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doi: 10.24412/2687-1092-2022-9-112-116 1 Computer and Software Engineering Department, Polytechnique Montréal, Montreal, Canada 2 Earth Cryosphere Institute FRS Tyumen Science Center SB RAS, Tyumen, Russia 3 Tyumen State University, Tyumen, Russia
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Abstract. Paleoglaciological modelling were carried out for sectors of the North Europe and west of the Arctic. For same bed topography for different profils of British–Irish, Scandinavian and Barents–Kara Ice Sheet during the MIS1, we are in our research launched a whole ensemble of simulations with noisy accumulation rates. We can also control during our modelling the mean accumulation rate, which varies the evolving position of the grounding line over the course of the simulation. We can also experiment the standard deviation of the accumulation rate, drawn from a Gaussian distribution, which varies the spread of evolving position of the grounding line over the course of the simulation. Keywords: Late Pleistocene, Arctic, paleoglaciological modeling, grounding line, accumulation rate
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Cite this article:
Kashdan A.Y., Sheinkman V.S. 2022. Surface balance and grounding line of ancient Arctic ice sheets // Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. Issue 9. P. 112-116. doi: 10.24412/2687-1092-2022-9-112-116
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