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Exploring the extent to which fluctuations in ice‐rafted debris reflect mass changes in the source ice sheet: a model–observation comparison using the last British–Irish Ice Sheet ArchiMer
Wilton, David J.; Bigg, Grant R.; Scourse, James D.; Ely, Jeremy C.; Clark, Chris D..
The British and Irish Ice Sheet (BIIS) was highly dynamic during the Late Quaternary, with considerable regional differences in the timing and extent of its change. This was reflected in equally variable offshore ice‐rafted debris (IRD) records. Here we reconcile these two records using the FRUGAL intermediate complexity iceberg–climate model, with varying BIIS catchment‐level iceberg fluxes, to simulate change in IRD origin and magnitude along the western European margin at 1000‐year time steps during the height of the last BIIS glaciation (31–6 ka bp). This modelled IRD variability is compared with existing IRD records from the deep ocean at five cores along this margin. There is general agreement of the temporal and spatial IRD variability between...
Tipo: Text Palavras-chave: British and Irish Ice Sheet; Coupled model; Deglaciation; Heinrich event; Ice]rafted debris.
Ano: 2021 URL: https://archimer.ifremer.fr/doc/00682/79424/82009.pdf
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Holocene ice-rafting and sediment transport from the glaciated margin of East Greenland (67-70 degrees N) to the N Iceland shelves: detecting and modelling changing sediment sources ArchiMer
Andrews, John T.; Bigg, Grant R.; Wilton, David J..
We examine variations in the ice-rafted sources for sediments in the Iceland/East Greenland offshore marine archives by utilizing a sediment unmixing model and link the results to a coupled iceberg-ocean model. Surface samples from around Iceland and along the E/NE Greenland shelf are used to define potential sediment sources, and these are examined within the context of the down-core variations in mineralogy in the <2 mm sediment fraction from a transect of cores across Denmark Strait. A sediment unmixing model is used to estimate the fraction of sediment <2 mm off NW and N Iceland exported across Denmark Strait; this averaged between 10 and 20%. Both the sediment unmixing model and the coupled iceberg-ocean model are consistent in finding that the...
Tipo: Text Palavras-chave: Holocene; Ice-rafting; Ice bergs; East Greenland; Iceland.
Ano: 2014 URL: https://archimer.ifremer.fr/doc/00290/40150/39091.pdf
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Modelling abrupt glacial North Atlantic freshening: Rates of change and their implications for Heinrich events ArchiMer
Bigg, Grant R.; Levine, Richard C.; Green, Clare L..
The abrupt delivery of large amounts of freshwater to the North Atlantic in the form of water or icebergs has been thought to lead to significant climate change, including abrupt slowing of the Atlantic Ocean meridional overturning circulation. In this paper we examine intermediate complexity coupled modelling evidence to estimate the rates of change, and recovery, in oceanic climate that would be expected for such events occurring during glacial times from likely sources around the North Atlantic and Arctic periphery. We show that rates of climate change are slower for events with a European or Arctic origin. Palaeoceanographic data are presented to consider, through the model results, the origin and likely strength of major ice-rafting, or Heinrich,...
Tipo: Text Palavras-chave: Heinrich events; Modelling; Quaternary; Icebergs.
Ano: 2011 URL: https://archimer.ifremer.fr/doc/00227/33777/82665.pdf
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