More than a century of direct glacier mass-balance observations on Claridenfirn, Switzerland
1904 Earth-Surface Processes
Earth
15. Life on land
melt
01 natural sciences
Environmental sciences
Surface
10122 Institute of Geography
Surface Processes
Accumulation
Mass-balance reconstruction
13. Climate action
mass-balance reconstruction
Meteorology. Climatology
glacier monitoring
surface
GE1-350
910 Geography & travel
QC851-999
Glacier monitoring
Melt
0105 earth and related environmental sciences
DOI:
10.1017/jog.2021.22
Publication Date:
2021-03-11T07:31:51Z
AUTHORS (7)
ABSTRACT
AbstractGlacier mass-balance observations at seasonal resolution have been performed since 1914 at two sites on Claridenfirn, Switzerland. The measurements are the longest uninterrupted records of glacier mass balance worldwide. Here, we provide a complete re-analysis of the 106-year series (1914–2020), focusing on both point and glacier-wide mass balance. The approaches to evaluate and homogenize the direct observations are described in detail. Based on conservative assumptions, average uncertainties of$\pm$0.25 m w.e. are estimated for glacier-wide mass balances at the annual scale. It is demonstrated that long-term variations in mass balance are clearly driven by melting, whereas decadal changes in accumulation are uncorrelated with mass balance and can only be relevant in short periods. Mass change of Claridenfirn is impacted by dry calving at a frontal ice cliff. Considerations of ice volume flux at a cross-profile reveal long-term variations in frontal ice loss accounting for$\sim$9% of total annual ablation on average. The effect of changes in frontal ablation mostly explains$\lt$10% of the mass-balance difference relative to the period 1960–1990, but accounts for$\sim$20% in 2010–2020. Glacier mass changes are discussed in the context of observations throughout the European Alps indicating that Claridenfirn is regionally representative.
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