ISCLIM
Polar Ice sheets in the climate system

Assessing the future of the polar ice sheets and their impact on climate and sea levels.

Project lead:
Gaël DURAND (CNRS – IGE)

Co-leads:
Sylvie CHARBIT (LSCE-IPSL)
Christophe DUMAS (LSCE-IPSL)

The ISCLIM project aims to study the evolution of the polar ice sheets and their interactions with the climate system. In particular, it aims to better constrain projections of the contribution of the polar ice sheets to sea level rise and the effects on other components of the climate system.

PC9 ISCLIM will establish a hierarchy of numerical approaches to improve the assessment of the impacts and feedbacks of the ice sheets on the climate system through four actions:

1. Development of ice-sheet models capable of reproducing as closely as possible currently observed changes and producing projections on different time scales (over 100 years or simulating major quaternary deglaciations and rapid events).

2. Improve the description of ocean circulation in subglacial cavities and fjords, and its interactions with outflowing glaciers.

3. Improve the description of atmospheric and surface processes and their relationship to the evolution of the physical properties of snow cover and surface elevation.

4. To represent the feedbacks of ice sheets with the ocean and atmosphere using approaches of varying complexity, ranging from parameterisation to explicit coupling of an ice sheet model, whatever the resolution used in Earth system models.


Developthe polar ice sheet models of tomorrow

Refine the description of the processes impacting the polar ice sheets from seasonal time scales (e.g. calving) to multimillennial time scales (e.g. isostasy).


Model sheet-ocean interfaces

Improve estimates of melting under ice shelves and on vertical ice faces at the bottom of fjords at low resolution, integrating the effect of ice sheets into the global ocean freshwater cycle.


Model sheet-atmosphere interfaces

Improve the representation of the atmosphere and exchanges with the surface at high latitudes, and develop coupling with a snow model on the polar ice sheets in order to simulate a surface mass balance in better agreement with observations.


Anticipate changes in the polar ice sheets and feedback from the climate system

Refine decadal to multi-millennial projections of sea-level rise, taking into account the instability mechanisms of the polar ice sheets , and to assess the impact on oceanic and atmospheric circulation.

CEA, CNRS, Météo-France, UGA


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