The Existence and Vertical Structure of Fast, Eastward-Moving Disturbances in the Equatorial Troposphere

A study examines the fast, eastward propagating signal associated with the intraseasonal tropical oscillation. The signal is conceptualized as a far-field dispersion product of strong convection with the intraseasonal tropical oscillation in the Indian Ocean and Western Pacific.

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Veröffentlicht in:Journal of the atmospheric sciences 1996-02, Vol.53 (4), p.586-597
Hauptverfasser: Milliff, Ralph F, Madden, Roland A
Format: Artikel
Sprache:eng
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Zusammenfassung:A study examines the fast, eastward propagating signal associated with the intraseasonal tropical oscillation. The signal is conceptualized as a far-field dispersion product of strong convection with the intraseasonal tropical oscillation in the Indian Ocean and Western Pacific.
ISSN:0022-4928
1520-0469
DOI:10.1175/1520-0469(1996)053<0586:teavso>2.0.co;2