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
Original language | English (US) |
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Pages (from-to) | 7245-7258 |
Number of pages | 14 |
Journal | Journal of Geophysical Research |
Volume | 89 |
Issue number | D5 |
DOIs | |
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