Review of Survey activities 2012: Darkening of the Greenland ice sheet due to the melt-albedo feedback observed at PROMICE weather stations

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

The East Siberian Ice Sheet loses mass by surface melt along all margins except for the Arctic Ocean coast, where the losses occur by calving and shelf basal melt only.. Further

In our case, there are three local maxima of the entropy production rate for the present value of the solar constant, as discussed in the previ- ous section.. We know from the

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

Because of the increas- ing the speed of the decomposition of the anhydrite, together with the growth of the temperature of casting the bronze to the plaster mould, the gases

Observed surface speed of the years 1997 to 2000 as well as calculated fracture density and ice speed in the Larsen B Ice Shelf (a–c). Point-by-point correlation of calculated

The two points considered at the alternate sides, of the tangents through the diameter of the circle, and then the line joining these points divides the circle

Over East China, when the NHS occurs at perihelion, the ice sheets reinforce the summer precipitation due to a wave train topographically induced by the Eurasian ice sheet