Serveur d'exploration sur les relations entre la France et l'Australie

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The El Niño–Southern Oscillation and daily temperature extremes in east Asia and the west Pacific

Identifieur interne : 002120 ( Istex/Curation ); précédent : 002119; suivant : 002121

The El Niño–Southern Oscillation and daily temperature extremes in east Asia and the west Pacific

Auteurs : N. Nicholls [Australie] ; H. Baek [Corée du Sud] ; A. Gosai [Nouvelle-Zélande] ; L. E. Chambers [Australie] ; Y. Choi [Corée du Sud] ; D. Collins [Australie] ; P. M. Della-Marta [Suisse] ; G. M. Griffiths [Nouvelle-Zélande] ; M. R. Haylock [Royaume-Uni] ; N. Iga [Papouasie-Nouvelle-Guinée] ; R. Lata [Fidji] ; L. Maitrepierre ; M. J. Manton [Australie] ; H. Nakamigawa [Japon] ; N. Ouprasitwong [Thaïlande] ; D. Solofa [Samoa] ; L. Tahani ; D. T. Thuy [Viêt Nam] ; L. Tibig [Philippines] ; B. Trewin [Australie] ; K. Vediapan [Malaisie] ; P. Zhai [République populaire de Chine]

Source :

RBID : ISTEX:AE9152E2403CEAA24BC837B7D1265752ABF25912

English descriptors

Abstract

The numbers of warm nights and hot days, across most of the east Asia – west Pacific region, increase substantially in the year after the onset of an El Niño event. The number of cool days and cold nights tend to decrease, although the relationship with El Niño is weaker for these variables. The relationship is confounded, for warm nights and hot days, by a strong increasing trend in the numbers of extremes not matched by a trend in the El Niño. Removal of this trend leads to even stronger correlations with the El Niño. Strong correlations exist between some of the extremes indices and an index of the El Niño – Southern Oscillation in months prior to the occurrence of the extremes, indicating that predictions of the frequency of extreme temperatures across the region should be feasible.

Url:
DOI: 10.1029/2005GL022621

Links toward previous steps (curation, corpus...)


Links to Exploration step

ISTEX:AE9152E2403CEAA24BC837B7D1265752ABF25912

Curation

No country items

L. Maitrepierre
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L. Tahani
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Le document en format XML

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<title level="j" type="main">Geophysical Research Letters</title>
<title level="j" type="alt">GEOPHYSICAL RESEARCH LETTERS</title>
<idno type="ISSN">0094-8276</idno>
<idno type="eISSN">1944-8007</idno>
<imprint>
<biblScope unit="vol">32</biblScope>
<biblScope unit="issue">16</biblScope>
<biblScope unit="page-count">4</biblScope>
<date type="published" when="2005-08">2005-08</date>
</imprint>
<idno type="ISSN">0094-8276</idno>
</series>
</biblStruct>
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<idno type="ISSN">0094-8276</idno>
</seriesStmt>
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<keywords scheme="KwdEn" xml:lang="en">
<term>Annual numbers</term>
<term>Annual values</term>
<term>Atmospheric research</term>
<term>Calendar year</term>
<term>Climate extremes</term>
<term>Climate research centre</term>
<term>Climatic research unit</term>
<term>Cold nights</term>
<term>Cool days</term>
<term>Daily data</term>
<term>Daily temperature extremes</term>
<term>Data rescue</term>
<term>Detrended</term>
<term>Detrended data</term>
<term>Detrended number</term>
<term>East anglia</term>
<term>East asia</term>
<term>East asia west</term>
<term>Extreme indices</term>
<term>Extreme temperatures</term>
<term>Extremes indices</term>
<term>Full lines</term>
<term>Global change research</term>
<term>Konkuk university</term>
<term>Manton</term>
<term>Maximum temperature</term>
<term>Meteorological department</term>
<term>Meteorological division</term>
<term>Meteorological research institute</term>
<term>Meteorology research centre</term>
<term>Meteorology research group</term>
<term>Minimum temperature</term>
<term>Monthly values</term>
<term>National institute</term>
<term>Nino</term>
<term>Nino episode</term>
<term>Nino event</term>
<term>Oscillation</term>
<term>Percentile</term>
<term>Petaling jaya</term>
<term>Port moresby</term>
<term>Previous year</term>
<term>Quality control</term>
<term>Quezon city</term>
<term>Solomon islands</term>
<term>Southern oscillation</term>
<term>Strong trend</term>
<term>Stronger correlations</term>
<term>Strongest correlations</term>
<term>Surface temperatures</term>
<term>Temperature data</term>
<term>Temperature extremes</term>
<term>Temperature indices</term>
<term>Thin lines</term>
<term>Time series</term>
<term>Warm nights</term>
<term>Weather service</term>
</keywords>
<keywords scheme="Teeft" xml:lang="en">
<term>Annual numbers</term>
<term>Annual values</term>
<term>Atmospheric research</term>
<term>Calendar year</term>
<term>Climate extremes</term>
<term>Climate research centre</term>
<term>Climatic research unit</term>
<term>Cold nights</term>
<term>Cool days</term>
<term>Daily data</term>
<term>Daily temperature extremes</term>
<term>Data rescue</term>
<term>Detrended</term>
<term>Detrended data</term>
<term>Detrended number</term>
<term>East anglia</term>
<term>East asia</term>
<term>East asia west</term>
<term>Extreme indices</term>
<term>Extreme temperatures</term>
<term>Extremes indices</term>
<term>Full lines</term>
<term>Global change research</term>
<term>Konkuk university</term>
<term>Manton</term>
<term>Maximum temperature</term>
<term>Meteorological department</term>
<term>Meteorological division</term>
<term>Meteorological research institute</term>
<term>Meteorology research centre</term>
<term>Meteorology research group</term>
<term>Minimum temperature</term>
<term>Monthly values</term>
<term>National institute</term>
<term>Nino</term>
<term>Nino episode</term>
<term>Nino event</term>
<term>Oscillation</term>
<term>Percentile</term>
<term>Petaling jaya</term>
<term>Port moresby</term>
<term>Previous year</term>
<term>Quality control</term>
<term>Quezon city</term>
<term>Solomon islands</term>
<term>Southern oscillation</term>
<term>Strong trend</term>
<term>Stronger correlations</term>
<term>Strongest correlations</term>
<term>Surface temperatures</term>
<term>Temperature data</term>
<term>Temperature extremes</term>
<term>Temperature indices</term>
<term>Thin lines</term>
<term>Time series</term>
<term>Warm nights</term>
<term>Weather service</term>
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</teiHeader>
<front>
<div type="abstract">The numbers of warm nights and hot days, across most of the east Asia – west Pacific region, increase substantially in the year after the onset of an El Niño event. The number of cool days and cold nights tend to decrease, although the relationship with El Niño is weaker for these variables. The relationship is confounded, for warm nights and hot days, by a strong increasing trend in the numbers of extremes not matched by a trend in the El Niño. Removal of this trend leads to even stronger correlations with the El Niño. Strong correlations exist between some of the extremes indices and an index of the El Niño – Southern Oscillation in months prior to the occurrence of the extremes, indicating that predictions of the frequency of extreme temperatures across the region should be feasible.</div>
</front>
</TEI>
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