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Gisela Winckler

Researcher at Lamont–Doherty Earth Observatory

Publications -  132
Citations -  5176

Gisela Winckler is an academic researcher from Lamont–Doherty Earth Observatory. The author has contributed to research in topics: Glacial period & Last Glacial Maximum. The author has an hindex of 36, co-authored 121 publications receiving 4292 citations. Previous affiliations of Gisela Winckler include Columbia University & University of Idaho.

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Gas hydrate destabilization: enhanced dewatering, benthic material turnover and large methane plumes at the Cascadia convergent margin

TL;DR: In this paper, the authors characterize a newly recognized mechanism of dewatering at convergent margins, where freshening of pore waters from hydrate destabilization at depth and free gas drives fluids upward.
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Covariant glacial-interglacial dust fluxes in the equatorial Pacific and Antarctica.

TL;DR: Equatorial Pacific dust fluxes are highly correlated with global ice volume and withdust fluxes to Antarctica, which suggests that dust generation in interhemispheric source regions exhibited a common response to climate change over late-Pleistocene glacial cycles.
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The magnitude, timing and abruptness of changes in North African dust deposition over the last 20,000 yr

TL;DR: In this paper, the authors present new records from a meridional transect of cores stretching from 311 Nt o 191N along the northwest African margin, which are able to document spatial and temporal changes in dust deposition under the North African dust plume throughout the last 20 ka.
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Increased Dust Deposition in the Pacific Southern Ocean During Glacial Periods

TL;DR: Data sets of glacial-interglacial dust-supply cycles from the largest Southern Ocean sector, the polar South Pacific, are presented, indicating three times higher dust deposition during glacial periods than during interglacials for the past million years.
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Gustiness: The driver of glacial dustiness?

TL;DR: In this paper, a wide range of data supports wind gustiness as a primary driver of global dust levels, with steepened meridional temperature gradients during glacial periods causing increases in dust emissions through increases in the intensity and frequency of highspeed wind events in dust source areas.