<?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>2026-05-29T21:23:42Z</responseDate><request verb="GetRecord" identifier="oai:riuma.uma.es:10630/33463" metadataPrefix="marc">https://riuma.uma.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:riuma.uma.es:10630/33463</identifier><datestamp>2026-02-03T10:57:09Z</datestamp><setSpec>com_10630_2254</setSpec><setSpec>col_10630_37953</setSpec></header><metadata><record xmlns="http://www.loc.gov/MARC21/slim" xmlns:dcterms="http://purl.org/dc/terms/" xmlns:doc="http://www.lyncode.com/xoai" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.loc.gov/MARC21/slim http://www.loc.gov/standards/marcxml/schema/MARC21slim.xsd">
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   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">Ayarzagüena, Blanca</subfield>
      <subfield code="e">author</subfield>
   </datafield>
   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">López Parages, Jorge</subfield>
      <subfield code="e">author</subfield>
   </datafield>
   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">Iza, Madalen</subfield>
      <subfield code="e">author</subfield>
   </datafield>
   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">Calvo, Natalia</subfield>
      <subfield code="e">author</subfield>
   </datafield>
   <datafield ind2=" " ind1=" " tag="720">
      <subfield code="a">Rodríguez de Fonseca, Belén</subfield>
      <subfield code="e">author</subfield>
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   <datafield ind2=" " ind1=" " tag="260">
      <subfield code="c">2018-04-02</subfield>
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      <subfield code="a">The European precipitation response to El Niño (EN) has been found to present interdecadal changes, with alternated periods&#xd;
of important or negligible EN impact in late winter. These periods are associated with opposite phases of multi-decadal sea&#xd;
surface temperature (SST) variability, which modifies the tropospheric background and EN teleconnections. In addition,&#xd;
other studies have shown how SST anomalies in the equatorial Pacific, and in particular, the location of the largest anomalous&#xd;
SST, modulate the stratospheric response to EN. Nevertheless, the role of the stratosphere on the stationarity of EN response&#xd;
has not been investigated in detail so far. Using reanalysis data, we present a comprehensive study of EN teleconnections to&#xd;
Europe including the role of the ocean background and the stratosphere in the stationarity of the signal. The results reveal&#xd;
multidecadal variability in the location of EN-related SST anomalies that determines different teleconnections. In periods&#xd;
with relevant precipitation signal over Europe, the EN SST pattern resembles Eastern Pacific EN and the stratospheric&#xd;
pathway plays a key role in transmitting the signal to Europe in February, together with two tropospheric wavetrains that&#xd;
transmit the signal in February and April. Conversely, the stratospheric pathway is not detected in periods with a weak EN&#xd;
impact on European precipitation, corresponding to EN-related SST anomalies primarily located over the central Pacific.&#xd;
SST mean state and its associated atmospheric background control the location of EN-related SST anomalies in different&#xd;
periods and modulate the establishment of the aforementioned stratospheric pathway of EN teleconnection to Europe too.</subfield>
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   <datafield ind1="8" ind2=" " tag="024">
      <subfield code="a">Ayarzagüena, B., López-Parages, J., Iza, M. et al. Stratospheric role in interdecadal changes of El Niño impacts over Europe. Clim Dyn 52, 1173–1186 (2019). https://doi.org/10.1007/s00382-018-4186-3</subfield>
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      <subfield code="a">https://hdl.handle.net/10630/33463</subfield>
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   <datafield ind1="8" ind2=" " tag="024">
      <subfield code="a">10.1007/s00382-018-4186-3</subfield>
   </datafield>
   <datafield tag="653" ind2=" " ind1=" ">
      <subfield code="a">El Niño (Corriente marina)</subfield>
   </datafield>
   <datafield tag="653" ind2=" " ind1=" ">
      <subfield code="a">Precipitaciones atmosféricas - Europa</subfield>
   </datafield>
   <datafield tag="653" ind2=" " ind1=" ">
      <subfield code="a">Estratosfera</subfield>
   </datafield>
   <datafield ind2="0" ind1="0" tag="245">
      <subfield code="a">Stratospheric role in interdecadal changes of El Niño impacts over Europe.</subfield>
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