Studies on Convection in Polar Oceans

Abstract

A laboratory experimental program was carried out to investigate fundamental physical processes related to deep-ocean and under-ice convection occurring in high latitude oceans. With regard to deep convection, the aspects of interest were the preconditioning of a stratified region prior to the onset of convection, breakdown of stratification leading to turbulent convection, growth of convective layer against stable stratification, scales of convection, lateral processes leading to horizontal buoyancy exchanges and the final collapse of deep-convective regions. Studies on convection under an ice cap included the formation and melting of ice due to surface cooling of a two-layer stratified fluid. This problem is rich in a variety of physical processes such as double-diffusive transports of heat and salt and turbulent mixing across the pycnocline that separates the two layers. Important new mechanisms related to above-described convective processes were delineated and simple parameterizations were proposed to represent convective events in numerical models.

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Document Details

Document Type
Technical Report
Publication Date
Jun 30, 1998
Accession Number
ADA355737

Entities

People

  • Harindra Fernando

Organizations

  • Arizona State University

Tags

Communities of Interest

  • Energy and Power Technologies
  • Materials and Manufacturing Processes

DTIC Thesaurus Topics

  • Boundary Layer
  • Buoyancy
  • Convection
  • Fluid Dynamics
  • Fluid Mechanics
  • Fluids
  • Glaciers
  • High Latitudes
  • Hydrodynamics
  • Ice
  • Layers
  • Mechanical Phenomena
  • Mechanics
  • Stratified Fluids
  • Turbulence
  • Turbulent Mixing
  • Water

Readers

  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers