Review of Survey activities 2013: Katabatic winds and piteraq storms: observations from the Greenland ice sheet

Consequences of a warmer climate on the Greenland Ice Sheet (GrIS) mass balance will be a thickening inland, due to increased solid precipitation, and a thinning at the GrIS

Since the PROMICE stations measure close to the ice surface where temperature variability is dampened over a melting surface, a stronger correlation could be expected between

(1998) is typical, it yields a loss rate of 0.14 % a − 1 if applied to the whole Greenland ice perimeter divided by Greenland ice area, or 0.006 % a − 1 if applied to the

We apply the method to calculate depth-averaged ve- locities of the Greenland Ice Sheet, and find that the method produces grid-independent velocity fields for a sufficient

To assess the effect of direct signal transmission or horizon- tal coupling on the dynamic response of the GrIS over the next century, five model versions of a 3-D ice-dynamic

In 2004 the Geological Survey of Denmark and Greenland (GEUS) initiated a study of the origin and tectono-meta- morphic evolution of greenstone belts and important regio- nal

With the main focus on hydrogeology and the urban water cycle, the Municipality of Odense, the local water- works (VandCenter Syd), the Geological Survey of Den- mark and

The SMB anomaly projection for k = a/b =− 1 as well as the cumulated sea level rises equivalent are shown in Fig. This record surface mass loss rate is likely to become com- mon at