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008 | 220822b |||||||| |||| 00| 0 eng d | ||
100 |
_aWeber, Paul _952287 |
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245 | _aEvolution of the Norwegian plateau icefield Hardangerjøkulen since the ‘Little Ice Age’/ | ||
260 |
_bsage _c2019 |
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300 | _aVol 29, Issue 12, 2019 : (1885-1905 p.). | ||
520 | _aThe maximum ‘Little Ice Age’ (LIA) glacier extent provides a significant baseline to assess long-term glacier change and to place currently observed rates of glacier recession in a broader temporal context. To that end, we examine the evolution of the plateau icefield Hardangerjøkulen since the LIA. First, we reconstruct Hardangerjøkulen’s maximum LIA extent (~AD 1750) and subsequent recession based on the glacial landform record and aided by historical map interpretation. Ice-marginal moraines, glacial drift limits, trimlines, and identifiable erosion and weathering boundaries provide evidence of a LIA icefield with an area of 110 km2. Existing LIA model simulations of Hardangerjøkulen are not yet fully able to reproduce our reconstructed extent. Second, we compile a set of remotely sensed icefield outlines from successive time points in the 20th and 21st century to calculate icefield area and length change since the LIA. This reveals a substantial reduction in icefield size, with a total area loss of 41 km2 (37%; 2% 10 a–1) by 2010 and a cumulative frontal retreat averaging 1.3 km (29%; 5 m a–1) by 2013. Icefield recession has been greatest since the end of the 20th century, when rates of areal shrinkage increased to 6.5–10% 10 a–1 in 1995–2010, and the rate of average terminus retreat accelerated to 17 m a–1 in 2003–2010. Third, we present a relative dating approach, based on the known age of the different icefield outlines, that allows bracketing ages to be assigned to all ice-marginal landforms between any two outlines. This approach shows that episodes of moraine formation vary temporally between individual outlet glaciers of Hardangerjøkulen, suggesting that the moraine record of a single outlet glacier alone may not be sufficient to derive an icefield-wide picture of past ice advances, and thereby climate fluctuations. | ||
650 |
_aglacier change, _952288 |
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650 |
_aglacier reconstruction, _952289 |
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650 |
_a Hardangerjøkulen, _952290 |
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650 |
_a‘Little Ice Age’ (LIA), _951574 |
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650 |
_a Norway, _952291 |
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650 |
_aplateau icefield _952292 |
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700 |
_aBoston, Clare M _952293 |
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700 |
_aLovell, Harold _952294 |
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773 | 0 |
_012756 _916504 _dLondon: Sage Publication Ltd, 2019. _tHolocene/ _x09596836 |
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856 | _uhttps://doi.org/10.1177/0959683619865601 | ||
942 |
_2ddc _cART |
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999 |
_c12872 _d12872 |