Influence of Indian Ocean sea-surface temperature variability on winter rainfall across eastern Australia
Identifieur interne :
001803 ( PascalFrancis/Curation );
précédent :
001802;
suivant :
001804
Influence of Indian Ocean sea-surface temperature variability on winter rainfall across eastern Australia
Auteurs : Danielle C. Verdon [
Australie] ;
Stewart W. Franks [
Australie]
Source :
-
IAHS-AISH publication [ 0144-7815 ] ; 2005.
RBID : Pascal:05-0298586
Descripteurs français
- Pascal (Inist)
- Australie,
Impact,
Climat,
Température,
Eau surface,
Océan Indien,
Précipitation atmosphérique,
Pluie,
El Nino,
Oscillation,
Anomalie,
Variation saisonnière,
Variabilité climatique,
Température surface,
Température superficielle,
ENSO.
- Wicri :
English descriptors
- KwdEn :
- Australia,
El Nino,
Indian Ocean,
anomalies,
atmospheric precipitation,
climate,
impacts,
oscillations,
rainfall,
seasonal variations,
surface water,
temperature.
Abstract
This study investigates the relationship between sea-surface temperature (SST) variability occurring over the Indian Ocean and winter rainfall variability in eastern Australia. Previous research has identified a number of modes of SST variability over the Indian Ocean that may be connected to rainfall variability in Australia. Six indices of SST variability are compared and their relationship to winter rainfall over eastern Australia is determined. It is shown that a strong relationship exists between a number of these indices and winter rainfall. Additionally, this relationship is shown to hold true irrespective of potential impacts on rainfall by the El Niño/Southern Oscillation (ENSO). A possible physical process by which Indian Ocean SST anomalies may influence winter rainfall in eastern Australia is proposed involving impacts on the nature of the Northwest Australian Cloud Band. This study demonstrates marked controls on winter climate variability comparable to that induced in summer by the better known ENSO processes, and hence offers improved understanding of year-round seasonal climates.
pA |
A01 | 01 | 1 | | @0 0144-7815 |
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A05 | | | | @2 295 |
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A08 | 01 | 1 | ENG | @1 Influence of Indian Ocean sea-surface temperature variability on winter rainfall across eastern Australia |
---|
A09 | 01 | 1 | ENG | @1 Regional hydrological impacts of climatic change - impact assessment and decision making : Foz do Iguaço, 3-9 April 2005 |
---|
A11 | 01 | 1 | | @1 VERDON (Danielle C.) |
---|
A11 | 02 | 1 | | @1 FRANKS (Stewart W.) |
---|
A12 | 01 | 1 | | @1 WAGENER (Thorsten) @9 ed. |
---|
A12 | 02 | 1 | | @1 FRANKS (Stewart) @9 ed. |
---|
A12 | 03 | 1 | | @1 GUPTA (Hoshin V.) @9 ed. |
---|
A12 | 04 | 1 | | @1 BOGH (Eva) @9 ed. |
---|
A12 | 05 | 1 | | @1 BASTIDAS (Luis) @9 ed. |
---|
A12 | 06 | 1 | | @1 NOBRE (Carlos) @9 ed. |
---|
A12 | 07 | 1 | | @1 DE OLIVEIRA GALVAO (Carlos) @9 ed. |
---|
A14 | 01 | | | @1 School ofEngineering, University of Newcastle @2 Callaghan, New South Wales 2308 @3 AUS @Z 1 aut. @Z 2 aut. |
---|
A18 | 01 | 1 | | @1 International Association of Hydrological Sciences @2 Paris @3 FRA @9 org-cong. |
---|
A20 | | | | @1 335-345 @7 5 |
---|
A21 | | | | @1 2005 |
---|
A23 | 01 | | | @0 ENG |
---|
A26 | 01 | | | @0 1-901502-08-2 |
---|
A43 | 01 | | | @1 INIST @2 8967 @5 354000124484120360 |
---|
A44 | | | | @0 0000 @1 © 2005 INIST-CNRS. All rights reserved. |
---|
A45 | | | | @0 24 ref. |
---|
A47 | 01 | 1 | | @0 05-0298586 |
---|
A60 | | | | @1 P @2 C |
---|
A61 | | | | @0 A |
---|
A64 | 01 | 1 | | @0 IAHS-AISH publication |
---|
A66 | 01 | | | @0 GBR |
---|
C01 | 01 | | ENG | @0 This study investigates the relationship between sea-surface temperature (SST) variability occurring over the Indian Ocean and winter rainfall variability in eastern Australia. Previous research has identified a number of modes of SST variability over the Indian Ocean that may be connected to rainfall variability in Australia. Six indices of SST variability are compared and their relationship to winter rainfall over eastern Australia is determined. It is shown that a strong relationship exists between a number of these indices and winter rainfall. Additionally, this relationship is shown to hold true irrespective of potential impacts on rainfall by the El Niño/Southern Oscillation (ENSO). A possible physical process by which Indian Ocean SST anomalies may influence winter rainfall in eastern Australia is proposed involving impacts on the nature of the Northwest Australian Cloud Band. This study demonstrates marked controls on winter climate variability comparable to that induced in summer by the better known ENSO processes, and hence offers improved understanding of year-round seasonal climates. |
