Weather Regimes: Recurrence and Quasi Stationarity
Open Access
- 1 April 1995
- journal article
- research article
- Published by American Meteorological Society in Journal of the Atmospheric Sciences
- Vol. 52 (8) , 1237-1256
- https://doi.org/10.1175/1520-0469(1995)052<1237:wrraqs>2.0.co;2
Abstract
Two different definitions of midlatitude weather regimes are compared. The first seeks recurrent atmospheric patterns. The second seeks quasi-stationary patterns, whose average tendency vanishes. Recurrent patterns are identified by cluster analysis, and quasi-stationary patterns are identified by solving a nonlinear equilibration equation. Both methods are applied on the same dataset: the NMC final analyses of 700-hPa geopotential heights covering 44 winters. The analysis is performed separately over the Atlantic and Pacific sectors. The two methods give the same number of weather regimes—four over the Atlantic sector and three over the Pacific sector. However, the patterns differ significantly. The investigation of the tendency, or drift, of the clusters shows that recurrent flows have a systematic slow evolution, explaining this difference. The patterns are in agreement with the ones obtained from previous studies, but their number differs. The cluster analysis algorithm used here is a partiti... Abstract Two different definitions of midlatitude weather regimes are compared. The first seeks recurrent atmospheric patterns. The second seeks quasi-stationary patterns, whose average tendency vanishes. Recurrent patterns are identified by cluster analysis, and quasi-stationary patterns are identified by solving a nonlinear equilibration equation. Both methods are applied on the same dataset: the NMC final analyses of 700-hPa geopotential heights covering 44 winters. The analysis is performed separately over the Atlantic and Pacific sectors. The two methods give the same number of weather regimes—four over the Atlantic sector and three over the Pacific sector. However, the patterns differ significantly. The investigation of the tendency, or drift, of the clusters shows that recurrent flows have a systematic slow evolution, explaining this difference. The patterns are in agreement with the ones obtained from previous studies, but their number differs. The cluster analysis algorithm used here is a partiti...Keywords
This publication has 8 references indexed in Scilit:
- Empirical Normal-Mode Analysis of Atmospheric DataJournal of the Atmospheric Sciences, 1994
- Cluster Analysis of the Northern Hemisphere Wintertime 500-hPa Height Field: Spatial PatternsJournal of the Atmospheric Sciences, 1993
- Multiple Flow Regimes in the Northern Hemisphere Winter. Part II: Sectorial Regimes and Preferred TransitionsJournal of the Atmospheric Sciences, 1993
- Multiple Flow Regimes in the Northern Hemisphere Winter. Part I: Methodology and Hemispheric RegimesJournal of the Atmospheric Sciences, 1993
- Multiple Weather Regimes over the North Atlantic: Analysis of Precursors and SuccessorsMonthly Weather Review, 1990
- Cluster analysis of multiple planetary flow regimesJournal of Geophysical Research: Atmospheres, 1988
- Retrograding Wintertime Low-Frequency Disturbances over the North Pacific OceanJournal of the Atmospheric Sciences, 1987
- Blocking Action in the Middle Troposphere and its Effect upon Regional ClimateTellus, 1950