A Study of Cloud Patterns Observed from ESSA 3 Satellite Photographs and their Relationship to Sea Surface Temperatures in the Eastern Gulf of Mexico.

Abstract

Cloud patterns in the eastern Gulf of Mexico are the result of frontal systems, terrestrial radiation, atmospheric motions, and thermal differences between sea surface and the adjacent air masses. ESSA 3 weather satellite photographs reveal temperature patterns of the surface oceanic environment by the presence or absence of cumulus type clouds during atmospheric calm periods. Relatively cool water under warm air causes cumulus cloud development, while relatively warm water under cool air causes dissipation of low clouds. Remote sensors and high altitude cloud photographs can present real-time, synoptic coverage of ocean surface temperatures provided that accurate ground-truth temperatures are incorporated with data. (Author)

Document Details

Document Type
Technical Report
Publication Date
Oct 01, 1968
Accession Number
AD0854007

Entities

People

  • William T. Morton

Organizations

  • Naval Oceanographic Office

Tags

Communities of Interest

  • Space

DTIC Thesaurus Topics

  • Air Masses
  • Altitude
  • Artificial Satellites
  • Atmospheric Motion
  • Clouds
  • Cumulus Clouds
  • High Altitude
  • Photographs
  • Radiation
  • Remote Detectors
  • Sea Surface Temperature
  • Surface Temperature
  • Terrestrial Radiation
  • Transition Temperature

Fields of Study

  • Environmental science

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Computer Vision.
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers

Technology Areas

  • Space