Multi-decadal variability of rainfall and streamflow across eastern Australia
Identifieur interne :
001816 ( PascalFrancis/Curation );
précédent :
001815;
suivant :
001817
Multi-decadal variability of rainfall and streamflow across eastern Australia
Auteurs : Danielle C. Verdon [
Australie] ;
Adam M. Wyatt [
Australie] ;
Anthony S. Kiem [
Australie] ;
Stewart W. Franks [
Australie]
Source :
-
IAHS-AISH publication [ 0144-7815 ] ; 2005.
RBID : Pascal:05-0305480
Descripteurs français
- Pascal (Inist)
- Australie,
Nouvelle Galles du Sud,
Précipitation atmosphérique,
Pluie,
Ecoulement cours eau,
El Nino,
Oscillation,
Océan Pacifique,
Variabilité climatique,
ENSO,
La Nina.
- Wicri :
English descriptors
Abstract
This study investigates the influence of the El Niño/Southern Oscillation (ENSO) and the Interdecadal Pacific Oscillation (IPO) on rainfall and streamflow regimes of eastern Australia. An analysis of historical rainfall and streamflow data for Queensland (QLD), New South Wales (NSW) and Victoria (VIC) reveals strong relationships between these indices and seasonal rainfall and streamflow totals. Rainfall and streamflow in NSW and QLD are shown to be significantly enhanced during the La Niña phase of ENSO, with La Niña impacts diminishing as one moves south into VIC. In addition, the study shows that on a multi-decadal time scale, the negative phase of the IPO is associated with "wetter" conditions than the positive phase. Importantly, the already enhanced La Niña rainfall and streamflow is demonstrated to be even further magnified during La Niña events that occur in the IPO negative phase. The results also indicate that some useful predictability of ENSO impacts can be achieved during the negative phase of the IPO for VIC.
| pA |
| A01 | 01 | 1 | | @0 0144-7815 |
|---|
| A05 | | | | @2 296 |
|---|
| A08 | 01 | 1 | ENG | @1 Multi-decadal variability of rainfall and streamflow across eastern Australia |
|---|
| A09 | 01 | 1 | ENG | @1 Regional hydrological impacts of climatic change - hydroclimatic variability : Foz do Iguaço, 3-9 April 2005 |
|---|
| A11 | 01 | 1 | | @1 VERDON (Danielle C.) |
|---|
| A11 | 02 | 1 | | @1 WYATT (Adam M.) |
|---|
| A11 | 03 | 1 | | @1 KIEM (Anthony S.) |
|---|
| A11 | 04 | 1 | | @1 FRANKS (Stewart W.) |
|---|
| A12 | 01 | 1 | | @1 FRANKS (Stewart) @9 ed. |
|---|
| A12 | 02 | 1 | | @1 WAGENER (Thorsten) @9 ed. |
|---|
| A12 | 03 | 1 | | @1 BOGH (Eva) @9 ed. |
|---|
| A12 | 04 | 1 | | @1 GUPTA (Hoshin V.) @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 of Engineering, University of Newcastle @2 Callaghan, New South Wales 2308 @3 AUS @Z 1 aut. @Z 2 aut. @Z 3 aut. @Z 4 aut. |
|---|
| A18 | 01 | 1 | | @1 International Association of Hydrological Sciences @2 Paris @3 FRA @9 org-cong. |
|---|
| A20 | | | | @1 42-52 @7 1 |
|---|
| A21 | | | | @1 2005 |
|---|
| A23 | 01 | | | @0 ENG |
|---|
| A26 | 01 | | | @0 1-901502-13-9 |
|---|
| A43 | 01 | | | @1 INIST @2 8967 @5 354000124484790040 |
|---|
| A44 | | | | @0 0000 @1 © 2005 INIST-CNRS. All rights reserved. |
|---|
| A45 | | | | @0 23 ref. |
|---|
