Modelled glacier dynamics over the last quarter of a century at Jakobshavn Isbræ

Ioana S. Muresan; Shfaqat A. Khan; Andy Aschwanden; Constantine Khroulev; Tonie Van Dam; Jonathan Bamber; Michiel R. van den Broeke; Bert Wouters; Peter Kuipers Munneke; Kurt H. Kjær

doi:10.5194/tc-10-597-2016

Modelled glacier dynamics over the last quarter of a century at Jakobshavn Isbræ

Ioana S. Muresan, Shfaqat A. Khan, Andy Aschwanden, Constantine Khroulev, Tonie Van Dam, Jonathan Bamber, Michiel R. van den Broeke, Bert Wouters, Peter Kuipers Munneke, Kurt H. Kjær

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › peer review

11 Citationer (Scopus)

466 Downloads (Pure)

Originalsprog	Engelsk
Tidsskrift	The Cryosphere
Vol/bind	10
Udgave nummer	2
Sider (fra-til)	597-611
Antal sider	15
ISSN	1994-0416
DOI	https://doi.org/10.5194/tc-10-597-2016
Status	Udgivet - 2016

Adgang til dokumentet

10.5194/tc-10-597-2016Licens: CC BY

Muresan_2016_Modelled_glacier_dynamicsForlagets udgivne version, 5,82 MBLicens: CC BY

Citationsformater

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title = "Modelled glacier dynamics over the last quarter of a century at Jakobshavn Isbr{\ae}",

author = "Muresan, {Ioana S.} and Khan, {Shfaqat A.} and Andy Aschwanden and Constantine Khroulev and {Van Dam}, Tonie and Jonathan Bamber and {van den Broeke}, {Michiel R.} and Bert Wouters and Munneke, {Peter Kuipers} and Kj{\ae}r, {Kurt H.}",

year = "2016",

doi = "10.5194/tc-10-597-2016",

language = "English",

volume = "10",

pages = "597--611",

journal = "The Cryosphere",

issn = "1994-0416",

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TY - JOUR

T1 - Modelled glacier dynamics over the last quarter of a century at Jakobshavn Isbræ

AU - Muresan, Ioana S.

AU - Khan, Shfaqat A.

AU - Aschwanden, Andy

AU - Khroulev, Constantine

AU - Van Dam, Tonie

AU - Bamber, Jonathan

AU - van den Broeke, Michiel R.

AU - Wouters, Bert

AU - Munneke, Peter Kuipers

AU - Kjær, Kurt H.

PY - 2016

Y1 - 2016

U2 - 10.5194/tc-10-597-2016

DO - 10.5194/tc-10-597-2016

M3 - Journal article

SN - 1994-0416

VL - 10

SP - 597

EP - 611

JO - The Cryosphere

JF - The Cryosphere

IS - 2

ER -