Modeling a Rain-Induced Mixed Layer

Abstract

With the development of ocean surface remote sensing, air sea interaction theory and the theory of underwater sound generation at the ocean surface, the potential calming effect on surface gravity waves by raindrop induced mixing has become important. The rain induced mixed layer was studied with models based on the turbulent kinetic energy budget. A bulk mixed layer model was tuned with laboratory experimental data. The turbulent kinetic energy going into subsurface mixing was found to be less than 10% of the total raindrop kinetic energy. The length scale for mixing is proportional to both raindrop size and rain intensity. Furthermore, there is some indication of an initial penetration depth for raindrops. Although the available data was inadequate to complete model development and verification, a prediction for a hypothetical situation in the North Pacific is proposed. The diffusion processes are illustrated by solving for the diffusion and dissipation terms of the turbulent kinetic energy equation with a finite difference scheme. New experiments are suggested to allow future model development and testing.

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Document Details

Document Type
Technical Report
Publication Date
Jun 01, 1990
Accession Number
ADA238022

Entities

People

  • Hong B. Hur

Organizations

  • Naval Postgraduate School

Tags

Communities of Interest

  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Boundary Layer
  • Diffusion
  • Drops
  • Energy
  • Energy Transfer
  • Equations
  • Experimental Data
  • Gravity Waves
  • Intensity
  • Kinetic Energy
  • Mixing
  • Raindrops
  • Rainfall Intensity
  • Surface Waves
  • Temperature Gradients
  • Turbulent Mixing
  • Waves

Fields of Study

  • Environmental science

Readers

  • Atmospheric Remote Sensing.
  • Combustion science or combustion engineering.
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers