Atmosphere- sea ice interactions in the Beaufort/ Chukchi Sea and in the European sector of the Arctic.

Research output: Contribution to journalArticle

12 Citations (Scopus)

Abstract

Electrically Scanning Microwave Radiometer data for 'winter' months, November 1973 to April 1974, and for 'summer', May to October 1974, are used to examine the synoptic scale sea ice-atmosphere interactions. The synoptic scale variability in the microwave brightness temperatures and sea level atmospheric pressure and temperature is examined through the use of principal components analysis. Changes occurring in the ice ablation season are found to be responsible for much of the variance in the data.-from Author

Original languageEnglish (US)
Pages (from-to)4505-4523
Number of pages19
JournalJournal of Geophysical Research
Volume88
Issue numberC7
DOIs
StatePublished - Jan 1 1983

Fingerprint

Chukchi Sea
Beaufort Sea (North America)
Sea ice
sea ice
Arctic region
ice
sectors
Microwaves
Atmospheric temperature
atmospheres
microwave radiometers
atmospheric temperature
atmosphere
brightness temperature
atmospheric pressure
Sea level
microwave radiometer
Ice
sea level pressure
Radiometers

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Forestry
  • Oceanography
  • Aquatic Science
  • Ecology
  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth-Surface Processes
  • Atmospheric Science
  • Space and Planetary Science
  • Earth and Planetary Sciences (miscellaneous)
  • Palaeontology

Cite this

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Atmosphere- sea ice interactions in the Beaufort/ Chukchi Sea and in the European sector of the Arctic. / Crane, Robert George.

In: Journal of Geophysical Research, Vol. 88, No. C7, 01.01.1983, p. 4505-4523.

Research output: Contribution to journalArticle

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AB - Electrically Scanning Microwave Radiometer data for 'winter' months, November 1973 to April 1974, and for 'summer', May to October 1974, are used to examine the synoptic scale sea ice-atmosphere interactions. The synoptic scale variability in the microwave brightness temperatures and sea level atmospheric pressure and temperature is examined through the use of principal components analysis. Changes occurring in the ice ablation season are found to be responsible for much of the variance in the data.-from Author

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