Laterally forced equatorial perturbations in a linear model. Part I: stationary transient forcing

Chidong Zhang, P. J. Webster

Research output: Contribution to journalArticle

27 Citations (Scopus)

Abstract

Atmospheric equatorial perturbations generated by extratropical transient forcing are simulated numerically in a linear model. Impacts of mean zonal wind on such lateral forcing processes are emphasized. The extratropical forcing source is stationary and localized, with its amplitude varying with time. This forcing configuration simulates atmospheric events that may intrude into the tropics from the extratropics, such as the cold surges during the Asian winter monsoons and the deep midocean troughs. For forcing of large time scales (≥4 day), the equatorial responses are completely dominated by the Rossby mode component. When the forcing time scale is one day or smaller, the major components in the equatorial perturbations are the Rossby, westward mixed Rossby-gravity, and Kelvin modes. -from Authors

Original languageEnglish (US)
Pages (from-to)585-607
Number of pages23
JournalJournal of the Atmospheric Sciences
Volume49
Issue number7
StatePublished - 1992
Externally publishedYes

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Tropics
Gravitation
perturbation
timescale
zonal wind
trough
monsoon
gravity
winter
cold
tropics

ASJC Scopus subject areas

  • Atmospheric Science
  • Engineering(all)

Cite this

Laterally forced equatorial perturbations in a linear model. Part I : stationary transient forcing. / Zhang, Chidong; Webster, P. J.

In: Journal of the Atmospheric Sciences, Vol. 49, No. 7, 1992, p. 585-607.

Research output: Contribution to journalArticle

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