Synoptic sea ice - atmosphere interactions in the Chukchi and Beaufort seas from Nimbus 5 ESMR data.

Andrew Mark Carleton

doi:10.1029/JD089iD05p07245

Synoptic sea ice - atmosphere interactions in the Chukchi and Beaufort seas from Nimbus 5 ESMR data.

Andrew Mark Carleton

Geography

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5 Scopus citations

Abstract

Three case studies are used to evaluate the interactions between individual synoptic events and the sea ice cover of parts of the western Arctic. Stong anticyclonic conditions are associated with relatively static surface brightness temperatures (T_B) and hence with generally stable ice conditions. Conversely, a quasi-stationary cyclonic system produces marked T_B variations involving rapid changes in ice edge position and ice concentrations.-from Author

Original language	English (US)
Pages (from-to)	7245-7258
Number of pages	14
Journal	Journal of Geophysical Research
Volume	89
Issue number	D5
DOIs	https://doi.org/10.1029/JD089iD05p07245
State	Published - Jan 1 1984

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

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10.1029/JD089iD05p07245

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title = "Synoptic sea ice - atmosphere interactions in the Chukchi and Beaufort seas from Nimbus 5 ESMR data.",

abstract = "Three case studies are used to evaluate the interactions between individual synoptic events and the sea ice cover of parts of the western Arctic. Stong anticyclonic conditions are associated with relatively static surface brightness temperatures (TB) and hence with generally stable ice conditions. Conversely, a quasi-stationary cyclonic system produces marked TB variations involving rapid changes in ice edge position and ice concentrations.-from Author",

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N2 - Three case studies are used to evaluate the interactions between individual synoptic events and the sea ice cover of parts of the western Arctic. Stong anticyclonic conditions are associated with relatively static surface brightness temperatures (TB) and hence with generally stable ice conditions. Conversely, a quasi-stationary cyclonic system produces marked TB variations involving rapid changes in ice edge position and ice concentrations.-from Author

AB - Three case studies are used to evaluate the interactions between individual synoptic events and the sea ice cover of parts of the western Arctic. Stong anticyclonic conditions are associated with relatively static surface brightness temperatures (TB) and hence with generally stable ice conditions. Conversely, a quasi-stationary cyclonic system produces marked TB variations involving rapid changes in ice edge position and ice concentrations.-from Author

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JO - Journal of Geophysical Research

JF - Journal of Geophysical Research

SN - 0148-0227

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ER -

Synoptic sea ice - atmosphere interactions in the Chukchi and Beaufort seas from Nimbus 5 ESMR data.

Abstract

All Science Journal Classification (ASJC) codes

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