Bifurcation of the Pacific North Equatorial Current in a Wind-Driven Model: Response to Climatological Winds

Abstract

The sensitivity of the bifurcation of the North Equatorial Current in the Pacific to different wind products is investigated. Variations of the bifurcation latitude with season is simulated in a purely wind-driven model and is found to be in agreement with recent observations. The seasonal cycle is nearly independent of the wind climatology, but the annual average latitude depends on the wind stress curl. It is also shown that in the upper ocean, the poleward shift in bifurcation latitude with depth is realistic in our simple model. This implies that given a stratification close to the observed, it is primarily the wind forcing that determines the location of the bifurcation and its seasonal variation.

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Document Details

Document Type
Technical Report
Publication Date
May 30, 2011
Accession Number
ADA556056

Entities

People

  • Tommy G. Jensen

Organizations

  • United States Naval Research Laboratory

Tags

Communities of Interest

  • Ground and Sea Platforms

DTIC Thesaurus Topics

  • Agreements
  • Atmospheric Sciences
  • Climatology
  • Earth Sciences
  • Latitude
  • Layers
  • Observation
  • Oceanography
  • Oceans
  • Rossby Waves
  • Seasonal Variations
  • Seasons
  • Sensitivity
  • Stratification
  • Stresses
  • Topography
  • Wind Stress

Fields of Study

  • Mathematics

Readers

  • Atmospheric Science/Meteorology
  • Structural Dynamics.