Giant boulders and Last Interglacial storm intensity in the North Atlantic

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Giant boulders and Last Interglacial storm intensity in the North Atlantic.

As global climate warms and sea level rises, coastal areas will be subject to more frequent extreme flooding and hurricanes. Geologic evidence for extreme coastal storms during past warm periods has the potential to provide fundamental insights into their future intensity. Recent studies argue that during the Last Interglacial (MIS 5e, ∼128-116 ka) tropical and extratropical North Atlantic cycl...

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Oceanographic dynamics and the end of the last interglacial in the subpolar North Atlantic.

The last interglacial interval was terminated by the inception of a long, progressive glaciation that is attributed to astronomically influenced changes in the seasonal distribution of sunlight over the earth. However, the feedbacks, internal dynamics, and global teleconnections associated with declining northern summer insolation remain incompletely understood. Here we show that a crucial earl...

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Rapid switches in subpolar North Atlantic hydrography and climate during the Last Interglacial (MIS 5e)

[1] At the peak of the previous interglacial period, North Atlantic and subpolar climate shared many features in common with projections of our future climate, including warmer-than-present conditions and a diminished Greenland Ice Sheet (GIS). Here we portray changes in North Atlantic hydrography linked with Greenland climate during Marine Isotope Stage (MIS) 5e using (sub)centennially sampled...

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Rapid reductions in North Atlantic Deep Water during the peak of the last interglacial period.

Deep ocean circulation has been considered relatively stable during interglacial periods, yet little is known about its behavior on submillennial time scales. Using a subcentennially resolved epibenthic foraminiferal δ(13)C record, we show that the influence of North Atlantic Deep Water (NADW) was strong at the onset of the last interglacial period and was then interrupted by several prominent ...

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Causes of Reduced North Atlantic Storm Activity in a CAM3 Simulation of the Last Glacial Maximum

The aim of this paper is to determine how an atmosphere with enhanced mean-state baroclinity can support weaker baroclinic wave activity than an atmosphere with weak mean-state baroclinity. As a case study, a Last Glacial Maximum (LGM) model simulation previously documented to have reduced baroclinic storm activity, relative to the modern-day climate (simulated by the same model), despite havin...

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ژورنال

عنوان ژورنال: Proceedings of the National Academy of Sciences

سال: 2017

ISSN: 0027-8424,1091-6490

DOI: 10.1073/pnas.1712433114