ACCURACY OF SEA SURFACE TEMPERATURE ANALYSIS-PART I.

Abstract

Five sea surface temperature analyses (Fleet Numerical Weather Facility, Monterey; Fleet Weather Facility, Norfolk; NAVOCEANO 15-day composite; H. O. 225 Atlas; and a historical chart) are compared with surface temperatures obtained on a recent airborne radiation thermometer flight. The flight from Halifax, Nova Scotia, to Patuxent River, Maryland, was made under conditions of clear skies and with sufficient wind to mix the surface film. Fleet Weather Facility, Norfolk and the NAVOCEANO composite analysis proved most reliable with mean absolute errors of 3.7 F and 3.6 F, respectively. These charts were also considered more useful in that they show details such as countercurrents, the north wall of the Gulf Stream, and other high gradient areas. A May 1965 mean monthly sea surface temperature chart was used as a historical chart and had an error of 3.8 F. The Atlas and Monterey's charts had errors of 5.3 F and 9.6 F, respectively. By elimination of bias, errors were reduced on all analyses; Fleet Weather Facility showing the smallest error, 3.2 F. It is concluded that considerable improvement can still be realized in sea surface temperatture analyses once sufficient data of a reliable nature are available. With present data input, the Fleet Weather Facility manually prepared, subjective chart provides the most reliable sea surface temperature information for the ASWEPS area. (Author)

Document Details

Document Type
Technical Report
Publication Date
Aug 01, 1966
Accession Number
AD0489639

Entities

People

  • Richard W. James

Organizations

  • Naval Oceanographic Office

Tags

DTIC Thesaurus Topics

  • Accuracy
  • Airborne
  • Composite Materials
  • Elimination
  • Errors
  • Gulf Stream
  • Isotherms
  • Maryland
  • Nova Scotia
  • Radiation
  • Sea Surface Temperature
  • Surface Temperature
  • Temperature Gradients
  • Thermometers

Fields of Study

  • Environmental science

Readers

  • Atmospheric Science/Meteorology
  • Geodesy
  • Oceanography.