| A47 | 01 | 1 | | @0 05-0305480 |
|---|
| 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 influence of the El Niño/Southern Oscillation (ENSO) and the Interdecadal Pacific Oscillation (IPO) on rainfall and streamflow regimes of eastern Australia. An analysis of historical rainfall and streamflow data for Queensland (QLD), New South Wales (NSW) and Victoria (VIC) reveals strong relationships between these indices and seasonal rainfall and streamflow totals. Rainfall and streamflow in NSW and QLD are shown to be significantly enhanced during the La Niña phase of ENSO, with La Niña impacts diminishing as one moves south into VIC. In addition, the study shows that on a multi-decadal time scale, the negative phase of the IPO is associated with "wetter" conditions than the positive phase. Importantly, the already enhanced La Niña rainfall and streamflow is demonstrated to be even further magnified during La Niña events that occur in the IPO negative phase. The results also indicate that some useful predictability of ENSO impacts can be achieved during the negative phase of the IPO for VIC. |
|---|
| C02 | 01 | 2 | | @0 226A01 |
|---|
| C02 | 02 | 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 Nouvelle Galles du Sud @2 NG @5 02 |
|---|
| C03 | 02 | 2 | ENG | @0 New South Wales @2 NG @5 02 |
|---|
| C03 | 02 | 2 | SPA | @0 Nueva Gales del Sur @2 NG @5 02 |
|---|
| C03 | 03 | 2 | FRE | @0 Précipitation atmosphérique @5 03 |
|---|
| C03 | 03 | 2 | ENG | @0 atmospheric precipitation @5 03 |
|---|
| C03 | 03 | 2 | SPA | @0 Precipitación atmosférica @5 03 |
|---|
| C03 | 04 | 2 | FRE | @0 Pluie @5 06 |
|---|
| C03 | 04 | 2 | ENG | @0 rainfall @5 06 |
|---|
| C03 | 04 | 2 | SPA | @0 Lluvia @5 06 |
|---|
| C03 | 05 | 2 | FRE | @0 Ecoulement cours eau @5 07 |
|---|
| C03 | 05 | 2 | ENG | @0 streamflow @5 07 |
|---|
| C03 | 06 | 2 | FRE | @0 El Nino @5 08 |
|---|
| C03 | 06 | 2 | ENG | @0 El Nino @5 08 |
|---|
| C03 | 07 | 2 | FRE | @0 Oscillation @5 09 |
|---|
| C03 | 07 | 2 | ENG | @0 oscillations @5 09 |
|---|
| C03 | 07 | 2 | SPA | @0 Oscilación @5 09 |
|---|
| C03 | 08 | 2 | FRE | @0 Océan Pacifique @5 11 |
|---|
| C03 | 08 | 2 | ENG | @0 Pacific Ocean @5 11 |
|---|
| C03 | 08 | 2 | SPA | @0 Océano Pacífico @5 11 |
|---|
| C03 | 09 | 2 | FRE | @0 Variabilité climatique @4 INC @5 52 |
|---|
| C03 | 10 | 2 | FRE | @0 ENSO @4 INC @5 53 |
|---|
| C03 | 11 | 2 | FRE | @0 La Nina @4 INC @5 54 |
|---|
| C06 | | | | @0 ILS @0 TA |
|---|
| C07 | 01 | 2 | FRE | @0 Australasie |
|---|
| C07 | 01 | 2 | ENG | @0 Australasia |
|---|
| C07 | 01 | 2 | SPA | @0 Australasia |
|---|
| N21 | | | | @1 213 |
|---|
| 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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Le document en format XML
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<author><name sortKey="Verdon, Danielle C" sort="Verdon, Danielle C" uniqKey="Verdon D" first="Danielle C." last="Verdon">Danielle C. Verdon</name>
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<s2>Callaghan, New South Wales 2308</s2>
<s3>AUS</s3>
