In: Regional Environmental Change, 2015, vol. 15, no. 3, p. 505-515
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In: Biogeochemistry, 2015, vol. 124, no. 1-3, p. 95-111
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In: Climate Dynamics, 2015, vol. 44, no. 7-8, p. 1857-1869
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In: Plant and Soil, 2015, vol. 392, no. 1-2, p. 345-356
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In: Nature Geoscience, 2019, vol. 12, no. 8, p. 650–656
During the first half of the nineteenth century, several large tropical volcanic eruptions occurred within less than three decades. The global climate effects of the 1815 Tambora eruption have been investigated, but those of an eruption in 1808 or 1809 whose source is unknown and the eruptions in the 1820s and 1830s have received less attention. Here we analyse the effect of the sequence of...
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In: Cold Regions Science and Technology, 2019, vol. 165, p. 102788
The warming climate is changing the surface dynamics of the Greenland Ice Sheet, including the balance between snowfall and melt. Increasing surface melt impacts the structure of the relatively porous near-surface layer known as firn. Camp Century, a base abandoned in 1967, now comprises a subsurface debris field within the firn in Northwest Greenland. We collected 80 km of 100 or 250 MHz...
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In: Holzforschung, 2015, vol. 69, no. 1, p. 103-112
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In: Holzforschung, 2016, vol. 70, no. 7, p. 619-631
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In: Climatic Change, 2014, vol. 122, no. 1-2, p. 141-155
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In: Oecologia, 2014, vol. 175, no. 3, p. 747-762
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