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Link between autumnal Arctic Sea ice and Northern Hemisphere winter forecast skill

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10.1029/2019GL086753
 
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Acosta Navarro, Juan CamiloMés informació
Ortega, Pablo
Batté, Lauriane
Smith, Doug
Bretonnière, Pierre-AntoineMés informació
Guemas, Virginie
Massonnet, François
Sicardi, ValentinaMés informació
Torralba, Veronica
Tourigny, EtienneMés informació
Doblas-Reyes, FranciscoMés informació
Document typeArticle
Defense date2020-02-28
PublisherAmerican Geophysical Union (AGU)
Rights accessOpen Access
All rights reserved. This work is protected by the corresponding intellectual and industrial property rights. Without prejudice to any existing legal exemptions, reproduction, distribution, public communication or transformation of this work are prohibited without permission of the copyright holder
ProjectAPPLICATE - Advanced Prediction in Polar regions and beyond: Modelling, observing system design and LInkages associated with ArctiC ClimATE change (EC-H2020-727862)
PRIMAVERA - PRocess-based climate sIMulation: AdVances in high resolution modelling and European climate Risk Assessment (EC-H2020-641727)
INTAROS - Integrated Arctic observation system (EC-H2020-727890)
SPFireSD - Seasonal Prediction of Fire danger using Statistical and Dynamical models (EC-H2020-748750)
Abstract
Dynamical forecast systems have low to moderate skill in continental winter predictions in the extratropics. Here we assess the multimodel predictive skill over Northern Hemisphere high latitudes and midlatitudes using four state‐of‐the‐art forecast systems. Our main goal was to quantify the impact of the Arctic sea ice state during November on the sea level pressure (SLP), surface temperature, and precipitation skill during the following winter. Interannual variability of the November Barents and Kara Sea ice is associated with an important fraction of December to February (DJF) prediction skill in regions of Eurasia. We further show that skill related to sea ice in these regions is accompanied with enhanced skill of DJF SLP in western Russia, established by a sea ice‐atmosphere teleconnection mechanism. The teleconnection is strongest when atmospheric blocking conditions in Scandinavia/western Russia in November reduce a systematic SLP bias that is present in all systems.
CitationAcosta Navarro, J. C. [et al.]. Link between autumnal Arctic Sea ice and Northern Hemisphere winter forecast skill. "Geophysical Research Letters", 28 Febrer 2020, vol. 47, p. 1-9. 
URIhttp://hdl.handle.net/2117/185324
DOI10.1029/2019GL086753
Publisher versionhttps://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2019GL086753
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