
Rain
Seasons
Subsidence
Troposphere
Vertical motion
Water outflow
Zonal flow
Indian Ocean
ISW, Indian Ocean
Tropical Indian Ocean
Zonal circulation
Data analysis
Vertical circulation
Climate variation
Troposphere
Interannual variation
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Summary:The NCEP–NCAR 1958–97 upper-air dataset and surface observations have been analyzed for evidence of zonal–vertical circulations along the Indian Ocean equator and their role in climatic variability. The long-term mean upper-tropospheric circulation is dominated in boreal winter by divergent outflow from the southern Indian Ocean northwestward into southern Asia, and in summer from southern Asia southwestward into the Southern Hemisphere. In boreal autumn only, divergent easterlies blow from Indonesia along the equator into an upper-tropospheric convergence band over East Africa, and only then a closed zonal–vertical circulation cell materializes along the Indian Ocean equator, between the centers of ascending motion over Indonesia and of subsidence over equatorial East Africa, and featuring westerlies in the lower layers. The boreal autumn zonal–vertical circulation varies interannually. A regime of intense circulation features accelerated equatorial surface westerlies, enhanced subsidence, and deficient rainfall at the coast of East Africa. In the high phase of the Southern Oscillation [anomalously high (low) pressure at Tahiti (Darwin)] this regime is preferred. The regime of weak zonal circulation has the opposite departure characteristics.
Bibliography:ObjectType-Article-2
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ISSN:0894-8755
1520-0442
DOI:10.1175/1520-0442(2000)013<2746:zcotei>2.0.co;2