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Permanent URL to this publication: http://dx.doi.org/10.5167/uzh-63216

Hoelzle, M; Haeberli, W; Dischl, M; Peschke, W (2003). Secular glacier mass balances derived from cumulative glacier length changes. Global and Planetary Change, 36(4):295-306.

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Glacier mass changes are considered to represent natural key variables with respect to strategies for early detection of enhanced greenhouse effects on climate. The main problem, however, with interpreting worldwide glacier mass balance evolution concerns the question of representativity. One important key to deal with such uncertainties and to assess the spatio-temporal representativity of the few available measurements is the long-term change in cumulative glacier length. The mean specific mass balance determined from glacier length change data since 1900 shows considerable regional variability but centers around a mean value of about −0.25 m year⁻¹ water equivalent.


100 citations in Web of Science®
110 citations in Scopus®
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Additional indexing

Item Type:Journal Article, refereed, original work
Communities & Collections:07 Faculty of Science > Institute of Geography
Dewey Decimal Classification:910 Geography & travel
Deposited On:20 Jul 2012 19:48
Last Modified:05 Apr 2016 15:52
Publisher DOI:10.1016/S0921-8181(02)00223-0

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