---|
C02 | 01 | 2 | | @0 223B |
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C02 | 02 | 2 | | @0 226A01 |
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C02 | 03 | 2 | | @0 001E01H |
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C02 | 04 | 2 | | @0 001E01N01 |
---|
C03 | 01 | 2 | FRE | @0 Australie @2 NG @5 01 |
---|
C03 | 01 | 2 | ENG | @0 Australia @2 NG @5 01 |
---|
C03 | 01 | 2 | SPA | @0 Australia @2 NG @5 01 |
---|
C03 | 02 | 2 | FRE | @0 Impact @5 02 |
---|
C03 | 02 | 2 | ENG | @0 impacts @5 02 |
---|
C03 | 03 | 2 | FRE | @0 Climat @5 03 |
---|
C03 | 03 | 2 | ENG | @0 climate @5 03 |
---|
C03 | 03 | 2 | SPA | @0 Clima @5 03 |
---|
C03 | 04 | 2 | FRE | @0 Température @5 04 |
---|
C03 | 04 | 2 | ENG | @0 temperature @5 04 |
---|
C03 | 04 | 2 | SPA | @0 Temperatura @5 04 |
---|
C03 | 05 | 2 | FRE | @0 Eau surface @5 05 |
---|
C03 | 05 | 2 | ENG | @0 surface water @5 05 |
---|
C03 | 05 | 2 | SPA | @0 Agua superficie @5 05 |
---|
C03 | 06 | 2 | FRE | @0 Océan Indien @5 06 |
---|
C03 | 06 | 2 | ENG | @0 Indian Ocean @5 06 |
---|
C03 | 06 | 2 | SPA | @0 Océano Indico @5 06 |
---|
C03 | 07 | 2 | FRE | @0 Précipitation atmosphérique @5 07 |
---|
C03 | 07 | 2 | ENG | @0 atmospheric precipitation @5 07 |
---|
C03 | 07 | 2 | SPA | @0 Precipitación atmosférica @5 07 |
---|
C03 | 08 | 2 | FRE | @0 Pluie @5 08 |
---|
C03 | 08 | 2 | ENG | @0 rainfall @5 08 |
---|
C03 | 08 | 2 | SPA | @0 Lluvia @5 08 |
---|
C03 | 09 | 2 | FRE | @0 El Nino @5 09 |
---|
C03 | 09 | 2 | ENG | @0 El Nino @5 09 |
---|
C03 | 10 | 2 | FRE | @0 Oscillation @5 10 |
---|
C03 | 10 | 2 | ENG | @0 oscillations @5 10 |
---|
C03 | 10 | 2 | SPA | @0 Oscilación @5 10 |
---|
C03 | 11 | 2 | FRE | @0 Anomalie @5 11 |
---|
C03 | 11 | 2 | ENG | @0 anomalies @5 11 |
---|
C03 | 11 | 2 | SPA | @0 Anomalía @5 11 |
---|
C03 | 12 | 2 | FRE | @0 Variation saisonnière @5 14 |
---|
C03 | 12 | 2 | ENG | @0 seasonal variations @5 14 |
---|
C03 | 12 | 2 | SPA | @0 Variación estacional @5 14 |
---|
C03 | 13 | 2 | FRE | @0 Variabilité climatique @4 INC @5 52 |
---|
C03 | 14 | 2 | FRE | @0 Température surface @4 INC @5 53 |
---|
C03 | 15 | 2 | FRE | @0 Température superficielle @4 INC @5 54 |
---|
C03 | 16 | 2 | FRE | @0 ENSO @4 INC @5 55 |
---|
C06 | | | | @0 ILS @0 TAS |
---|
C07 | 01 | 2 | FRE | @0 Australasie |
---|
C07 | 01 | 2 | ENG | @0 Australasia |
---|
C07 | 01 | 2 | SPA | @0 Australasia |
---|
N21 | | | | @1 206 |
---|
N44 | 01 | | | @1 PSI |
---|
N82 | | | | @1 PSI |
---|
|
pR |
A30 | 01 | 1 | ENG | @1 International symposium on regional hydrological impacts of climatic variability and change with an emphasis on less developed countries @3 Foz do Iguaço BRA @4 2005-04-03 |
---|
|
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Pascal:05-0298586
Le document en format XML
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<front><div type="abstract" xml:lang="en">This study investigates the relationship between sea-surface temperature (SST) variability occurring over the Indian Ocean and winter rainfall variability in eastern Australia. Previous research has identified a number of modes of SST variability over the Indian Ocean that may be connected to rainfall variability in Australia. Six indices of SST variability are compared and their relationship to winter rainfall over eastern Australia is determined. It is shown that a strong relationship exists between a number of these indices and winter rainfall. Additionally, this relationship is shown to hold true irrespective of potential impacts on rainfall by the El Niño/Southern Oscillation (ENSO). A possible physical process by which Indian Ocean SST anomalies may influence winter rainfall in eastern Australia is proposed involving impacts on the nature of the Northwest Australian Cloud Band. This study demonstrates marked controls on winter climate variability comparable to that induced in summer by the better known ENSO processes, and hence offers improved understanding of year-round seasonal climates.</div>
