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Vanessa Winchester

Researcher at University of Oxford

Publications -  29
Citations -  1119

Vanessa Winchester is an academic researcher from University of Oxford. The author has contributed to research in topics: Glacier & Lichenometry. The author has an hindex of 17, co-authored 27 publications receiving 1076 citations. Previous affiliations of Vanessa Winchester include Mansfield University of Pennsylvania.

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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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Characteristics of tide-water calving at Glaciar San Rafael, Chile

TL;DR: In this paper, the influence of local environmental variables on the magnitude and frequency distributions of calving behavior at glaciersiar San Rafael, Chile was investigated. But the authors were unable to identify the most frequent and frequent calving events.
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A glacial lake outburst flood associated with recent mountain glacier retreat, Patagonian Andes

TL;DR: Harrison, S., Glasser, N. F., Winchester, V., Haresign, E., Warren, C., Jansson, K. as mentioned in this paper reported a glacial lake outburst flood associated with recent mountain glacier retreat, Patagonian Andes.
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Dendrochronology and lichenometry: colonization, growth rates and dating of geomorphological events on the east side of the North Patagonian Icefield, Chile

TL;DR: In this paper, the authors used dendrochronology and lichenometry to estimate tree ages and growth rates in the Arco and Colonia valleys of the North Patagonian Icefield, showing that tree ages below a core height of 112 cm can vary from 5 to 41 years.
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Buoyancy-driven lacustrine calving, Glaciar Nef, Chilean Patagonia

TL;DR: In this article, a hinge-calving mechanism is proposed in which buoyant forces impose a torque on the glacier tongue, resulting in the release of coherent sections of the glacier glacier tongue as tabular ice-bergs.