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

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Broadening the Spatial Applicability of Paleoclimate Information-A Case Study for the Murray-Darling Basin, Australia

Identifieur interne : 005C66 ( PascalFrancis/Curation ); précédent : 005C65; suivant : 005C67

Broadening the Spatial Applicability of Paleoclimate Information-A Case Study for the Murray-Darling Basin, Australia

Auteurs : Michelle Ho [Australie] ; Danielle C. Verdon-Kidd [Australie] ; Anthony S. Kiem [Australie] ; Russell N. Drysdale [Australie, France]

Source :

RBID : Pascal:14-0270569

Descripteurs français

English descriptors

Abstract

Recent advances in the collection and analysis of paleoclimate data have provided significant insights into preinstrumental environmental events and processes, enabling a greater understanding of long-term environmental change and associated hydroclimatic risks. Unfortunately, it is often the case that there is a dearth of readily available paleoclimate data from regions where such insights and long-term data are most needed. The Murray-Darling basin (MDB), known as Australia's "food bowl," is an example of such a region where currently there are very limited in situ paleoclimate data available. While previous studies have utilized paleoclimate proxy records of large-scale climate mechanisms to infer preinstrumental MDB hydroclimatic variability, there is a lack of studies that utilize Australian terrestrial proxy records to garner similar information. Given the immediate need for improved understanding of MDB hydroclimatic variability, this paper identifies key locations in Australia where existing and as yet unrealized paleoclimate records will be most useful in reconstructing such information. To identify these key locations, rainfall relationships between MDB and non-MDB locations were explored through correlations and principal component analysis. An objective analysis using optimal interpolation was then used to pinpoint the most strategic locations to further develop proxy records and gain insights into the benefits of obtaining this additional information. The findings reveal that there is potential for the future assembly of high-resolution paleoclimate records in Australia capable of informing MDB rainfall variability, in particular southeast Australia and central-northern Australia. This study highlights the need for further investment in the development of these potential proxy sources to subsequently enable improved assessments of long-term hydroclimatic risks.
pA  
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A08 01  1  ENG  @1 Broadening the Spatial Applicability of Paleoclimate Information-A Case Study for the Murray-Darling Basin, Australia
A11 01  1    @1 HO (Michelle)
A11 02  1    @1 VERDON-KIDD (Danielle C.)
A11 03  1    @1 KIEM (Anthony S.)
A11 04  1    @1 DRYSDALE (Russell N.)
A14 01      @1 Environmental and Climate Change Research Group, Faculty of Science and Information Technology, The University of Newcastle @2 Callaghan, New South Wales @3 AUS @Z 1 aut. @Z 2 aut. @Z 3 aut.
A14 02      @1 Department of Resource Management and Geography, The University of Melbourne @2 Melbourne, Victoria @3 AUS @Z 4 aut.
A14 03      @1 Laboratoire EDYTEM-UMR4204, Université de Savoie @2 Le Bourget-du-Lac @3 FRA @Z 4 aut.
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C01 01    ENG  @0 Recent advances in the collection and analysis of paleoclimate data have provided significant insights into preinstrumental environmental events and processes, enabling a greater understanding of long-term environmental change and associated hydroclimatic risks. Unfortunately, it is often the case that there is a dearth of readily available paleoclimate data from regions where such insights and long-term data are most needed. The Murray-Darling basin (MDB), known as Australia's "food bowl," is an example of such a region where currently there are very limited in situ paleoclimate data available. While previous studies have utilized paleoclimate proxy records of large-scale climate mechanisms to infer preinstrumental MDB hydroclimatic variability, there is a lack of studies that utilize Australian terrestrial proxy records to garner similar information. Given the immediate need for improved understanding of MDB hydroclimatic variability, this paper identifies key locations in Australia where existing and as yet unrealized paleoclimate records will be most useful in reconstructing such information. To identify these key locations, rainfall relationships between MDB and non-MDB locations were explored through correlations and principal component analysis. An objective analysis using optimal interpolation was then used to pinpoint the most strategic locations to further develop proxy records and gain insights into the benefits of obtaining this additional information. The findings reveal that there is potential for the future assembly of high-resolution paleoclimate records in Australia capable of informing MDB rainfall variability, in particular southeast Australia and central-northern Australia. This study highlights the need for further investment in the development of these potential proxy sources to subsequently enable improved assessments of long-term hydroclimatic risks.
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C03 01  X  FRE  @0 Hydroclimatologie @5 01
C03 01  X  ENG  @0 Hydroclimatology @5 01
C03 01  X  SPA  @0 Hidroclimatología @5 01
C03 02  X  FRE  @0 Reconstruction historique @5 02
C03 02  X  ENG  @0 Historical reconstruction @5 02
C03 02  X  SPA  @0 Reconstrucción histórico @5 02
C03 03  X  FRE  @0 Siècle 20eme @5 03
C03 03  X  ENG  @0 Century 20th @5 03
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C03 04  2  FRE  @0 Bassin versant @5 04
C03 04  2  ENG  @0 drainage basins @5 04
C03 04  2  SPA  @0 Cuenca @5 04
C03 05  2  FRE  @0 Précipitation atmosphérique @5 05
C03 05  2  ENG  @0 atmospheric precipitation @5 05
C03 05  2  SPA  @0 Precipitación atmosférica @5 05
C03 06  2  FRE  @0 Pluie @5 06
C03 06  2  ENG  @0 rainfall @5 06
C03 06  2  SPA  @0 Lluvia @5 06
C03 07  2  FRE  @0 Variabilité climatique @5 07
C03 07  2  ENG  @0 climate variability @5 07
C03 08  X  FRE  @0 Analyse corrélation @5 08
C03 08  X  ENG  @0 Correlation analysis @5 08
C03 08  X  SPA  @0 Análisis correlación @5 08
C03 09  2  FRE  @0 Analyse composante principale @5 09
C03 09  2  ENG  @0 principal components analysis @5 09
C03 09  2  SPA  @0 Análisis componente principal @5 09
C03 10  X  FRE  @0 Interpolation optimale @5 10
C03 10  X  ENG  @0 Optimum interpolation @5 10
C03 10  X  SPA  @0 Interpolación óptima @5 10
C03 11  X  FRE  @0 Analyse objective @5 11
C03 11  X  ENG  @0 Objective analysis @5 11
C03 11  X  SPA  @0 Análisis objetivos @5 11
C03 12  3  FRE  @0 Evaluation risque @5 12
C03 12  3  ENG  @0 Risk assessment @5 12
C03 13  X  FRE  @0 Long terme @5 13
C03 13  X  ENG  @0 Long term @5 13
C03 13  X  SPA  @0 Largo plazo @5 13
C03 14  2  FRE  @0 Bassin Murray @2 NG @5 21
C03 14  2  ENG  @0 Murray Basin @2 NG @5 21
C03 14  2  SPA  @0 Cuenca Murray @2 NG @5 21
C03 15  X  FRE  @0 Gestion risque @5 41
C03 15  X  ENG  @0 Risk management @5 41
C03 15  X  SPA  @0 Gestión riesgo @5 41
C03 16  2  FRE  @0 Indicateur @4 CD @5 96
C03 16  2  ENG  @0 Proxy @4 CD @5 96
C03 16  2  SPA  @0 Indicador @4 CD @5 96
C07 01  2  FRE  @0 Australie @2 NG
C07 01  2  ENG  @0 Australia @2 NG
C07 01  2  SPA  @0 Australia @2 NG
C07 02  2  FRE  @0 Australasie
C07 02  2  ENG  @0 Australasia
C07 02  2  SPA  @0 Australasia
N21       @1 335

