Multiyear climate predictions using two initialization strategies

Multiyear climate predictions with two initialization strategies are systematically assessed in the EC‒Earth V2.3 climate model. In one ensemble, an estimate of the observed climate state is used to initialize the model. The other uses estimates of observed ocean and sea ice anomalies on top of the...

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Published inGeophysical research letters Vol. 40; no. 9; pp. 1794 - 1798
Main Authors Hazeleger, W., Guemas, V., Wouters, B., Corti, S., Andreu‒Burillo, I., Doblas‒Reyes, F. J., Wyser, K., Caian, M.
Format Journal Article
LanguageEnglish
Published Washington Blackwell Publishing Ltd 16.05.2013
John Wiley & Sons, Inc
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Summary:Multiyear climate predictions with two initialization strategies are systematically assessed in the EC‒Earth V2.3 climate model. In one ensemble, an estimate of the observed climate state is used to initialize the model. The other uses estimates of observed ocean and sea ice anomalies on top of the model climatology. The ensembles show similar spatial characteristics of drift related to the biases in control simulations. As expected, the drift is less with anomaly initialization. The full field initialization overshoots to a colder state which is related to cold biases in the tropics and North Atlantic, associated with oceanic processes. Despite different amplitude of the drift, both ensembles show similar skill in multiyear global temperature predictions, but regionally differences are found. On multiyear time scales, initialization with observations enhances both deterministic and probabilistic skill scores in the North Atlantic. The probabilistic verification shows skill over the European continent. Key Points Multiyear climate variability is predictable Different initialization strategies give similar results There is scope for probabilistic predictability in Europe
Bibliography:istex:692D630F8F76070F1FE37869539E1CB58525C7FB
RUCSS - No. CGL2010‒20657
ark:/67375/WNG-QDZ596DS-8
ArticleID:GRL50355
COMBINE - No. 226520
THOR - No. 212643
QWeCI - No. 243964
CLIM‒RUN - No. 265192
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0094-8276
1944-8007
DOI:10.1002/grl.50355