AustralieFrV1, PascalFrancis, Curation, bibRecord, 002C83

Evolution of the glacial landscape of the Southern Alps of New Zealand : Insights from a glacial erosion model

Identifieur interne : 002C83 ( PascalFrancis/Curation ); précédent : 002C82; suivant : 002C84

Evolution of the glacial landscape of the Southern Alps of New Zealand : Insights from a glacial erosion model

Auteurs : Frédéric Herman [Australie, États-Unis, Suisse] ; Jean Braun [France]

Source :

Journal of geophysical research [ 0148-0227 ] ; 2008.

RBID : Pascal:08-0395030

Descripteurs français

Pascal (Inist)
- Paysage, Erosion glaciaire, Modèle tectonique, Calotte glaciaire, Modélisation, Aluminium, Complexité, Glacier, Massif montagneux, Surrection, Précipitation atmosphérique, Oscillation, Rétroaction, Boucle réaction, Forme relief, Dynamique, Phénomène transitoire, Cycle, Alpes, Nouvelle Zélande, Faille Alpine.
Wicri :
- topic : Aluminium.

English descriptors

KwdEn :
- Alpine Fault, Alps, Complexity, Feedback, Modeling, New Zealand, aluminum, atmospheric precipitation, cycles, dynamics, feedback, glacial erosion, glaciers, ice caps, landforms, landscapes, mountains, oscillations, tectonic models, transient phenomena, uplifts.

Abstract

[1] A new version of a landscape evolution model that includes the evolution of an ice cap at a 10³ to 10⁵ year timescale and its associated erosion patterns is presented and applied to the Southern Alps of New Zealand. Modeling of the ice cap evolution is performed on a higher-resolution grid (i.e., ∼100 m) than previously (Braun et al., 1998). It predicts which parts of the landscape are, and have been, affected by glacial erosion. The model results highlight the complexity of the erosion patterns induced by ice caps and glaciers. Glacial erosion in a tectonically active area is, as suggested by the model, not uniform across the mountain range. Furthermore, high rock uplift rates, heavy precipitation, and climatic oscillations constantly interact. The feedback mechanisms are such that they render the landform very dynamic and transient. However, under conditions of reduced rock uplift rate and precipitation, the landform becomes more stable at the timescale of the glacial cycle. Finally, the modeling results favor a tectonic model in the Southern Alps in which the maximum rock uplift is offset from the Alpine Fault.

