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  1. 16 sie 2019 · Our reconstructions illustrate pronounced ice-sheet asymmetry within the last glacial cycle and significant variations in ice-marginal positions between older glacial cycles.

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  2. 27 lip 2021 · Glacier ice covers about 10% of Earth's land surface and has a profound influence on human activity. As ice continues to melt around the world in response to anthropogenic and natural global heating, the dynamics of glaciers and ice sheets are changing.

  3. 23 lut 2021 · Glacial isostatic adjustment (GIA)-based ice sheet reconstructions are commonly used for paleoclimate modeling and assessing present-day Earth deformation and sea-level change. As a result,...

  4. We have spearheaded methods to collect invaluable field data and developed new computer modelling techniques to monitor and predict changes in the Earth's ice-covered regions. Our work is providing key input to climate change decision-making worldwide.

  5. 1 sty 2021 · SROCC reviewed post-AR5 Greenland-scale ice sheet model studies that used higher resolution and updated boundary conditions (Aschwanden et al., 2019), higher-order representations of ice flow (Fürst et al., 2015), more explicit representations of ice sheet processes (Calov et al., 2018), and accounted for coupling between the ice sheet and ...

  6. 22 gru 2021 · This paper introduces the Instructed Glacier Model (IGM) – a model that simulates ice dynamics, mass balance and its coupling to predict the evolution of glaciers, icefields or ice sheets.

  7. 23 lut 2018 · GRANTISM (GReenland and ANTarctic Ice Sheet Model) is an educational Excel™ model introduced by Pattyn (2006). Here, GRANTISM is amended to simulate the Svalbard-Barents-Sea Ice Sheet during the Last Glacial Maximum, an analogue for the contemporary West Antarctic Ice Sheet.

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