<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-04-13T01:17:24Z</responseDate><request verb="GetRecord" identifier="oai:www.recercat.cat:2117/114139" metadataPrefix="marc">https://recercat.cat/oai/request</request><GetRecord><record><header><identifier>oai:recercat.cat:2117/114139</identifier><datestamp>2026-02-02T08:57:00Z</datestamp><setSpec>com_2072_1033</setSpec><setSpec>col_2072_452950</setSpec></header><metadata><record xmlns="http://www.loc.gov/MARC21/slim" xmlns:dcterms="http://purl.org/dc/terms/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.loc.gov/MARC21/slim http://www.loc.gov/standards/marcxml/schema/MARC21slim.xsd">
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      <subfield code="a">dc</subfield>
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   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">Volpi, Danila</subfield>
      <subfield code="e">author</subfield>
   </datafield>
   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">Guemas, Virginie</subfield>
      <subfield code="e">author</subfield>
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   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">Doblas-Reyes, Francisco</subfield>
      <subfield code="e">author</subfield>
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      <subfield code="c">2017-08</subfield>
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      <subfield code="a">Decadal prediction exploits sources of predictability from both the internal variability through the initialisation of the climate model from observational estimates, and the external radiative forcings. When a model is initialised with the observed state at the initial time step (Full Field Initialisation—FFI), the forecast run drifts towards the biased model climate. Distinguishing between the climate signal to be predicted and the model drift is a challenging task, because the application of a-posteriori bias correction has the risk of removing part of the variability signal. The anomaly initialisation (AI) technique aims at addressing the drift issue by answering the following question: if the model is allowed to start close to its own attractor (i.e. its biased world), but the phase of the simulated variability is constrained toward the contemporaneous observed one at the initialisation time, does the prediction skill improve? The relative merits of the FFI and AI techniques applied respectively to the ocean component and the ocean and sea ice components simultaneously in the EC-Earth global coupled model are assessed. For both strategies the initialised hindcasts show better skill than historical simulations for the ocean heat content and AMOC along the first two forecast years, for sea ice and PDO along the first forecast year, while for AMO the improvements are statistically significant for the first two forecast years. The AI in the ocean and sea ice components significantly improves the skill of the Arctic sea surface temperature over the FFI.</subfield>
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      <subfield code="a">The authors acknowledge funding support for&#xd;
this study from the SPECS (ENV-2012-308378) project funded by the&#xd;
Seventh Framework Programme (FP7) of the European Commission&#xd;
and the PICA-ICE (CGL2012-31987) project funded by the Ministry&#xd;
of Economy and Competitiveness of Spain. The authors thankfully&#xd;
acknowledge the computer resources, technical expertise and assistance&#xd;
provided by the Red Española de Supercomputación through&#xd;
the Barcelona Supercomputing Center.</subfield>
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      <subfield code="a">Peer Reviewed</subfield>
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      <subfield code="a">Postprint (author's final draft)</subfield>
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   <datafield tag="653" ind2=" " ind1=" ">
      <subfield code="a">Àrees temàtiques de la UPC::Energies</subfield>
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      <subfield code="a">Climate science</subfield>
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   <datafield tag="653" ind2=" " ind1=" ">
      <subfield code="a">Seasonal prediction (Meteorology)</subfield>
   </datafield>
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      <subfield code="a">Decadal climate prediction</subfield>
   </datafield>
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      <subfield code="a">Full field initialisation</subfield>
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      <subfield code="a">Anomaliy initialisation</subfield>
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      <subfield code="a">Global coupled model</subfield>
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      <subfield code="a">Previsió del temps</subfield>
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      <subfield code="a">Comparison of full field and anomaly initialisation for decadal climate prediction: towards an optimal consistency between the ocean and sea-ice anomaly initialisation state</subfield>
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