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A08	`01`	`1`	`ENG`	`@1 Evolution of the glacial landscape of the Southern Alps of New Zealand : Insights from a glacial erosion model`
A11	`01`	`1`		`@1 HERMAN (Frédéric)`
A11	`02`	`1`		`@1 BRAUN (Jean)`
A14	`01`			`@1 Research School of Earth Sciences, Australian National University @2 Canberra, ACT @3 AUS @Z 1 aut.`
A14	`02`			`@1 Geological and Planetary Science Division, California Institute of Technology @2 Pasadena, California @3 USA @Z 1 aut.`
A14	`03`			`@1 Geologisches Institut, ETH Zurich @2 Zurich @3 CHE @Z 1 aut.`
A14	`04`			`@1 Géosciences Rennes, Université de Rennes 1 @2 Rennes @3 FRA @Z 2 aut.`
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C03	`01`	`2`	`ENG`	`@0 landscapes @5 01`
C03	`01`	`2`	`SPA`	`@0 Paisaje @5 01`
C03	`02`	`2`	`FRE`	`@0 Erosion glaciaire @5 02`
C03	`02`	`2`	`ENG`	`@0 glacial erosion @5 02`
C03	`02`	`2`	`SPA`	`@0 Erosión glaciar @5 02`
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C03	`04`	`2`	`ENG`	`@0 ice caps @5 04`
C03	`04`	`2`	`SPA`	`@0 Casquete glaciar @5 04`
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C03	`06`	`2`	`FRE`	`@0 Aluminium @5 06`
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C03	`07`	`X`	`FRE`	`@0 Complexité @5 07`
C03	`07`	`X`	`ENG`	`@0 Complexity @5 07`
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C03	`09`	`2`	`FRE`	`@0 Massif montagneux @5 09`
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C03	`09`	`2`	`SPA`	`@0 Macizo montañoso @5 09`
C03	`10`	`2`	`FRE`	`@0 Surrection @5 11`
C03	`10`	`2`	`ENG`	`@0 uplifts @5 11`
C03	`11`	`2`	`FRE`	`@0 Précipitation atmosphérique @5 12`
C03	`11`	`2`	`ENG`	`@0 atmospheric precipitation @5 12`
C03	`11`	`2`	`SPA`	`@0 Precipitación atmosférica @5 12`
C03	`12`	`2`	`FRE`	`@0 Oscillation @5 13`
C03	`12`	`2`	`ENG`	`@0 oscillations @5 13`
C03	`12`	`2`	`SPA`	`@0 Oscilación @5 13`
C03	`13`	`2`	`FRE`	`@0 Rétroaction @5 14`
C03	`13`	`2`	`ENG`	`@0 feedback @5 14`
C03	`14`	`X`	`FRE`	`@0 Boucle réaction @5 15`
C03	`14`	`X`	`ENG`	`@0 Feedback @5 15`
C03	`14`	`X`	`SPA`	`@0 Retroalimentación @5 15`
C03	`15`	`2`	`FRE`	`@0 Forme relief @5 16`
C03	`15`	`2`	`ENG`	`@0 landforms @5 16`
C03	`16`	`2`	`FRE`	`@0 Dynamique @5 17`
C03	`16`	`2`	`ENG`	`@0 dynamics @5 17`
C03	`16`	`2`	`SPA`	`@0 Dinámica @5 17`
C03	`17`	`2`	`FRE`	`@0 Phénomène transitoire @5 18`
C03	`17`	`2`	`ENG`	`@0 transient phenomena @5 18`
C03	`18`	`2`	`FRE`	`@0 Cycle @5 19`
C03	`18`	`2`	`ENG`	`@0 cycles @5 19`
C03	`19`	`2`	`FRE`	`@0 Alpes @2 NG @5 61`
C03	`19`	`2`	`ENG`	`@0 Alps @2 NG @5 61`
C03	`19`	`2`	`SPA`	`@0 Alpes @2 NG @5 61`
C03	`20`	`2`	`FRE`	`@0 Nouvelle Zélande @2 NG @5 62`
C03	`20`	`2`	`ENG`	`@0 New Zealand @2 NG @5 62`
C03	`20`	`2`	`SPA`	`@0 Nueva Zelandia @2 NG @5 62`
C03	`21`	`2`	`FRE`	`@0 Faille Alpine @2 NG @5 64`
C03	`21`	`2`	`ENG`	`@0 Alpine Fault @2 NG @5 64`
C03	`21`	`2`	`SPA`	`@0 Falla Alpina @2 NG @5 64`
C07	`01`	`2`	`FRE`	`@0 Europe @2 564`
C07	`01`	`2`	`ENG`	`@0 Europe @2 564`
C07	`01`	`2`	`SPA`	`@0 Europa @2 564`
C07	`02`	`2`	`FRE`	`@0 Australasie`
C07	`02`	`2`	`ENG`	`@0 Australasia`
C07	`02`	`2`	`SPA`	`@0 Australasia`
C07	`03`	`2`	`FRE`	`@0 Nouvelle Zélande Ile Sud @2 NG`
C07	`03`	`2`	`ENG`	`@0 South Island @2 NG`
C07	`03`	`2`	`SPA`	`@0 Nueva Zelanda Isla Sur @2 NG`
N21				`@1 252`
N44	`01`			`@1 OTO`
N82				`@1 OTO`

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Le document en format XML

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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Alpine Fault</term>
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<term>Modeling</term>
<term>New Zealand</term>
<term>aluminum</term>
<term>atmospheric precipitation</term>
<term>cycles</term>
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<term>glacial erosion</term>
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<front><div type="abstract" xml:lang="en">[1] A new version of a landscape evolution model that includes the evolution of an ice cap at a 10<sup>3</sup>
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 year timescale and its associated erosion patterns is presented and applied to the Southern Alps of New Zealand. Modeling of the ice cap evolution is performed on a higher-resolution grid (i.e., ∼100 m) than previously (Braun et al., 1998). It predicts which parts of the landscape are, and have been, affected by glacial erosion. The model results highlight the complexity of the erosion patterns induced by ice caps and glaciers. Glacial erosion in a tectonically active area is, as suggested by the model, not uniform across the mountain range. Furthermore, high rock uplift rates, heavy precipitation, and climatic oscillations constantly interact. The feedback mechanisms are such that they render the landform very dynamic and transient. However, under conditions of reduced rock uplift rate and precipitation, the landform becomes more stable at the timescale of the glacial cycle. Finally, the modeling results favor a tectonic model in the Southern Alps in which the maximum rock uplift is offset from the Alpine Fault.</div>
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<fC01 i1="01" l="ENG"><s0>[1] A new version of a landscape evolution model that includes the evolution of an ice cap at a 10<sup>3</sup>
 to 10<sup>5</sup>
 year timescale and its associated erosion patterns is presented and applied to the Southern Alps of New Zealand. Modeling of the ice cap evolution is performed on a higher-resolution grid (i.e., ∼100 m) than previously (Braun et al., 1998). It predicts which parts of the landscape are, and have been, affected by glacial erosion. The model results highlight the complexity of the erosion patterns induced by ice caps and glaciers. Glacial erosion in a tectonically active area is, as suggested by the model, not uniform across the mountain range. Furthermore, high rock uplift rates, heavy precipitation, and climatic oscillations constantly interact. The feedback mechanisms are such that they render the landform very dynamic and transient. However, under conditions of reduced rock uplift rate and precipitation, the landform becomes more stable at the timescale of the glacial cycle. Finally, the modeling results favor a tectonic model in the Southern Alps in which the maximum rock uplift is offset from the Alpine Fault.</s0>
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<fC03 i1="04" i2="2" l="ENG"><s0>ice caps</s0>
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<fC03 i1="04" i2="2" l="SPA"><s0>Casquete glaciar</s0>
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<fC03 i1="08" i2="2" l="SPA"><s0>Glaciar</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Massif montagneux</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>mountains</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Macizo montañoso</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Surrection</s0>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>uplifts</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Précipitation atmosphérique</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>atmospheric precipitation</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Precipitación atmosférica</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Oscillation</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>oscillations</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Oscilación</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Rétroaction</s0>
<s5>14</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>feedback</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="X" l="FRE"><s0>Boucle réaction</s0>
<s5>15</s5>
</fC03>
<fC03 i1="14" i2="X" l="ENG"><s0>Feedback</s0>
<s5>15</s5>
</fC03>
<fC03 i1="14" i2="X" l="SPA"><s0>Retroalimentación</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Forme relief</s0>
<s5>16</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>landforms</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Dynamique</s0>
<s5>17</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>dynamics</s0>
<s5>17</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Dinámica</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Phénomène transitoire</s0>
<s5>18</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>transient phenomena</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Cycle</s0>
<s5>19</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG"><s0>cycles</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>Alpes</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG"><s0>Alps</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="19" i2="2" l="SPA"><s0>Alpes</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="20" i2="2" l="FRE"><s0>Nouvelle Zélande</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC03 i1="20" i2="2" l="ENG"><s0>New Zealand</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC03 i1="20" i2="2" l="SPA"><s0>Nueva Zelandia</s0>
<s2>NG</s2>
<s5>62</s5>
</fC03>
<fC03 i1="21" i2="2" l="FRE"><s0>Faille Alpine</s0>
<s2>NG</s2>
<s5>64</s5>
</fC03>
<fC03 i1="21" i2="2" l="ENG"><s0>Alpine Fault</s0>
<s2>NG</s2>
<s5>64</s5>
</fC03>
<fC03 i1="21" i2="2" l="SPA"><s0>Falla Alpina</s0>
<s2>NG</s2>
<s5>64</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Europe</s0>
<s2>564</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Europe</s0>
<s2>564</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Europa</s0>
<s2>564</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>
<fC07 i1="03" i2="2" l="FRE"><s0>Nouvelle Zélande Ile Sud</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="2" l="ENG"><s0>South Island</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="2" l="SPA"><s0>Nueva Zelanda Isla Sur</s0>
<s2>NG</s2>
</fC07>
<fN21><s1>252</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
</inist>
</record>

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   |area=    AustralieFrV1
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   |texte=   Evolution of the glacial landscape of the Southern Alps of New Zealand : Insights from a glacial erosion model
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This area was generated with Dilib version V0.6.33.
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	Serveur d'exploration sur les relations entre la France et l'Australie
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Serveur d'exploration sur les relations entre la France et l'Australie

Evolution of the glacial landscape of the Southern Alps of New Zealand : Insights from a glacial erosion model

Evolution of the glacial landscape of the Southern Alps of New Zealand : Insights from a glacial erosion model

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