This study assesses the medium‐range flow‐dependent forecast skill of Euro‐Atlantic weather regimes: the positive and negative phases of the North Atlantic Oscillation (NAO+ and NAO−), Atlantic ridge (ATLR), and Euro‐Atlantic blocking (EABL), for extended winters (November–March) in the periods 2006/2007–2013/2014 and 1985/1986–2013/2014 using The Interactive Grand Global Ensemble (TIGGE) and the National Oceanic and Atmospheric Administration (NOAA)'s Global Ensemble Forecasting System (GEFS) reforecast datasets, respectively. The models show greater‐than‐observed (smaller‐than‐observed) frequencies of NAO− and ATLR (NAO+) with forecast lead time. The increased frequency of NAO− is not due to its excess persistence but due to more frequent...
Extra‐tropical cyclones and their associated extreme wind speeds are a major cause of vast damage an...
The variability of the North Atlantic Oscillation is a key aspect of Northern Hemisphere atmospheric...
This study investigates the influence of atmospheric initial conditions on winter seasonal forecasts...
International audienceAbstract. Issuing skillful forecasts beyond the typical horizon of weather pre...
International audienceAbstract. Issuing skillful forecasts beyond the typical horizon of weather pre...
International audienceAbstract. Issuing skillful forecasts beyond the typical horizon of weather pre...
International audienceAbstract. Issuing skillful forecasts beyond the typical horizon of weather pre...
Weather regimes are large-scale atmospheric circulation states that frequently occur in the climate ...
Weather regime forecasts are a prominent use case of sub‐seasonal prediction in the midlatitudes. A ...
Issuing skillful forecasts beyond the typical horizon of weather predictability remains a challenge ...
Weather regimes are large-scale atmospheric circulation states that frequently occur in the climate ...
A key determinant of winter weather and climate in Europe and North America is the North Atlantic Os...
This is the final version. Available from AGU via the DOI in this recordUntil recently, long-range f...
The simulation and prediction of winter Northern Hemisphere atmospheric blocking in the seasonal pre...
The North Atlantic Oscillation (NAO) is the leading mode of variability in the large scale circulati...
Extra‐tropical cyclones and their associated extreme wind speeds are a major cause of vast damage an...
The variability of the North Atlantic Oscillation is a key aspect of Northern Hemisphere atmospheric...
This study investigates the influence of atmospheric initial conditions on winter seasonal forecasts...
International audienceAbstract. Issuing skillful forecasts beyond the typical horizon of weather pre...
International audienceAbstract. Issuing skillful forecasts beyond the typical horizon of weather pre...
International audienceAbstract. Issuing skillful forecasts beyond the typical horizon of weather pre...
International audienceAbstract. Issuing skillful forecasts beyond the typical horizon of weather pre...
Weather regimes are large-scale atmospheric circulation states that frequently occur in the climate ...
Weather regime forecasts are a prominent use case of sub‐seasonal prediction in the midlatitudes. A ...
Issuing skillful forecasts beyond the typical horizon of weather predictability remains a challenge ...
Weather regimes are large-scale atmospheric circulation states that frequently occur in the climate ...
A key determinant of winter weather and climate in Europe and North America is the North Atlantic Os...
This is the final version. Available from AGU via the DOI in this recordUntil recently, long-range f...
The simulation and prediction of winter Northern Hemisphere atmospheric blocking in the seasonal pre...
The North Atlantic Oscillation (NAO) is the leading mode of variability in the large scale circulati...
Extra‐tropical cyclones and their associated extreme wind speeds are a major cause of vast damage an...
The variability of the North Atlantic Oscillation is a key aspect of Northern Hemisphere atmospheric...
This study investigates the influence of atmospheric initial conditions on winter seasonal forecasts...