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Open AccessJournal ArticleDOI

Recent Retreat Glaciar Nef, Chilean Patagonia, Dated by Lichenometry and Dendrochronology

TLDR
In this paper, the authors present the results of a lichenometric and dendrochronological study of the recent retreat history of Glaciar Nef, an eastern outlet glacier of the Hielo Patag6nico Norte.
Abstract
This paper presents the results of a lichenometric and dendrochronological study of the recent retreat history of Glaciar Nef, an eastern outlet glacier of the Hielo Patag6nico Norte. A 600-yr tree regeneration time, based on maximum tree age in the ancient forest, suggests that the forest-clad lateral moraines in the valley, southeast of the 19th century terminal moraine system, were formed some time before A.D. 1370. Dating estimates suggest that retreat from a 19th century maximum began around 1863, a decade or two earlier than the date established for other glaciers in the region, with glacier thinning near the ice front averaging 1.11 m yr- between 1863-1881. After 1884, retreat seems to have slowed, with glacier thinning averaging 0.09 m yr-~. Lichen and tree dating suggests that the glacier had retreated approximately 500 m by 1938; this estimate is supported by an aerial photograph showing a proglacial lake just beginning to form in 1944. Recent glacier movements around the Hielo Patagonico Norte are discussed and it is concluded that the general trend of glacier retreat around the icefield, beginning in the 1860s to 1870s, is consistent with Northern Hemisphere trends.

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Glacier fluctuations in extratropical South America during the past 1000 years

TL;DR: In this paper, the authors presented an updated, extensive review of glacier fluctuations during the past 1000 years in the extratropical Andes of South America between ca. 17° and 55°S.
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Late Pleistocene and Holocene palaeoclimate and glacier fluctuations in Patagonia

TL;DR: The evidence for Late Pleistocene and Holocene palaeoclimate and glacier fluctuations of the two major icefields in Patagonia, the Hielo Patagonico Norte (47°00′S, 73°39′W) and the hielo Pico Sur (between 48°50′S and 51°30′S) is presented in this article.
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The chronology of the last glacial maximum and deglacial events in central Argentine Patagonia

TL;DR: In this article, the authors provide a direct chronology for the age of the Rio Blanco moraine system by utilizing cosmogenic-nuclide surface exposure ages, which indicates the last glacial maximum (LGM) maximum extent occurred by 27-25-ka and subsequent advances occurred at 23-22-ka, 20-18-k, and ca. 18-17-k.
References
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The Little Ice Age

Jean M. Grove
TL;DR: The evidence for the Little Ice Age, the most important fluctuation in global climate in historical times, is most dramatically represented by the advance of mountain glaciers in the sixteenth and seventeenth centuries and their retreat since about 1850 as discussed by the authors.

Little Ice Age

TL;DR: The Neoglacial period as discussed by the authors is the most extensive recent period of mountain glacier expansion and is conventionally defined as the 16th-mid 19th century period during which European climate was most strongly impacted.
Journal ArticleDOI

The Little Ice Age in the Canadian Rockies

TL;DR: This article reviewed the evidence and history of glacier fluctuations during the Little Ice Age (LIA) in the Canadian Rockies and concluded that the use of the term LIA should be restricted to describing a period of extended glacier cover rather than being used to define a period with specific climate conditions.
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The Patagonian Icefields: A Glaciological Review

TL;DR: In this paper, the authors studied the anomalous behavior of certain calving glaciers, the oscillations of which contrast in magnitude, timing and sign with each other and with non-calving glaciers.
Journal ArticleDOI

The calving glaciers of southern South America

TL;DR: A review of recent research in the region in the context of glaciological and Quaternary debates, and discusses current understanding and uncertainties can be found in this paper, where the relative importance of climatic, topographic and glaciodynamic controls on regional patterns of glacier fluctuation remain an enigma, especially in the Cordillera Darwin, but space-borne radar imagery is now yielding much information.
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