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Frank Lamy

Researcher at Alfred Wegener Institute for Polar and Marine Research

Publications -  152
Citations -  7008

Frank Lamy is an academic researcher from Alfred Wegener Institute for Polar and Marine Research. The author has contributed to research in topics: Glacial period & Holocene. The author has an hindex of 42, co-authored 141 publications receiving 6103 citations. Previous affiliations of Frank Lamy include University of Bremen & Deutsche Forschungsgemeinschaft.

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Holocene rainfall variability in southern Chile: a marine record of latitudinal shifts of the Southern Westerlies

TL;DR: In this paper, a high accumulation marine sediment core from the Chilean continental slope (41‡S) provides a 7700 yr record of rainfall variability in southern Chile related to the position of the Southern Westerlies.
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Antarctic timing of surface water changes off Chile and Patagonian ice sheet response.

TL;DR: Marine sediments from the Chilean continental margin are used to infer millennial-scale changes in southeast Pacific surface ocean water properties and Patagonian ice sheet extent since the last glacial period, showing a clear “Antarctic” timing of sea surface temperature changes.
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Holocene changes in the position and intensity of the southern westerly wind belt

TL;DR: In this article, the authors used sedimentological and pollen records to reconstruct precipitation patterns over the past 12,500 yr from sites along the windward side of the Andes, and found a distinct anti-phasing of wind strength between the core and northern margin over multimillennial timescales.
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Mediterranean Moisture Source for an Early-Holocene Humid Period in the Northern Red Sea

TL;DR: It is concluded that Afro-Asian monsoonal rains did not cross the subtropical desert zone during the early to mid-Holocene and is best explained by enhancement and southward extension of rainfall from Mediterranean sources.
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Coherent high- and low-latitude control of the northwest African hydrological balance

TL;DR: In this paper, the authors studied the development of the hydrological balance during the Pleistocene period and found that the change in humidity may be related to changes in the strength of the North Atlantic meridional overturning circulation.