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<fC01 i1="01" l="ENG"><s0>This study investigates the relationship between sea-surface temperature (SST) variability occurring over the Indian Ocean and winter rainfall variability in eastern Australia. Previous research has identified a number of modes of SST variability over the Indian Ocean that may be connected to rainfall variability in Australia. Six indices of SST variability are compared and their relationship to winter rainfall over eastern Australia is determined. It is shown that a strong relationship exists between a number of these indices and winter rainfall. Additionally, this relationship is shown to hold true irrespective of potential impacts on rainfall by the El Niño/Southern Oscillation (ENSO). A possible physical process by which Indian Ocean SST anomalies may influence winter rainfall in eastern Australia is proposed involving impacts on the nature of the Northwest Australian Cloud Band. This study demonstrates marked controls on winter climate variability comparable to that induced in summer by the better known ENSO processes, and hence offers improved understanding of year-round seasonal climates.</s0>
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<s5>02</s5>
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<s5>03</s5>
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<s5>03</s5>
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<fC03 i1="03" i2="2" l="SPA"><s0>Clima</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Température</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>temperature</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="SPA"><s0>Temperatura</s0>
<s5>04</s5>
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<s5>05</s5>
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<s5>05</s5>
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<s5>05</s5>
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<s5>06</s5>
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<fC03 i1="06" i2="2" l="ENG"><s0>Indian Ocean</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA"><s0>Océano Indico</s0>
<s5>06</s5>
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<fC03 i1="07" i2="2" l="FRE"><s0>Précipitation atmosphérique</s0>
<s5>07</s5>
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<fC03 i1="07" i2="2" l="ENG"><s0>atmospheric precipitation</s0>
<s5>07</s5>
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<fC03 i1="07" i2="2" l="SPA"><s0>Precipitación atmosférica</s0>
<s5>07</s5>
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<fC03 i1="08" i2="2" l="FRE"><s0>Pluie</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>rainfall</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Lluvia</s0>
<s5>08</s5>
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<fC03 i1="09" i2="2" l="FRE"><s0>El Nino</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>El Nino</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Oscillation</s0>
<s5>10</s5>
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<fC03 i1="10" i2="2" l="ENG"><s0>oscillations</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Oscilación</s0>
<s5>10</s5>
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<fC03 i1="11" i2="2" l="FRE"><s0>Anomalie</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>anomalies</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Anomalía</s0>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Variation saisonnière</s0>
<s5>14</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>seasonal variations</s0>
<s5>14</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Variación estacional</s0>
<s5>14</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Variabilité climatique</s0>
<s4>INC</s4>
<s5>52</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Température surface</s0>
<s4>INC</s4>
<s5>53</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Température superficielle</s0>
<s4>INC</s4>
<s5>54</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>ENSO</s0>
<s4>INC</s4>
<s5>55</s5>
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<fC06><s0>ILS</s0>
<s0>TAS</s0>
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<fC07 i1="01" i2="2" l="FRE"><s0>Australasie</s0>
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<pR><fA30 i1="01" i2="1" l="ENG"><s1>International symposium on regional hydrological impacts of climatic variability and change with an emphasis on less developed countries</s1>
<s3>Foz do Iguaço BRA</s3>
<s4>2005-04-03</s4>
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