Eemian Greenland ice sheet simulated with a higher-order model shows strong sensitivity to surface mass balance forcing

influenced directly by our actions. More commonly, the actor is influenced indirectly by threats posed against the assets we believe are vital to him. Possible targets may be symbolic

List of the 13 models used in this study listing the type (energy balance model (EBM), regional climate model (RCM), general circulation model (GCM), positive degree day (PDD)

In this study, a global climate model (NorESM) and a re- gional climate model (MAR), constrained by global climate output, are used to estimate the SMB during the Eemian

and Sættem, J., 2001: Glacial processes and large-scale morphology on the mid-Norwegian continental shelf, a dynamic ice-sheet model with the palaeo-ice streams and intermediate

The two different grids in the polythermal ice sheet model and the fact that the ice extent and the thicknesses of cold and temperate ice changes with time makes the

The SWIPA Project is being conducted according to three main Arctic cryosphere components: sea ice, the Greenland Ice Sheet, and the terrestrial cryosphere, composed of

This study follows the more traditional approach of seeing interaction designing as dealing with digital materials as it engages with SR-RFID as design material.

The lack of well-constrained limits on the eastern margin of the BSIS in the Kara Sea (cf. Hughes et al., 2016) makes this region particularly dif fi cult to resolve with any con