This is summarized as a deglaciation map of the Fennoscandian Ice Sheet with isochrons marking every 1000 years between 22 and 13 cal kyr BP and every hundred years between 11.6 and final ice decay after 9.7 cal kyr BP.Deglaciation patterns vary across the Fennoscandian Ice Sheet domain, reflecting differences in climatic and geomorphic settings as well as ice sheet basal thermal conditions and terrestrial versus marine margins.For example, the LGM extent of the ice sheet in northwestern Russia was located far east and it occurred at a later time than the rest of the ice sheet, at around 17–15 cal kyr BP.We also propose a slightly different chronology of moraine formation over southern Sweden based on improved correlations of moraine segments using new Li DAR data and tying the timing of moraine formation to Greenland ice core cold stages.You get access to thousands of profiles of your choice without registration and just in case you want contact somebody, just sign up in 3 easy steps free of charge. We have compiled a detailed questionnaire which incorporates your search criteria and your personal characteristics (these are not obligatory but offer additional match criteria for members).
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Retreat rates vary by as much as an order of magnitude in different sectors of the ice sheet, with the lowest rates on the high-elevation and maritime Norwegian margin.
Retreat rates compared to the climatic information provided by the Greenland ice core record show a general correspondence between retreat rate and climatic forcing, although a close match between retreat rate and climate is unlikely because of other controls, such as topography and marine versus terrestrial margins.
The union, which represents almost 1 million members, or a fifth of the Finnish population, said the model being tested is, “impossibly expensive, since it would increase the government deficit by about 5 per cent” of gross domestic product.
In March, Ontario, Canada's largest province, announced it was trialling a similar universal basic income scheme.