In: Biological Invasions, 2015, vol. 17, no. 10, p. 3041-3047
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In: Oecologia, 2015, vol. 179, no. 3, p. 765-775
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In: Extremophiles, 2015, vol. 19, no. 3, p. 631-642
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In: Oecologia, 2015, vol. 177, no. 1, p. 97-111
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In: The Cryosphere, 2019, vol. 13, no. 12, p. 3413–3434
Snow water equivalent (SWE) measurements of seasonal snowpack are crucial in many research fields. Yet accurate measurements at a high temporal resolution are difficult to obtain in high mountain regions. With a cosmic ray sensor (CRS), SWE can be inferred from neutron counts. We present the analyses of temporally continuous SWE measurements by a CRS on an alpine glacier in Switzerland...
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In: Nature, 2019, vol. 573, no. 7774, p. 403–407
In recent decades, meltwater runoff has accelerated to become the dominant mechanism for mass loss in the Greenland ice sheet1,2,3. In Greenland’s high- elevation interior, porous snow and firn accumulate; these can absorb surface meltwater and inhibit runoff4, but this buffering effect is limited if enough water refreezes near the surface to restrict percolation5,6. However, the influence...
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In: Biogeochemistry, 2014, vol. 117, no. 2-3, p. 395-412
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In: Climatic Change, 2014, vol. 127, no. 3-4, p. 521-534
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In: Multibody System Dynamics, 2014, vol. 32, no. 2, p. 241-271
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In: Plant and Soil, 2014, vol. 374, no. 1-2, p. 579-591
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