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| Titel |
Accelerated contributions of Canada's Baffin and Bylot Island glaciers to sea level rise over the past half century |
| VerfasserIn |
A. Gardner, G. Moholdt, A. Arendt, B. Wouters |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1994-0416
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| Digitales Dokument |
URL |
| Erschienen |
In: The Cryosphere ; 6, no. 5 ; Nr. 6, no. 5 (2012-10-12), S.1103-1125 |
| Datensatznummer |
250003790
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| Publikation (Nr.) |
 copernicus.org/tc-6-1103-2012.pdf |
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| Zusammenfassung |
| Canadian Arctic glaciers have recently contributed large volumes of
meltwater to the world's oceans. To place recently observed glacier wastage
into a historical perspective and to determine the region's longer-term
(~50 years) contribution to sea level, we estimate mass and volume
changes for the glaciers of Baffin and Bylot Islands using digital elevation
models generated from airborne and satellite stereoscopic imagery and
elevation postings from repeat airborne and satellite laser altimetry. In
addition, we update existing glacier mass change records from GRACE
satellite gravimetry to cover the period from 2003 to 2011. Using this
integrated approach, we find that the rate of mass loss from the region's
glaciers increased from 11.1 ± 3.4 Gt a−1 (271 ± 84 kg m−2 a−1)
for the period 1963–2006 to 23.8 ± 6.1 Gt a−1
(581 ± 149 kg m−2 a−1) for the period 2003–2011. The doubling
of the rate of mass loss is attributed to higher temperatures in summer with
little change in annual precipitation. Through both direct and indirect
effects, changes in summer temperatures accounted for 70–98% of the
variance in the rate of mass loss, to which the Barnes Ice Cap was found to
be 1.7 times more sensitive than either the Penny Ice Cap or the region's
glaciers as a whole. This heightened sensitivity is the result of a glacier
hypsometry that is skewed to lower elevations, which are shown to have a
higher mass change sensitive to temperature compared to glacier surfaces at
higher elevations. Between 2003 and 2011 the glaciers of Baffin and Bylot
Islands contributed 0.07 ± 0.02 mm a−1 to sea level rise
accounting for 16% of the total contribution from glaciers outside of
Greenland and Antarctica, a rate much higher than the longer-term average of
0.03 ± 0.01 mm a−1 (1963 to 2006). |
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