<?xml version="1.0" encoding="UTF-8"?>
<modsCollection xmlns="http://www.loc.gov/mods/v3" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-3.xsd">
  <mods>
    <titleInfo>
      <title>Sub-seasonal forcing drives year-to-year variations of Southern Ocean primary productivity</title>
    </titleInfo>
    <name type="personnal">
      <namePart type="family">Prend</namePart>
      <namePart type="given">C. J.</namePart>
      <role>
        <roleTerm type="text">auteur</roleTerm>
        <roleTerm type="code" authority="marcrelator">aut</roleTerm>
      </role>
      <affiliation>IRD</affiliation>
    </name>
    <name type="personnal">
      <namePart type="family">Keerthi</namePart>
      <namePart type="given">M. G.</namePart>
      <role>
        <roleTerm type="text">auteur</roleTerm>
        <roleTerm type="code" authority="marcrelator">aut</roleTerm>
      </role>
      <affiliation>IRD</affiliation>
    </name>
    <name type="personnal">
      <namePart type="family">Levy</namePart>
      <namePart type="given">Marina</namePart>
      <role>
        <roleTerm type="text">auteur</roleTerm>
        <roleTerm type="code" authority="marcrelator">aut</roleTerm>
      </role>
      <affiliation>IRD</affiliation>
    </name>
    <name type="personnal">
      <namePart type="family">Aumont</namePart>
      <namePart type="given">Olivier</namePart>
      <role>
        <roleTerm type="text">auteur</roleTerm>
        <roleTerm type="code" authority="marcrelator">aut</roleTerm>
      </role>
      <affiliation>IRD</affiliation>
    </name>
    <name type="personnal">
      <namePart type="family">Gille</namePart>
      <namePart type="given">S. T.</namePart>
      <role>
        <roleTerm type="text">auteur</roleTerm>
        <roleTerm type="code" authority="marcrelator">aut</roleTerm>
      </role>
      <affiliation>IRD</affiliation>
    </name>
    <name type="personnal">
      <namePart type="family">Talley</namePart>
      <namePart type="given">L. D.</namePart>
      <role>
        <roleTerm type="text">auteur</roleTerm>
        <roleTerm type="code" authority="marcrelator">aut</roleTerm>
      </role>
      <affiliation>IRD</affiliation>
    </name>
    <typeOfResource>text</typeOfResource>
    <genre authority="local">journalArticle</genre>
    <language>
      <languageTerm type="code" authority="iso639-2b">eng</languageTerm>
    </language>
    <physicalDescription>
      <internetMediaType>text/pdf</internetMediaType>
      <digitalOrigin>reformatted digital</digitalOrigin>
      <reformattingQuality>access</reformattingQuality>
    </physicalDescription>
    <abstract>Primary productivity in the Southern Ocean plays a key role in global biogeochemical cycles. While much focus has been placed on phytoplankton production seasonality, non-seasonal fluctuations exceed the amplitude of the seasonal cycle across large swaths of the Antarctic Circumpolar Current. This non-seasonal variability comprises a broad range of timescales from sub-seasonal (&lt;3 months) to multi-annual (&gt;1 year), all of which can project onto the annual mean value. However, year-to-year variations of surface chlorophyll (SChl), a proxy for phytoplankton biomass, are typically attributed to ocean circulation changes associated with the Southern Annular Mode (SAM), which implicitly assumes that sub-seasonal variability averages to near-zero over long timescales. Here, we test this assumption by applying a timeseries decomposition method to satellite-derived SChl in order to separate the low-frequency and high-frequency contributions to the non-seasonal variability. We find that throughout most of the Southern Ocean, year-to-year SChl variations are dominated by the sub-seasonal component, which is not strongly correlated with the SAM. The multi-annual component, while correlated with the SAM, only accounts for about 10% of the total SChl variance. This suggests that changes in annual mean SChl are related to intermittent forcing at small scales, rather than low-frequency climate variability, and thus do not remain correlated over large regions.</abstract>
    <targetAudience authority="marctarget">specialized</targetAudience>
    <subject authority="local">
      <geographic>OCEAN AUSTRAL</geographic>
    </subject>
    <classification authority="local">021</classification>
    <classification authority="local">036</classification>
    <classification authority="local">126</classification>
    <relatedItem type="host">
      <titleInfo>
        <title>Global Biogeochemical Cycles</title>
      </titleInfo>
      <part>
        <detail type="volume">
          <number>36</number>
        </detail>
        <detail type="volume">
          <number>7</number>
        </detail>
        <extent unit="pages">
          <list> e2022GB007329 [15 p.]</list>
        </extent>
      </part>
      <originInfo>
        <dateIssued>2022</dateIssued>
      </originInfo>
      <identifier type="issn">0886-6236</identifier>
    </relatedItem>
    <identifier type="uri">https://www.documentation.ird.fr/hor/fdi:010085334</identifier>
    <identifier type="doi">10.1029/2022gb007329</identifier>
    <identifier type="issn">0886-6236</identifier>
    <location>
      <shelfLocator>[F B010085334]</shelfLocator>
      <url usage="primary display" access="object in context">https://www.documentation.ird.fr/hor/fdi:010085334</url>
      <url access="row object">https://horizon.documentation.ird.fr/exl-doc/pleins_textes/2022-09/010085334.pdf</url>
    </location>
    <recordInfo>
      <recordContentSource>IRD - Base Horizon / Pleins textes</recordContentSource>
      <recordCreationDate encoding="w3cdtf">2022-09-02</recordCreationDate>
      <recordChangeDate encoding="w3cdtf">2025-02-24</recordChangeDate>
      <recordIdentifier>fdi:010085334</recordIdentifier>
      <languageOfCataloging>
        <languageTerm authority="iso639-2b">fre</languageTerm>
      </languageOfCataloging>
    </recordInfo>
  </mods>
</modsCollection>
