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GEOPHYSICAL RESEARCH LETTERS,
VOL. 26, NO. 11,
PAGES 1621–1624,
1999
Atmospheric Patterns Forcing Two Regimes of Arctic Circulation: A Return to Anticyclonic Conditions?
Mark A. Johnson
Institute of Marine Science, University of Alaska Fairbanks, Fairbanks, Alaska
Andrey Y. Proshutinsky
Institute of Marine Science, University of Alaska Fairbanks, Fairbanks, Alaska
Igor V. Polyakov
Institute of Marine Science, University of Alaska Fairbanks, Fairbanks, Alaska
Abstract
Atmospheric sea level pressure (SLP) patterns associated with two regimes of ice-ocean circulation are identified by sorting
the data into bins depending on whether modeled Arctic Ocean circulation was anticyclonic or cyclonic. The transition between
regimes is a zonally symmetric SLP cell with maximum amplitude at the north pole. From 1946 to 1997, four anticyclonic and
four cyclonic regimes track the Arctic Ocean SLP oscillation. Recent SLP data suggest that the ocean-atmosphere system will
shift, or has already shifted, to an anticyclonic state.
Received 21
December
1998;
accepted 30
March
1999.
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Citation: Johnson, M. A., A. Y. Proshutinsky, and I. V. Polyakov
(1999),
Atmospheric Patterns Forcing Two Regimes of Arctic Circulation: A Return to Anticyclonic Conditions?,
Geophys. Res. Lett.,
26(11),
1621–1624.
Copyright 1999 by the American Geophysical Union.
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