European Glacial Landscapes 2024
DOI: 10.1016/b978-0-323-99712-6.00018-0
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Holocene glacier variations in the Alps

Melaine Le Roy,
Susan Ivy-Ochs,
Kurt Nicolussi
et al.
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Cited by 3 publications
(7 citation statements)
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“…The onset of ice accumulation at Mörkgletscher around 3.2 kyr BP may have been related to an episode of glacier advance in the Alps, known as the Göschenen 1 advance and more recently called Iron Age Advance Period 1, starting around 3 kyr BP 43 . The change towards a higher mean accumulation rate during approximately the thirteenth century AD occurred at the onset of the Little Ice Age, which started in the Alps around 1260 AD and ended at about 1860 AD 44 .…”
Section: Resultsmentioning
confidence: 99%
“…The onset of ice accumulation at Mörkgletscher around 3.2 kyr BP may have been related to an episode of glacier advance in the Alps, known as the Göschenen 1 advance and more recently called Iron Age Advance Period 1, starting around 3 kyr BP 43 . The change towards a higher mean accumulation rate during approximately the thirteenth century AD occurred at the onset of the Little Ice Age, which started in the Alps around 1260 AD and ended at about 1860 AD 44 .…”
Section: Resultsmentioning
confidence: 99%
“…Glacier variations were early linked to climate evolution in the region (e.g., Venetz, 1833). Later, improved knowledge about the climate sensitivity of Alpine glaciers has made them appear as the best suited proxies to reconstruct climate variability over a wide range of timescales during the Holocene (Oerlemans, 2005;Lüthi, 2014;Le Roy et al, 2024).…”
Section: Introductionmentioning
confidence: 99%
“…Based on historical sources and tree-ring dating three main periods of glacier maxima (14th, 17th and 19th centuries) have been identified in the Alps (Zumbühl and Holzhauser, 1988;Holzhauser et al, 2005;Nicolussi et al, 2022). As the most recent period of sustained glacier activity during the Holocene (Le Roy et al, 2024), the LIA can be used as an analogue to understand the triggers responsible for previous cold periods. Proposed main forcings for the LIA multi-secular cooling include solar activity and clusters of volcanic eruptions (Brönnimann et al, 2019).…”
mentioning
confidence: 99%
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