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Le document en format XML

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<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG">
<s0>rainfall</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA">
<s0>Lluvia</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE">
<s0>Variabilité climatique</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG">
<s0>climate variability</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE">
<s0>Analyse corrélation</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG">
<s0>Correlation analysis</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA">
<s0>Análisis correlación</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE">
<s0>Analyse composante principale</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG">
<s0>principal components analysis</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA">
<s0>Análisis componente principal</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="X" l="FRE">
<s0>Interpolation optimale</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="ENG">
<s0>Optimum interpolation</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="X" l="SPA">
<s0>Interpolación óptima</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="X" l="FRE">
<s0>Analyse objective</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="ENG">
<s0>Objective analysis</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="X" l="SPA">
<s0>Análisis objetivos</s0>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="3" l="FRE">
<s0>Evaluation risque</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="3" l="ENG">
<s0>Risk assessment</s0>
<s5>12</s5>
</fC03>
<fC03 i1="13" i2="X" l="FRE">
<s0>Long terme</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="X" l="ENG">
<s0>Long term</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="X" l="SPA">
<s0>Largo plazo</s0>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE">
<s0>Bassin Murray</s0>
<s2>NG</s2>
<s5>21</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG">
<s0>Murray Basin</s0>
<s2>NG</s2>
<s5>21</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA">
<s0>Cuenca Murray</s0>
<s2>NG</s2>
<s5>21</s5>
</fC03>
<fC03 i1="15" i2="X" l="FRE">
<s0>Gestion risque</s0>
<s5>41</s5>
</fC03>
<fC03 i1="15" i2="X" l="ENG">
<s0>Risk management</s0>
<s5>41</s5>
</fC03>
<fC03 i1="15" i2="X" l="SPA">
<s0>Gestión riesgo</s0>
<s5>41</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE">
<s0>Indicateur</s0>
<s4>CD</s4>
<s5>96</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG">
<s0>Proxy</s0>
<s4>CD</s4>
<s5>96</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA">
<s0>Indicador</s0>
<s4>CD</s4>
<s5>96</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE">
<s0>Australie</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG">
<s0>Australia</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA">
<s0>Australia</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE">
<s0>Australasie</s0>
</fC07>
<fC07 i1="02" i2="2" l="ENG">
<s0>Australasia</s0>
</fC07>
<fC07 i1="02" i2="2" l="SPA">
<s0>Australasia</s0>
</fC07>
<fN21>
<s1>335</s1>
</fN21>
</pA>
</standard>
</inist>
</record>

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