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- W4220997756 abstract "<p>Compared with the intensely studied interval of the last glacial maximum and termination, significantly less attention has been given to the preceding glacial period and Termination 2. This is perhaps understandable as the Greenland ice cores do not stretch this far back in time and the terrestrial record of the ice sheets has in part been lost during the subsequent glacial period. However, there are many questions remaining about how these two glacial intervals differed and whether this was important in driving some of the differences between the last interglacial and our current interglacial. Here I&#8217;ll present transient ice sheet modelling results of the northern hemisphere ice sheets through the last two glacial terminations. This work was stimulated by a new speleothem record from northern Spain that records the meltwater-driven d18O anomaly in the eastern North Atlantic and provides an absolutely dated chronology (U/Th) during the penultimate glacial and Termination 2. The character of which differs dramatically from a record for Termination 1 recovered from speleothems at the same site. I&#8217;ll discuss some possible reasons for the differences between the two glacial terminations recorded at this site and present model experiments to test these hypotheses and whether this can explain some of the differences between the last interglacial and our current interglacial.&#160;</p>" @default.
- W4220997756 created "2022-04-03" @default.
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- W4220997756 date "2022-03-28" @default.
- W4220997756 modified "2023-10-16" @default.
- W4220997756 title "Differences in the rates and character of the last two glacial terminations and impacts on the following interglacials" @default.
- W4220997756 doi "https://doi.org/10.5194/egusphere-egu22-7456" @default.
- W4220997756 hasPublicationYear "2022" @default.
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