Evaporation Duct Height Measurements in the Mid-Atlantic,

Abstract

Atmospheric boundary layer measurements were made in the Mid-Atlantic aboard USNS KANE during February and March 1978. The results were analyzed to obtain Monin-Obukhov similarity parameters and EM wave train propagation characteristics within the evaporation ducts that overlay the sea surface. Evaporation duct heights (Z*) varied between 2 and 25 meters during the cruise; the mean Z* value was 15 meters. In one instance, Z* changed from 3 meters to 20 meters in about 4 hours following a frontal passage. A comparison of the results obtained using a simplified 'bulk method' with those yielded by the established (but technically taxing) 'profile method' did not convincingly establish that the bulk method could consistently predict accurate values of Z*. Two factors predominate in controlling the duct height Z*: they are relative humidity and the air-sea temperature difference. Barring the development of radical new measurement techniques, the results of this work indicate that a program for routinely measuring Z* is most likely to be obstructed by shortfalls in the quality of air-sea temperature difference data. (Author)

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Document Details

Document Type
Technical Report
Publication Date
Aug 01, 1978
Accession Number
ADA091851

Entities

People

  • Christopher W. Fairall
  • G. E. Schacher
  • K. L. Davidson
  • T. M. Houlihan

Organizations

  • Naval Oceanographic Office

Tags

Communities of Interest

  • Ground and Sea Platforms
  • Materials and Manufacturing Processes
  • Sensors

DTIC Thesaurus Topics

  • Air Temperature
  • Analyzers
  • Boundary Layer
  • Data Analysis
  • Detectors
  • Environment
  • Hot Wire
  • Instrumentation
  • Measurement
  • Meteorological Data
  • Meteorology
  • Plastic Explosives
  • Recording Systems
  • Sea Surface Temperature
  • Surface Temperature
  • Water Vapor
  • Wind Velocity

Fields of Study

  • Environmental science

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Geodesy
  • Wave Propagation and Nonlinear Chaotic Dynamics.