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</publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Multi-decadal variability of rainfall and streamflow across eastern Australia</title>
<author><name sortKey="Verdon, Danielle C" sort="Verdon, Danielle C" uniqKey="Verdon D" first="Danielle C." last="Verdon">Danielle C. Verdon</name>
<affiliation wicri:level="1"><inist:fA14 i1="01"><s1>School of Engineering, University of Newcastle</s1>
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</affiliation><author><name sortKey="Wyatt, Adam M" sort="Wyatt, Adam M" uniqKey="Wyatt A" first="Adam M." last="Wyatt">Adam M. Wyatt</name>
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</inist:fA14><country>Australie</country>
</affiliation><author><name sortKey="Kiem, Anthony S" sort="Kiem, Anthony S" uniqKey="Kiem A" first="Anthony S." last="Kiem">Anthony S. Kiem</name>
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<sZ>4 aut.</sZ>
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</affiliation><author><name sortKey="Franks, Stewart W" sort="Franks, Stewart W" uniqKey="Franks S" first="Stewart W." last="Franks">Stewart W. Franks</name>
<affiliation wicri:level="1"><inist:fA14 i1="01"><s1>School of Engineering, University of Newcastle</s1>
<s2>Callaghan, New South Wales 2308</s2>
<s3>AUS</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
</inist:fA14><country>Australie</country>
</affiliation><series><title level="j" type="main">IAHS-AISH publication</title>
<idno type="ISSN">0144-7815</idno>
<imprint><date when="2005">2005</date>
</imprint><seriesStmt><title level="j" type="main">IAHS-AISH publication</title>
<idno type="ISSN">0144-7815</idno>
</seriesStmt><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Australia</term>
<term>El Nino</term>
<term>New South Wales</term>
<term>Pacific Ocean</term>
<term>atmospheric precipitation</term>
<term>oscillations</term>
<term>rainfall</term>
<term>streamflow</term>
</keywords><keywords scheme="Pascal" xml:lang="fr"><term>Australie</term>
<term>Nouvelle Galles du Sud</term>
<term>Précipitation atmosphérique</term>
<term>Pluie</term>
<term>Ecoulement cours eau</term>
<term>El Nino</term>
<term>Oscillation</term>
<term>Océan Pacifique</term>
<term>Variabilité climatique</term>
<term>ENSO</term>
<term>La Nina</term>
</keywords><keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>Australie</term>
</keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Océan Pacifique</term>
</keywords><front><div type="abstract" xml:lang="en">This study investigates the influence of the El Niño/Southern Oscillation (ENSO) and the Interdecadal Pacific Oscillation (IPO) on rainfall and streamflow regimes of eastern Australia. An analysis of historical rainfall and streamflow data for Queensland (QLD), New South Wales (NSW) and Victoria (VIC) reveals strong relationships between these indices and seasonal rainfall and streamflow totals. Rainfall and streamflow in NSW and QLD are shown to be significantly enhanced during the La Niña phase of ENSO, with La Niña impacts diminishing as one moves south into VIC. In addition, the study shows that on a multi-decadal time scale, the negative phase of the IPO is associated with "wetter" conditions than the positive phase. Importantly, the already enhanced La Niña rainfall and streamflow is demonstrated to be even further magnified during La Niña events that occur in the IPO negative phase. The results also indicate that some useful predictability of ENSO impacts can be achieved during the negative phase of the IPO for VIC.</div>
</front><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0144-7815</s0>
</fA01><fA05><s2>296</s2>
</fA05><fA08 i1="01" i2="1" l="ENG"><s1>Multi-decadal variability of rainfall and streamflow across eastern Australia</s1>
</fA08><fA09 i1="01" i2="1" l="ENG"><s1>Regional hydrological impacts of climatic change - hydroclimatic variability : Foz do Iguaço, 3-9 April 2005</s1>
</fA09><fA11 i1="01" i2="1"><s1>VERDON (Danielle C.)</s1>
</fA11><fA11 i1="02" i2="1"><s1>WYATT (Adam M.)</s1>
</fA11><fA11 i1="03" i2="1"><s1>KIEM (Anthony S.)</s1>
</fA11><fA11 i1="04" i2="1"><s1>FRANKS (Stewart W.)</s1>
</fA11><fA12 i1="01" i2="1"><s1>FRANKS (Stewart)</s1>
<s9>ed.</s9>
</fA12><fA12 i1="02" i2="1"><s1>WAGENER (Thorsten)</s1>
<s9>ed.</s9>
</fA12><fA12 i1="03" i2="1"><s1>BOGH (Eva)</s1>
<s9>ed.</s9>
</fA12><fA12 i1="04" i2="1"><s1>GUPTA (Hoshin V.)</s1>
<s9>ed.</s9>
</fA12><fA12 i1="05" i2="1"><s1>BASTIDAS (Luis)</s1>
<s9>ed.</s9>
</fA12><fA12 i1="06" i2="1"><s1>NOBRE (Carlos)</s1>
<s9>ed.</s9>
</fA12><fA12 i1="07" i2="1"><s1>DE OLIVEIRA GALVAO (Carlos)</s1>
<s9>ed.</s9>
</fA12><fA14 i1="01"><s1>School of Engineering, University of Newcastle</s1>
<s2>Callaghan, New South Wales 2308</s2>
<s3>AUS</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
</fA14><fA18 i1="01" i2="1"><s1>International Association of Hydrological Sciences</s1>
<s2>Paris</s2>
<s3>FRA</s3>
<s9>org-cong.</s9>
</fA18><fA20><s1>42-52</s1>
<s7>1</s7>
</fA20><fA21><s1>2005</s1>
</fA21><fA23 i1="01"><s0>ENG</s0>
</fA23><fA26 i1="01"><s0>1-901502-13-9</s0>
</fA26><fA43 i1="01"><s1>INIST</s1>
<s2>8967</s2>
<s5>354000124484790040</s5>
</fA43><fA44><s0>0000</s0>
<s1>© 2005 INIST-CNRS. All rights reserved.</s1>
</fA44><fA45><s0>23 ref.</s0>
</fA45><fA47 i1="01" i2="1"><s0>05-0305480</s0>
</fA47><fA60><s1>P</s1>
<s2>C</s2>
</fA60><fA64 i1="01" i2="1"><s0>IAHS-AISH publication</s0>
</fA64><fA66 i1="01"><s0>GBR</s0>
</fA66><fC01 i1="01" l="ENG"><s0>This study investigates the influence of the El Niño/Southern Oscillation (ENSO) and the Interdecadal Pacific Oscillation (IPO) on rainfall and streamflow regimes of eastern Australia. An analysis of historical rainfall and streamflow data for Queensland (QLD), New South Wales (NSW) and Victoria (VIC) reveals strong relationships between these indices and seasonal rainfall and streamflow totals. Rainfall and streamflow in NSW and QLD are shown to be significantly enhanced during the La Niña phase of ENSO, with La Niña impacts diminishing as one moves south into VIC. In addition, the study shows that on a multi-decadal time scale, the negative phase of the IPO is associated with "wetter" conditions than the positive phase. Importantly, the already enhanced La Niña rainfall and streamflow is demonstrated to be even further magnified during La Niña events that occur in the IPO negative phase. The results also indicate that some useful predictability of ENSO impacts can be achieved during the negative phase of the IPO for VIC.</s0>
