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Glacial boundary

A glacial boundary is a line on a map representing the farthest advance of a glacier that has retreated. It generally refers to the extent of… Expand
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Papers overview

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Highly Cited
2013
Highly Cited
2013
Abstract Mapping and forty-seven new 10 Be ages help define the timing of glaciation in the Ladakh and Pangong Ranges in… Expand
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Highly Cited
2009
Highly Cited
2009
With the recent rise of phylogeography, the biogeography of mountain species (species with their current main distribution above… Expand
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Highly Cited
2008
Highly Cited
2008
The speed of a glacier is affected most by sudden jumps in the water supply to the glacier, but it goes back to previous levels… Expand
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Highly Cited
2008
Highly Cited
2008
The term ‘refugia’ was originally used to describe the restricted full-glacial locations of modern mid- and high-latitude taxa… Expand
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Highly Cited
2007
Highly Cited
2007
[1] We use an Earth system model of intermediate complexity, CLIMBER-2, to investigate what recent improvements in the… Expand
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Highly Cited
2005
Highly Cited
2005
Abstract Temporal and spatial changes in glacier cover throughout the Late Quaternary in Tibet and the bordering mountains are… Expand
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Highly Cited
2004
Highly Cited
2004
The terrestrial glacial record reflects past snowline variability and atmospheric temperature changes. When combined with secure… Expand
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Highly Cited
2003
Highly Cited
2003
Aim To locate glacial refugia of thermophilous plant species in Spain. Methods We use pollen found in cave sediments as a source… Expand
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Highly Cited
1998
Highly Cited
1998
Northwestern Europe remains a key region for testing models of glacial isostasy because of the good geological record of crustal… Expand
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Highly Cited
1995
Highly Cited
1995
Long-term weathering rates ( RLT ) were determined from base cation depletion in soil profiles developed on six granitic glacial… Expand
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