Original paper
Decadal cyclone variability in the North Atlantic
Luksch, Ute; Raible, Christoph C.; Blender, Richard; Fraedrich, Klaus
Meteorologische Zeitschrift Vol. 14 No. 6 (2005), p. 747 - 753
published: Dec 19, 2005
DOI: 10.1127/0941-2948/2005/0075
Open Access (paper may be downloaded free of charge)
Abstract
The unstable midlatitude ocean-atmosphere coupling motivates the definition of two decadal regimes with distinct implications for the North Atlantic cyclone variability. Phases with low (high) decadal variability of the North Atlantic Oscillation, which are connected with an annular (sectoral) spatial scale of the geopotential height teleconnection pattern, are identified as a hemispheric (regional) regime. In the hemispheric regime during a positive El Niño/Southern Oscillation (ENSO) index (warm event), the North Atlantic cyclones and the regions of enhanced precipitation shift southward while over northern Europe the cyclone activity and the rainfall are reduced. During the regional regime this impact of ENSO on the Atlantic storm track is extremely small and a clear interpretation over Europe is inhibited.