Variability in the location of the Antarctic Polar Front (90°-20°W) from satellite sea surface temperature data

The path of the Antarctic Polar Front (PF) is mapped using satellite sea surface temperature data from the NOAA/NASA Pathfinder program. The mean path and variability of the PF are strongly influenced by bathymetry. Meandering intensity is weaker where the bathymetry is steeply sloped and increases...

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Bibliographic Details
Published in:Journal of Geophysical Research: Oceans
Main Authors: Moore, J. Keith, Abbott, Mark R, Richman, James G
Format: Article in Journal/Newspaper
Language:English
Published: eScholarship, University of California 1997
Subjects:
Physical Sciences and Mathematics
southern-ocean
circumpolar current
drake passage
temporal variability
circulation
altimetry
atlantic
africa
Antarctic
Drake Passage
Ewing
Falkland Plateau
Southern Ocean
The Antarctic
Antarc*
Online Access:http://www.escholarship.org/uc/item/9989q7rb
Description
Summary:The path of the Antarctic Polar Front (PF) is mapped using satellite sea surface temperature data from the NOAA/NASA Pathfinder program. The mean path and variability of the PF are strongly influenced by bathymetry. Meandering intensity is weaker where the bathymetry is steeply sloped and increases in areas where the bottom is relatively flat. There is an inverse relationship between meandering intensity and both the width of the front and the change in temperature across it There is a persistent, large separation between the surface and subsurface expressions of the PF at Ewing Bank on the Falkland Plateau.

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