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    <titleInfo>
        <title>Low-frequency climate variability in the Atlantic basin during the 20th century</title>
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    <name type="personal" ID="ymt1">
        <namePart type="family">Tourre</namePart>
        <namePart type="given">Yves Marcel</namePart>
        <role>
            <roleTerm type="text">author</roleTerm>
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        <affiliation>Columbia University. Lamont-Doherty Earth Observatory</affiliation>
    </name>
    <name type="personal">
        <namePart type="family">Paz</namePart>
        <namePart type="given">Shlomit</namePart>
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        <namePart type="family">Kushnir</namePart>
        <namePart type="given">Yochanan</namePart>
        <role>
            <roleTerm type="text">author</roleTerm>
        </role>
        <affiliation>Columbia University. Lamont-Doherty Earth Observatory</affiliation>
    </name>
    <name type="personal">
        <namePart type="family">White</namePart>
        <namePart type="given">Warren B.</namePart>
        <role>
            <roleTerm type="text">author</roleTerm>
        </role>
    </name>
    <name type="corporate">
        <namePart>Columbia University. Lamont-Doherty Earth Observatory</namePart>
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        <dateIssued encoding="w3cdtf" keyDate="yes">2010</dateIssued>
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    <abstract>From joint sea surface temperature/sea level pressure (SST/SLP) EOF analyses, lowfrequency variability modes are compared. The multi-decadal oscillation (MDO) changed phases twice during the 20th century, with its north Atlantic SST patterns resembling the Atlantic multi-decadal oscillation (AMO). The quasi-decadal oscillation (QDO) SST patterns displayed a double tripole configuration over the entire Atlantic basin, leading to tropical inter-hemispheric out-of-phase relationship. From the mid-1960s onward, while ST anomalies were negative to the north (negative phases of MDO/AMO), the Sahelian drought persisted with a weaker hurricane power dissipation index (PDI). During that period, the QDO modulated the intensity of the Sahelian drought.</abstract>
    <subject>
        <topic>Physical oceanography</topic>
    </subject>
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        <titleInfo>
            <title>Atmospheric Science Letters</title>
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        <part>
            <detail type="volume">
                <number>11</number>
            </detail>
            <detail type="issue">
                <number>3</number>
            </detail>
            <extent unit="page">
                <start>180</start>
                <end>185</end>
            </extent>
            <date>2010</date>
        </part>
        <identifier type="doi">http://dx.doi.org/10.1002/asl.265</identifier>
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    <identifier type="hdl">http://hdl.handle.net/10022/AC:P:15030</identifier>
    
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        <recordIdentifier>9033</recordIdentifier>
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