pre-printA perennial storage of water in a firn aquifer was discovered in southeast Greenland in 2011. We present the first in situ measurements of the aquifer, including densities and temperatures. Water was present at depths between ~12 and 37m and amounted to 18.7 ± 0.9 kg in the extracted core. The water filled the firn to capacity at ~35m. Measurements show the aquifer temperature remained at the melting point, representing a large heat reservoir within the firn. Using model results of liquid water extent and aquifer surface depth from radar measurements, we extend our in situ measurements to the Greenland ice sheet. The estimated water volume is 140 ± 20 Gt, representing ~0.4mm of sea level rise (SLR). It is unknown if the aquifer tem...
Approximately half of Greenland's current annual mass loss is attributed to runoff from surface melt...
In spring of 2011, a perennial storage of water was observed in the firn of the southeastern Greenla...
Firn aquifers in Greenland store liquid water within the upper ice sheet and impact the hydrological...
A perennial storage of water in a firn aquifer was discovered in southeast Greenland in 2011. We pre...
The accelerating loss of mass from the Greenland ice sheet is a major contribution to current sea le...
pre-printRecent observations have shown that the firn layer on the Greenland Ice Sheet features subs...
The delivery of surface meltwater through englacial drainage systems to the bed of the Greenland Ice...
The delivery of surface meltwater through englacial drainage systems to the bed of the Greenland Ice...
Recent observations of the Greenland ice sheet show an increase of the area affected by progressive ...
Poorly understood processes controlling retention of meltwater in snow and firn have important impli...
Within the lower percolation zone of the southeastern Greenland ice sheet, meltwater has accumulated...
Approximately half of Greenland's current annual mass loss is attributed to runoff from surface melt...
In spring of 2011, a perennial storage of water was observed in the firn of the southeastern Greenla...
Firn aquifers in Greenland store liquid water within the upper ice sheet and impact the hydrological...
A perennial storage of water in a firn aquifer was discovered in southeast Greenland in 2011. We pre...
The accelerating loss of mass from the Greenland ice sheet is a major contribution to current sea le...
pre-printRecent observations have shown that the firn layer on the Greenland Ice Sheet features subs...
The delivery of surface meltwater through englacial drainage systems to the bed of the Greenland Ice...
The delivery of surface meltwater through englacial drainage systems to the bed of the Greenland Ice...
Recent observations of the Greenland ice sheet show an increase of the area affected by progressive ...
Poorly understood processes controlling retention of meltwater in snow and firn have important impli...
Within the lower percolation zone of the southeastern Greenland ice sheet, meltwater has accumulated...
Approximately half of Greenland's current annual mass loss is attributed to runoff from surface melt...
In spring of 2011, a perennial storage of water was observed in the firn of the southeastern Greenla...
Firn aquifers in Greenland store liquid water within the upper ice sheet and impact the hydrological...