<?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>2026-05-27T05:24:15Z</responseDate><request verb="GetRecord" identifier="oai:riuma.uma.es:10630/7034" metadataPrefix="marc">https://riuma.uma.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:riuma.uma.es:10630/7034</identifier><datestamp>2026-02-03T11:22:36Z</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">Báez Barrionuevo, José Carlos</subfield>
      <subfield code="e">author</subfield>
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      <subfield code="a">Gimeno, L.</subfield>
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      <subfield code="a">Gómez-Gesteira, M.</subfield>
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      <subfield code="a">Ferri-Yáñez, F.</subfield>
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      <subfield code="a">Real-Giménez, Raimundo</subfield>
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   <datafield ind2=" " ind1=" " tag="260">
      <subfield code="c">2013-04-18</subfield>
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      <subfield code="a">We explored the possible effects of the North Atlantic Oscillation (NAO) and Arctic Oscillation (AO) on interannual sea&#xd;
surface temperature (SST) variations in the Albora´n Sea, both separately and combined. The probability of observing mean&#xd;
annual SST values higher than average was related to NAO and AO values of the previous year. The effect of NAO on SST&#xd;
was negative, while that of AO was positive. The pure effects of NAO and AO on SST are obscuring each other, due to the&#xd;
positive correlation between them. When decomposing SST, NAO and AO in seasonal values, we found that variation in&#xd;
mean annual SST and mean winter SST was significantly related to the mean autumn NAO of the previous year, while mean&#xd;
summer SST was related to mean autumn AO of the previous year. The one year delay in the effect of the NAO and AO on&#xd;
the SST could be partially related to the amount of accumulated snow, as we found a significant correlation between the&#xd;
total snow in the North Albora´n watershed for a year with the annual average SST of the subsequent year. A positive AO&#xd;
implies a colder atmosphere in the Polar Regions, which could favour occasional cold waves over the Iberian Peninsula&#xd;
which, when coupled with precipitations favoured by a negative NAO, may result in snow precipitation. This snow may be&#xd;
accumulated in the high peaks and melt down in spring-summer of the following year, which consequently increases the&#xd;
runoff of freshwater to the sea, which in turn causes a diminution of sea surface salinity and density, and blocks the local&#xd;
upwelling of colder water, resulting in a higher SST.</subfield>
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   <datafield ind1="8" ind2=" " tag="024">
      <subfield code="a">Baéz JC, Gimeno L, Gómez-Gesteira M, Ferri-Yáñez F, Real R (2013) Combined Effects of the North Atlantic Oscillation and the Arctic Oscillation on Sea Surface Temperature in the Albora´n Sea. PLoS ONE 8(4): e62201. doi:10.1371/journal.pone.0062201</subfield>
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      <subfield code="a">1932-6203</subfield>
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   <datafield ind1="8" ind2=" " tag="024">
      <subfield code="a">http://hdl.handle.net/10630/7034</subfield>
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   <datafield tag="653" ind2=" " ind1=" ">
      <subfield code="a">Temperatura - Cambios globales</subfield>
   </datafield>
   <datafield tag="653" ind2=" " ind1=" ">
      <subfield code="a">Mares y océanos - Temperatura - Alborán</subfield>
   </datafield>
   <datafield ind2="0" ind1="0" tag="245">
      <subfield code="a">Combined Effects of the North Atlantic Oscillation and the Arctic Oscillation on Sea Surface Temperature in the Alborán Sea</subfield>
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