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Matthias Prange

Researcher at University of Bremen

Publications -  160
Citations -  5745

Matthias Prange is an academic researcher from University of Bremen. The author has contributed to research in topics: Climate model & Holocene. The author has an hindex of 40, co-authored 150 publications receiving 4867 citations.

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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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Forcing of wet phases in southeast Africa over the past 17,000 years

TL;DR: It is shown that remote atmospheric forcing by cold events in the northern high latitudes appears to have been the main driver of hydro-climatology in southeast Africa during rapid climate changes over the past 17,000 years.
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Sahel megadroughts triggered by glacial slowdowns of Atlantic meridional overturning

TL;DR: This article reconstructed the history of eolian and fluvial sedimentation on the continental slope off Senegal during the past 57,000 years and found that abrupt onsets of arid conditions in the West African Sahel were linked to cold North Atlantic sea surface temperatures during times of reduced meridional overturning circulation associated with Heinrich Stadials.
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North Atlantic forcing of tropical Indian Ocean climate

TL;DR: It is shown that slowdowns of the Atlantic meridional overturning circulation during Heinrich stadials and the Younger Dryas stadial affected the tropical Indian Ocean hydroclimate through changes to the Hadley circulation including a southward shift in the rising branch (the intertropical convergence zone) and an overall weakening over the southern Indian Ocean.
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Radiocarbon simulations for the glacial ocean: the effects of wind stress, Southern Ocean sea ice and Heinrich events.

TL;DR: In this paper, simulations of oceanic radiocarbon for the last glacial maximum are presented, using a three-dimensional global ocean circulation model forced with glacial background states according to various reconstructions.