On the dynamics of flows induced by topographic ridges

Changheng Chen, Igor Kamenkovich, Pavel Berloff

Research output: Contribution to journalArticle

6 Scopus citations

Abstract

This study describes a nonlocal mechanism for the generation of oceanic alternating jets by topographic ridges. The dynamics of these jets is examined using a baroclinic quasigeostrophic model configured with an isolated meridional ridge. The zonal topographic slopes of the ridge lead to the formation of a system of currents, consisting of mesoscale eddies, meridional currents over the ridge, and multiple zonal jets in the far field. Dynamical analysis shows that transient eddies are vital in sustaining the deep meridional currents over the ridge, which in turn play a key role in the upper-layer potential vorticity (PV) balance. The zonal jets in the rest of the domain owe their existence to the eddy forcing over the ridge but are maintained by the local Reynolds and form stress eddy forcing. The analysis further shows that a broad stable current that either becomes locally nonzonal or encounters a topographic ridge tends to become unstable. This instability provides a vorticity source and generates multiple zonal jets in the far field through a nonlocal mechanism.

Original languageEnglish (US)
Pages (from-to)927-940
Number of pages14
JournalJournal of Physical Oceanography
Volume45
Issue number3
DOIs
StatePublished - Jan 1 2015

Keywords

  • Atm/Ocean structure/Phenomena
  • Baroclinic flows
  • Circulation/Dynamics
  • Eddies
  • Jets
  • Mesoscale processes
  • Ocean dynamics
  • Topographic effects

ASJC Scopus subject areas

  • Oceanography

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