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GEOPHYSICAL RESEARCH LETTERS,
VOL. 30, NO. 18,
1934,
doi:10.1029/2003GL017290,
2003
Regional and hemispheric circulation patterns in the northern hemisphere winter, or the NAO and the AO
Kunihiko Kodera
Meteorological Research Institute, Tsukuba, Ibaraki, Japan
Yuhji Kuroda
Meteorological Research Institute, Tsukuba, Ibaraki, Japan
Abstract
Two different scales of teleconnection patterns are found over the Euro-Atlantic region during the winter. One is a regional
seesaw between Iceland and the Azores, and the other is a hemispheric seesaw between the Mediterranean and the polar-Siberia
region. The North Atlantic Oscillation (NAO) and the Arctic Oscillation (AO) indices are sensitive to both modes, although
the NAO index reflects the more regional one. The principal process producing a hemispheric seesaw pattern in the surface
pressure is changing in vertical winds in the polar troposphere driven by wave forcings. Upward motion in the polar region
induces meridional flows near the surface, especially around the Norwegian Sea and Bering Strait, which induce wavy patterns
in the surface pressure. The importance of distinguishing the two modes in understanding recent trends is also addressed.
Received 8
April
2003;
accepted 16
June
2003;
published 20
September
2003.
Index Terms: 1620 Global Change: Climate dynamics (3309); 1610 Global Change: Atmosphere (0315, 0325); 3319 Meteorology and Atmospheric Dynamics: General circulation; 3349 Meteorology and Atmospheric Dynamics: Polar meteorology.
Read Full Article (file size: 544430 bytes) Cited by
Citation: Kodera, K., and Y. Kuroda
(2003),
Regional and hemispheric circulation patterns in the northern hemisphere winter, or the NAO and the AO,
Geophys. Res. Lett.,
30(18),
1934,
doi:10.1029/2003GL017290.
Copyright 2003 by the American Geophysical Union.
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