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NEMOSID SIGNED

Next-generation Modeling of Sedimentary Ice-sheet Dynamics

Total Cost €

EC-Contrib. €

Partnership

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NEMOSID project word cloud

Explore the words cloud of the NEMOSID project. It provides you a very rough idea of what is the project "NEMOSID" about.

shortcomings sedimentary flows mass reshaped deposits sheet projections incorporating coupled ice depositional saturated climate antarctic glacier assume weak dynamical deriving basal flow water laboratory fast predicted hydrology mean moving sediment model primarily sensitivity glaciations previously contributor patterns constrained century 21st wedges sea humanitarian evolution contemporary sliding transport grand framework global subglacial friction realistic accelerates models accuracy biggest investigation landforms undulations perturbation environment experiments

Project "NEMOSID" data sheet

The following table provides information about the project.

Coordinator	AARHUS UNIVERSITET Organization address address: NORDRE RINGGADE 1 city: AARHUS C postcode: 8000 website: www.au.dk contact info title: n.a. name: n.a. surname: n.a. function: n.a. email: n.a. telephone: n.a. fax: n.a.
Coordinator Country	Denmark [DK]
Total cost	219˙312 €
EC max contribution	219˙312 € (100%)
Programme	1. H2020-EU.1.3.2. (Nurturing excellence by means of cross-border and cross-sector mobility)
Code Call	H2020-MSCA-IF-2019
Funding Scheme	MSCA-IF-EF-RI
Starting year	2020
Duration (year-month-day)	from 2020-07-01 to 2022-06-30

Partnership

Take a look of project's partnership.

#	participants	country	role	EC contrib. [€]
1	AARHUS UNIVERSITET AARHUS UNIVERSITET Organization address address: NORDRE RINGGADE 1 city: AARHUS C postcode: 8000 website: www.au.dk contact info title: n.a. name: n.a. surname: n.a. function: n.a. email: n.a. telephone: n.a. fax: n.a.	DK (AARHUS C)	coordinator	219˙312.00

Map

Project objective

Global sea level changes are grand humanitarian challenges in the 21st century and beyond. The biggest contributor and uncertainty to sea-level projections is dynamical ice-mass loss from the Antarctic Ice Sheet. Fast-moving ice primarily flows by sliding over weak and water-saturated sedimentary deposits that are reshaped into undulations and depositional wedges in the process. Current ice-sheet models do not account for transport of sediment under ice, and commonly assume that basal friction increases if ice flow accelerates. In this project I propose to address these shortcomings by deriving a realistic coupled framework for glacier ice, water and sediment. The sediment model is constrained by laboratory experiments and is coupled to a new model of subglacial hydrology. The ice-water-sediment model is compared to landforms and sedimentary deposits from previous glaciations, as well as contemporary ice sheet flow patterns. The framework allows analysis of climate-perturbation sensitivity, with particular investigation into the dynamical evolution of ice flow and basal environment. By incorporating previously neglected processes, the developed model framework will improve the accuracy of predicted global-mean sea-level change in the future.

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The information about "NEMOSID" are provided by the European Opendata Portal: CORDIS opendata.