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Record #199772:

Modeling and hindcasting of the mass balance of Werenskioldbreen (southern Svalbard) / Mariusz Grabiec, Tomasz Budzik, Piotr Glowacki.

Title: Modeling and hindcasting of the mass balance of Werenskioldbreen (southern Svalbard) / Mariusz Grabiec, Tomasz Budzik, Piotr Glowacki.
Author(s): Grabiec, Mariusz.
Budzik, Tomasz.
Glowacki, Piotr.
Date: 2012.
In: Arctic, Antarctic, and Alpine Research. (2012.), Vol. 44(2) (2012)
Abstract: Proposes model of glacial mass balance based on correlations with meterological observations and data from climate reanalysis. Model is used to hindcast mass balance and its components at Werenskioldbreen, southern Svalbard, over period 1912-2005. Hindcast specific mass balance is then used to estimate change in thickness of snout of Werenskioldbreen over period 1958-1990. Results are compared with those obtained using cartographic method. Average difference in claculation of change in glacier thickness between methods amounted to 3.7 m (based on meterological data) and 0.2 m (using ERA-40 re-analysis data).
Notes:

Arctic, Antarctic, and Alpine Research. Vol. 44(2) :164-179 (2012).

Keywords: 519.673 -- Modelling.
551.324 -- Land ice.
551.324.22 -- Glaciers: Werenskioldbreen.
551.324.3 -- Land ice, depth measurements.
551.324.4 -- Land ice, mass and energy balance.
551.506 -- Meteorological data.
551.583 -- Climatic changes.
E5 -- Glaciology: land ice.
(*3) -- Arctic regions.
(*32) -- Svalbard.
SPRI record no.: 199772

MARCXML

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035 ## ‡aSPRI-199772
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aGrabiec, Mariusz.
245 10 ‡aModeling and hindcasting of the mass balance of Werenskioldbreen (southern Svalbard) /‡cMariusz Grabiec, Tomasz Budzik, Piotr Glowacki.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2012.
300 ## ‡ap. 164-179 :‡bill., diags., tables, maps.
500 ## ‡aArctic, Antarctic, and Alpine Research. Vol. 44(2) :164-179 (2012).
520 3# ‡aProposes model of glacial mass balance based on correlations with meterological observations and data from climate reanalysis. Model is used to hindcast mass balance and its components at Werenskioldbreen, southern Svalbard, over period 1912-2005. Hindcast specific mass balance is then used to estimate change in thickness of snout of Werenskioldbreen over period 1958-1990. Results are compared with those obtained using cartographic method. Average difference in claculation of change in glacier thickness between methods amounted to 3.7 m (based on meterological data) and 0.2 m (using ERA-40 re-analysis data).
530 ## ‡aAlso issued online ‡uurn:doi:10.1657/1938-4246-44.2.164‡uhttps://dx.doi.org/10.1657/1938-4246-44.2.164
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.22 -- Glaciers: Werenskioldbreen.‡2udc
650 07 ‡a551.324.3 -- Land ice, depth measurements.‡2udc
650 07 ‡a551.324.4 -- Land ice, mass and energy balance.‡2udc
650 07 ‡a551.506 -- Meteorological data.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*32) -- Svalbard.‡2udc
700 1# ‡aBudzik, Tomasz.
700 1# ‡aGlowacki, Piotr.
773 0# ‡7nnas ‡tArctic, Antarctic, and Alpine Research. ‡gVol. 44(2) (2012) ‡wSPRI-211524
916 ## ‡a2012/07/13 -- JW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20231204 ‡bJW