HEAT ABSORPTION AND HEAT BUDGET AT OCEAN STATION ECHO, SEPTEMBER 1959.

Abstract

Between 2 and 21 September 1959, approximately 900 bathythermograph observations (BT's) were obtained at Ocean Weather Station ECHO (35 deg N, 48 deg W). In addition, incoming radiation from sun and sky and reflected radiation from the sea surface were recorded. By grouping the BT data according to cloud amount, mean hourly temperatures were obtained. Estimates of heat absorption, evaporation and changes in horizontal heat content (advection) for clear, partly cloudy, and cloudy skies were derived from these mean temperatures. The ocean was assumed to be neither gaining nor losing heat during this season of the year. For clear skies, evaporative heat loss exceeded long wave (back radiation) heat loss; for cloudy skies, condensation resulted in a net gain of heat. Hourly mean temperatures and temperature gradients are presented. Surface temperature was changed about 0.1 deg F by evaporative heat flux and a comparable amount by horizontal heat flux. (Author)

Document Details

Document Type
Technical Report
Publication Date
Jan 01, 1967
Accession Number
AD0814063

Entities

People

  • Edward L. Corton

Organizations

  • Naval Oceanographic Office

Tags

DTIC Thesaurus Topics

  • Absorption
  • Enthalpy
  • Heat Energy
  • Heat Flux
  • Heat Loss
  • Isotherms
  • Losses
  • Radiation
  • Stations
  • Surface Temperature
  • Temperature Gradients
  • Transition Temperature
  • Weather Stations

Fields of Study

  • Environmental science

Readers

  • Atmospheric Remote Sensing.
  • Exercise and Sports Science.
  • Oceanography.