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JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 108, NO. D1,
4036,
doi:10.1029/2002JD002754,
2003
North Pacific–North Atlantic relationships under stratospheric control?
J. M. Castanheira
Department of Physics,
University of Aveiro,
Aveiro,
Portugal
H.-F. Graf
Max-Planck Institute for Meteorology,
Hamburg,
Germany
Abstract
Based on a linear regression/correlation analysis of monthly mean atmospheric sea level pressure (SLP) data from the National
Centers for Environmental Prediction (NCEP) reanalysis (1948–2000), we find a significant anticorrelation between pressure
in the northern North Atlantic and North Pacific only if the stratospheric circulation is in the “strong polar vortex” regime
but not when the vortex is weak. Since some general circulation models (GCMs) (e.g., European Center/Hamburg (ECHAM4)) are
biased toward the strong vortex regime (SVR), they tend to reproduce this anticorrelation already in the mean. The pattern
of the “Arctic Oscillation” (AO) is shown to be consistent with the mean surface pressure differences between the two stratospheric
regimes. The typical SW-NE tilt of the node line of the North Atlantic Oscillation (NAO) found with linear analyses (i.e.,
with such that do not take the regime character of the stratospheric circulation into account) in Northern Hemisphere winter
is due to a superposition of correlation patterns based on physical processes working in the troposphere (a strictly meridional
dipole and the pattern resulting from planetary wave refraction in the strong vortex regime) and those produced by the rapid
transition from one stratospheric regime to the other with subsequent downward propagation of the signal. This result underlines
the necessity of the application of nonlinear statistics or the restriction of linear statistics to variations in the stable
(quasi-linear) environment of natural regimes.
Published 15
January
2003.
Index Terms: 3309 Meteorology and Atmospheric Dynamics: Climatology (1620); 3319 Meteorology and Atmospheric Dynamics: General circulation; 3362 Meteorology and Atmospheric Dynamics: Stratosphere/troposphere interactions; 3384 Meteorology and Atmospheric Dynamics: Waves and tides.
Read Full Article (file size: 1881981 bytes) Cited by
Citation: Castanheira, J. M., and H.-F. Graf
(2003),
North Pacific–North Atlantic relationships under stratospheric control?,
J. Geophys. Res.,
108(D1),
4036,
doi:10.1029/2002JD002754.
Copyright 2003 by the American Geophysical Union.
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