Multiple Weather Regimes over the North Atlantic: Analysis of Precursors and Successors
Open Access
- 1 October 1990
- journal article
- research article
- Published by American Meteorological Society in Monthly Weather Review
- Vol. 118 (10) , 2056-2081
- https://doi.org/10.1175/1520-0493(1990)118<2056:mwrotn>2.0.co;2
Abstract
The algorithm developed by Vautard and Legras is applied to a series of 37 winter of 700 mb geopotential height observations, in order to identify quasi-stationary patterns occurring over the extratropical North Atlantic area. Weather regimes are obtained as solutions of a act of nine nonlinear statistical equations, giving the balance of the large-scale average tendency. Four regime patterns are found. The first one exhibits the typical European blocking dipole. The second one is an enhanced zonal flow. The third one consists of a positive anomaly over Greenland, and the last one is characterized by a ridge over the eastern Atlantic Ocean. The role played by the transient small scales in the maintenance of thew four regimes is discussed. Next, the backward and forward memory times of the different weather regimes are established. Evidence is brought that the atmosphere keeps its memory of regime occurrences into the medium range (10–20 days). Backward memory times are shorter (5–10 days), showin... Abstract The algorithm developed by Vautard and Legras is applied to a series of 37 winter of 700 mb geopotential height observations, in order to identify quasi-stationary patterns occurring over the extratropical North Atlantic area. Weather regimes are obtained as solutions of a act of nine nonlinear statistical equations, giving the balance of the large-scale average tendency. Four regime patterns are found. The first one exhibits the typical European blocking dipole. The second one is an enhanced zonal flow. The third one consists of a positive anomaly over Greenland, and the last one is characterized by a ridge over the eastern Atlantic Ocean. The role played by the transient small scales in the maintenance of thew four regimes is discussed. Next, the backward and forward memory times of the different weather regimes are established. Evidence is brought that the atmosphere keeps its memory of regime occurrences into the medium range (10–20 days). Backward memory times are shorter (5–10 days), showin...This publication has 5 references indexed in Scilit:
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