A Numerical Investigation of Mixed-Layer Processes in the Arabian Sea.

Abstract

The primary result accomplished during this-ONR project was the development of an ocean model of intermediate complexity that is able to simulate accurately the diurnal and annual cycles of mixed-layer thickness at the WHOI mooring site in the Arabian Sea. Modifications that allowed this success were: i) allowing the density jump at the bottom of the mixed layer to vary realistically throughout the day; and ii) including a diurnal-thermocline layer. When a biological model is coupled to this physical model, the response is improved in that blooms are weakened and broadened by the diurnal variability; however, the variability associated with active and break periods of the monsoon have a much larger effect on the blooms. The addition of salinity variability is essential for simulating mixed-layer variability in the Bay of Bengal where rainfall and river runoff are intense. In contrast, salinity effects are much smaller in the Arabian Sea where these forcings are an order of magnitude weaker.

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Document Details

Document Type
Technical Report
Publication Date
Feb 11, 1999
Accession Number
ADA360002

Tags

Communities of Interest

  • Materials and Manufacturing Processes

DTIC Thesaurus Topics

  • Air Temperature
  • Arabian Sea
  • Biological Phenomena
  • Contrast
  • Deep Oceans
  • Indian Ocean
  • Ocean Currents
  • Oceans
  • Pressure Gradients
  • Rainfall
  • Runoff
  • Salinity
  • Solar Radiation
  • Technical Information Centers
  • Temperature Gradients
  • Thermoclines
  • Thickness

Fields of Study

  • Environmental science

Readers

  • Atmospheric Science/Meteorology
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers