La maladie de Parkinson au Canada (serveur d'exploration)

Attention, ce site est en cours de développement !
Attention, site généré par des moyens informatiques à partir de corpus bruts.
Les informations ne sont donc pas validées.

What drove the dramatic retreat of arctic sea ice during summer 2007?

Identifieur interne : 002252 ( Main/Exploration ); précédent : 002251; suivant : 002253

What drove the dramatic retreat of arctic sea ice during summer 2007?

Auteurs : Jinlun Zhang [États-Unis] ; Ron Lindsay [États-Unis] ; Mike Steele [États-Unis] ; Axel Schweiger [États-Unis]

Source :

RBID : ISTEX:428870A506156F1D7A6FA65E12D3204578F60D66

Abstract

A model study has been conducted of the unprecedented retreat of arctic sea ice in the summer of 2007. It is found that preconditioning, anomalous winds, and ice‐albedo feedback are mainly responsible for the retreat. Arctic sea ice in 2007 was preconditioned to radical changes after years of shrinking and thinning in a warm climate. During summer 2007 atmospheric changes strengthened the transpolar drift of sea ice, causing more ice to move out of the Pacific sector and the central Arctic Ocean where the reduction in ice thickness due to ice advection is up to 1.5 m more than usual. Some of the ice exited Fram Strait and some piled up in part of the Canada Basin and along the coast of northern Greenland, leaving behind an unusually large area of thin ice and open water. Thin ice and open water allow more surface solar heating because of a much reduced surface albedo, leading to amplified ice melting. The Arctic Ocean lost additional 10% of its total ice mass in which 70% is due directly to the amplified melting and 30% to the unusual ice advection, causing the unprecedented ice retreat. Arctic sea ice has entered a state of being particularly vulnerable to anomalous atmospheric forcing.

Url:
DOI: 10.1029/2008GL034005


Affiliations:


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


Le document en format XML

<record>
<TEI wicri:istexFullTextTei="biblStruct">
<teiHeader>
<fileDesc>
<titleStmt>
<title xml:lang="en">What drove the dramatic retreat of arctic sea ice during summer 2007?</title>
<author>
<name sortKey="Zhang, Jinlun" sort="Zhang, Jinlun" uniqKey="Zhang J" first="Jinlun" last="Zhang">Jinlun Zhang</name>
</author>
<author>
<name sortKey="Lindsay, Ron" sort="Lindsay, Ron" uniqKey="Lindsay R" first="Ron" last="Lindsay">Ron Lindsay</name>
</author>
<author>
<name sortKey="Steele, Mike" sort="Steele, Mike" uniqKey="Steele M" first="Mike" last="Steele">Mike Steele</name>
</author>
<author>
<name sortKey="Schweiger, Axel" sort="Schweiger, Axel" uniqKey="Schweiger A" first="Axel" last="Schweiger">Axel Schweiger</name>
</author>
</titleStmt>
<publicationStmt>
<idno type="wicri:source">ISTEX</idno>
<idno type="RBID">ISTEX:428870A506156F1D7A6FA65E12D3204578F60D66</idno>
<date when="2008" year="2008">2008</date>
<idno type="doi">10.1029/2008GL034005</idno>
<idno type="url">https://api-v5.istex.fr/document/428870A506156F1D7A6FA65E12D3204578F60D66/fulltext/pdf</idno>
<idno type="wicri:Area/Istex/Corpus">000929</idno>
<idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000929</idno>
<idno type="wicri:Area/Istex/Curation">000929</idno>
<idno type="wicri:Area/Istex/Checkpoint">000855</idno>
<idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Checkpoint">000855</idno>
<idno type="wicri:doubleKey">0094-8276:2008:Zhang J:what:drove:the</idno>
<idno type="wicri:Area/Main/Merge">002445</idno>
<idno type="wicri:Area/Main/Curation">002252</idno>
<idno type="wicri:Area/Main/Exploration">002252</idno>
</publicationStmt>
<sourceDesc>
<biblStruct>
<analytic>
<title level="a" type="main" xml:lang="en">What drove the dramatic retreat of arctic sea ice during summer 2007?</title>
<author>
<name sortKey="Zhang, Jinlun" sort="Zhang, Jinlun" uniqKey="Zhang J" first="Jinlun" last="Zhang">Jinlun Zhang</name>
<affiliation wicri:level="4">
<country xml:lang="fr">États-Unis</country>
<wicri:regionArea>Polar Science Center, Applied Physics Laboratory, College of Ocean and Fishery Sciences, University of Washington, Washington, Seattle</wicri:regionArea>
<orgName type="university">Université de Washington</orgName>
<placeName>
<settlement type="city">Seattle</settlement>
<region type="state">Washington (État)</region>
</placeName>
</affiliation>
<affiliation wicri:level="1">
<country wicri:rule="url">États-Unis</country>
</affiliation>
</author>
<author>
<name sortKey="Lindsay, Ron" sort="Lindsay, Ron" uniqKey="Lindsay R" first="Ron" last="Lindsay">Ron Lindsay</name>
<affiliation wicri:level="4">
<country xml:lang="fr">États-Unis</country>
<wicri:regionArea>Polar Science Center, Applied Physics Laboratory, College of Ocean and Fishery Sciences, University of Washington, Washington, Seattle</wicri:regionArea>
<orgName type="university">Université de Washington</orgName>
<placeName>
<settlement type="city">Seattle</settlement>
<region type="state">Washington (État)</region>
</placeName>
</affiliation>
</author>
<author>
<name sortKey="Steele, Mike" sort="Steele, Mike" uniqKey="Steele M" first="Mike" last="Steele">Mike Steele</name>
<affiliation wicri:level="4">
<country xml:lang="fr">États-Unis</country>
<wicri:regionArea>Polar Science Center, Applied Physics Laboratory, College of Ocean and Fishery Sciences, University of Washington, Washington, Seattle</wicri:regionArea>
<orgName type="university">Université de Washington</orgName>
<placeName>
<settlement type="city">Seattle</settlement>
<region type="state">Washington (État)</region>
</placeName>
</affiliation>
</author>
<author>
<name sortKey="Schweiger, Axel" sort="Schweiger, Axel" uniqKey="Schweiger A" first="Axel" last="Schweiger">Axel Schweiger</name>
<affiliation wicri:level="4">
<country xml:lang="fr">États-Unis</country>
<wicri:regionArea>Polar Science Center, Applied Physics Laboratory, College of Ocean and Fishery Sciences, University of Washington, Washington, Seattle</wicri:regionArea>
<orgName type="university">Université de Washington</orgName>
<placeName>
<settlement type="city">Seattle</settlement>
<region type="state">Washington (État)</region>
</placeName>
</affiliation>
</author>
</analytic>
<monogr></monogr>
<series>
<title level="j">Geophysical Research Letters</title>
<title level="j" type="abbrev">Geophys. Res. Lett.</title>
<idno type="ISSN">0094-8276</idno>
<idno type="eISSN">1944-8007</idno>
<imprint>
<publisher>Blackwell Publishing Ltd</publisher>
<date type="published" when="2008-06">2008-06</date>
<biblScope unit="volume">35</biblScope>
<biblScope unit="issue">11</biblScope>
<biblScope unit="page" from="/">n/a</biblScope>
<biblScope unit="page" to="/">n/a</biblScope>
</imprint>
<idno type="ISSN">0094-8276</idno>
</series>
<idno type="istex">428870A506156F1D7A6FA65E12D3204578F60D66</idno>
<idno type="DOI">10.1029/2008GL034005</idno>
<idno type="ArticleID">2008GL034005</idno>
</biblStruct>
</sourceDesc>
<seriesStmt>
<idno type="ISSN">0094-8276</idno>
</seriesStmt>
</fileDesc>
<profileDesc>
<textClass></textClass>
<langUsage>
<language ident="en">en</language>
</langUsage>
</profileDesc>
</teiHeader>
<front>
<div type="abstract">A model study has been conducted of the unprecedented retreat of arctic sea ice in the summer of 2007. It is found that preconditioning, anomalous winds, and ice‐albedo feedback are mainly responsible for the retreat. Arctic sea ice in 2007 was preconditioned to radical changes after years of shrinking and thinning in a warm climate. During summer 2007 atmospheric changes strengthened the transpolar drift of sea ice, causing more ice to move out of the Pacific sector and the central Arctic Ocean where the reduction in ice thickness due to ice advection is up to 1.5 m more than usual. Some of the ice exited Fram Strait and some piled up in part of the Canada Basin and along the coast of northern Greenland, leaving behind an unusually large area of thin ice and open water. Thin ice and open water allow more surface solar heating because of a much reduced surface albedo, leading to amplified ice melting. The Arctic Ocean lost additional 10% of its total ice mass in which 70% is due directly to the amplified melting and 30% to the unusual ice advection, causing the unprecedented ice retreat. Arctic sea ice has entered a state of being particularly vulnerable to anomalous atmospheric forcing.</div>
</front>
</TEI>
<affiliations>
<list>
<country>
<li>États-Unis</li>
</country>
<region>
<li>Washington (État)</li>
</region>
<settlement>
<li>Seattle</li>
</settlement>
<orgName>
<li>Université de Washington</li>
</orgName>
</list>
<tree>
<country name="États-Unis">
<region name="Washington (État)">
<name sortKey="Zhang, Jinlun" sort="Zhang, Jinlun" uniqKey="Zhang J" first="Jinlun" last="Zhang">Jinlun Zhang</name>
</region>
<name sortKey="Lindsay, Ron" sort="Lindsay, Ron" uniqKey="Lindsay R" first="Ron" last="Lindsay">Ron Lindsay</name>
<name sortKey="Schweiger, Axel" sort="Schweiger, Axel" uniqKey="Schweiger A" first="Axel" last="Schweiger">Axel Schweiger</name>
<name sortKey="Steele, Mike" sort="Steele, Mike" uniqKey="Steele M" first="Mike" last="Steele">Mike Steele</name>
<name sortKey="Zhang, Jinlun" sort="Zhang, Jinlun" uniqKey="Zhang J" first="Jinlun" last="Zhang">Jinlun Zhang</name>
</country>
</tree>
</affiliations>
</record>

Pour manipuler ce document sous Unix (Dilib)

EXPLOR_STEP=$WICRI_ROOT/Wicri/Canada/explor/ParkinsonCanadaV1/Data/Main/Exploration
HfdSelect -h $EXPLOR_STEP/biblio.hfd -nk 002252 | SxmlIndent | more

Ou

HfdSelect -h $EXPLOR_AREA/Data/Main/Exploration/biblio.hfd -nk 002252 | SxmlIndent | more

Pour mettre un lien sur cette page dans le réseau Wicri

{{Explor lien
   |wiki=    Wicri/Canada
   |area=    ParkinsonCanadaV1
   |flux=    Main
   |étape=   Exploration
   |type=    RBID
   |clé=     ISTEX:428870A506156F1D7A6FA65E12D3204578F60D66
   |texte=   What drove the dramatic retreat of arctic sea ice during summer 2007?
}}

Wicri

This area was generated with Dilib version V0.6.29.
Data generation: Thu May 4 22:20:19 2017. Site generation: Fri Dec 23 23:17:26 2022