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Titel |
Comparison of direct and geodetic mass balances on a multi-annual time scale |
VerfasserIn |
A. Fischer |
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 ; 5, no. 1 ; Nr. 5, no. 1 (2011-02-24), S.107-124 |
Datensatznummer |
250002274
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Publikation (Nr.) |
copernicus.org/tc-5-107-2011.pdf |
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Zusammenfassung |
The geodetic mass balances of six Austrian glaciers over 19 periods between
1953 and 2006 are compared to the direct mass balances over the same periods.
For two glaciers, Hintereisferner and Kesselwandferner, case studies showing
possible reasons for discrepancies between the geodetic and the direct mass
balance are presented. The mean annual geodetic mass balance for all periods
is −0.5 m w.e. a−1, the mean annual direct mass balance
−0.4 m w.e. a−1. The mean cumulative difference is −0.6 m w.e.,
the minimum −7.3 m w.e., and the maximum 5.6 m w.e. The accuracy of
geodetic mass balance may depend on the accuracy of the DEMs, which ranges
from 2 m w.e. for photogrammetric data to 0.02 m w.e. for airborne
laser scanning (LiDAR) data. Basal melt, seasonal snow cover, and density
changes of the surface layer also contribute up to 0.7 m w.e. to the
difference between the two methods over the investigated period of 10 yr. On
Hintereisferner, the fraction of area covered by snow or firn has been
changing within 1953–2006. The accumulation area is not identical with the
firn area, and both are not coincident with areas of volume gain. Longer
periods between the acquisition of the DEMs do not necessarily result in a
higher accuracy of the geodetic mass balance. Trends in the difference
between the direct and the geodetic data vary from glacier to glacier and can
differ systematically for specific glaciers under specific types of climate
forcing. Ultimately, geodetic and direct mass balance data are complementary,
and great care must be taken when attempting to combine them. |
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