Atmospherically forced exchange through the Bab El Mandeb strait

William E. Johns, Sarantis S. Sofianos

Research output: Contribution to journalArticle

16 Scopus citations

Abstract

The exchange between the Red Sea and the Indian Ocean on synoptic time scales (days to weeks) is investigated using moored current meter data collected in the strait of Bab el Mandeb from June 1995 to November 1996. Transport variations through the strait on these time scales can reach amplitudes of up to 0.6 Sv (1 Sv ≡ 10 6 m 3 s -1), or nearly twice as large as the mean rate of exchange through the strait driven by annual evaporation over the Red Sea. The synoptic transport variability appears to be driven by two primary forcingmechanisms, 1) local wind stress variability over the strait and 2) variation in the large-scale barometric pressure over theRed Sea. Simple models of the forced response are developed and are shown to reproduce the essential features of the observations. The response to barometric pressure forcing over the Red Sea is fundamentally barotropic, whereas the response to along-strait winds is barotropic at high frequencies and tends toward a two-layer exchange at low frequencies. The responses to both types of forcing show enhanced amplitude at the Helmholtz resonance frequency for theRed Sea, which occurs at a period of about 5 days. A linear two-layer model, incorporating both types of forcing and a reasonable frictional parameterization, is shown to account for about 70% of the observed transport variance within the strait.

Original languageEnglish (US)
Pages (from-to)1143-1157
Number of pages15
JournalJournal of Physical Oceanography
Volume42
Issue number7
DOIs
StatePublished - Jul 1 2012

Keywords

  • Channel flowsl
  • Forcing
  • Indian Ocean
  • Mass fluxes/transport
  • Seas/gulfs/bays

ASJC Scopus subject areas

  • Oceanography

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