</fC01><fC02 i1="01" i2="2"><s0>226A01</s0>
</fC02><fC02 i1="02" i2="2"><s0>001E01N01</s0>
</fC02><fC03 i1="01" i2="2" l="FRE"><s0>Australie</s0>
<s2>NG</s2>
<s5>01</s5>
</fC03><fC03 i1="01" i2="2" l="ENG"><s0>Australia</s0>
<s2>NG</s2>
<s5>01</s5>
</fC03><fC03 i1="01" i2="2" l="SPA"><s0>Australia</s0>
<s2>NG</s2>
<s5>01</s5>
</fC03><fC03 i1="02" i2="2" l="FRE"><s0>Nouvelle Galles du Sud</s0>
<s2>NG</s2>
<s5>02</s5>
</fC03><fC03 i1="02" i2="2" l="ENG"><s0>New South Wales</s0>
<s2>NG</s2>
<s5>02</s5>
</fC03><fC03 i1="02" i2="2" l="SPA"><s0>Nueva Gales del Sur</s0>
<s2>NG</s2>
<s5>02</s5>
</fC03><fC03 i1="03" i2="2" l="FRE"><s0>Précipitation atmosphérique</s0>
<s5>03</s5>
</fC03><fC03 i1="03" i2="2" l="ENG"><s0>atmospheric precipitation</s0>
<s5>03</s5>
</fC03><fC03 i1="03" i2="2" l="SPA"><s0>Precipitación atmosférica</s0>
<s5>03</s5>
</fC03><fC03 i1="04" i2="2" l="FRE"><s0>Pluie</s0>
<s5>06</s5>
</fC03><fC03 i1="04" i2="2" l="ENG"><s0>rainfall</s0>
<s5>06</s5>
</fC03><fC03 i1="04" i2="2" l="SPA"><s0>Lluvia</s0>
<s5>06</s5>
</fC03><fC03 i1="05" i2="2" l="FRE"><s0>Ecoulement cours eau</s0>
<s5>07</s5>
</fC03><fC03 i1="05" i2="2" l="ENG"><s0>streamflow</s0>
<s5>07</s5>
</fC03><fC03 i1="06" i2="2" l="FRE"><s0>El Nino</s0>
<s5>08</s5>
</fC03><fC03 i1="06" i2="2" l="ENG"><s0>El Nino</s0>
<s5>08</s5>
</fC03><fC03 i1="07" i2="2" l="FRE"><s0>Oscillation</s0>
<s5>09</s5>
</fC03><fC03 i1="07" i2="2" l="ENG"><s0>oscillations</s0>
<s5>09</s5>
</fC03><fC03 i1="07" i2="2" l="SPA"><s0>Oscilación</s0>
<s5>09</s5>
</fC03><fC03 i1="08" i2="2" l="FRE"><s0>Océan Pacifique</s0>
<s5>11</s5>
</fC03><fC03 i1="08" i2="2" l="ENG"><s0>Pacific Ocean</s0>
<s5>11</s5>
</fC03><fC03 i1="08" i2="2" l="SPA"><s0>Océano Pacífico</s0>
<s5>11</s5>
</fC03><fC03 i1="09" i2="2" l="FRE"><s0>Variabilité climatique</s0>
<s4>INC</s4>
<s5>52</s5>
</fC03><fC03 i1="10" i2="2" l="FRE"><s0>ENSO</s0>
<s4>INC</s4>
<s5>53</s5>
</fC03><fC03 i1="11" i2="2" l="FRE"><s0>La Nina</s0>
<s4>INC</s4>
<s5>54</s5>
</fC03><fC06><s0>ILS</s0>
<s0>TA</s0>
</fC06><fC07 i1="01" i2="2" l="FRE"><s0>Australasie</s0>
</fC07><fC07 i1="01" i2="2" l="ENG"><s0>Australasia</s0>
</fC07><fC07 i1="01" i2="2" l="SPA"><s0>Australasia</s0>
</fC07><fN21><s1>213</s1>
</fN21><fN44 i1="01"><s1>PSI</s1>
</fN44><fN82><s1>PSI</s1>
</fN82><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>
</fA30>
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|wiki= Wicri/Asie
|area= AustralieFrV1
|flux= PascalFrancis
|étape= Curation
|type= RBID
|clé= Pascal:05-0305480
|texte= Multi-decadal variability of rainfall and streamflow across eastern Australia
}}
| This area was generated with Dilib version V0.6.33.
Data generation: Tue Dec 5 10:43:12 2017. Site generation: Tue Mar 5 14:07:20 2024 |  |
