| Search results - "melting" |

Ice Hazards19 views"Pedestaling" occurs in summer because structures shade the ice and snow beneath from the sun's heat. Although this supply bag offers an example on a small scale, pedestaling frequently occurred around buildings and large structures. Image credit: EWG.
|
|

Ice Hazards18 viewsA small lead (or crack in the ice) has opened in the foreground. New leads, which form under wind stress when the ice diverges, were a constant threat to the camps. Camps often had to be relocated due to the sudden appearance of an ice lead through the middle of the camp (unless the crack appeared during summer and was simply a melt channel). Image credit: EWG.
|
|

Ice Hazards19 viewsDuring summer, moving around camp became difficult, as melting snow formed large puddles (melt ponds) and channels everywhere. Image credit: EWG.
|
|

Ice Hazards19 viewsHere, melt ponds encroach on many of the buildings in the camp. Sometimes, inflatable boats were used for transportation. Image credit: EWG.
|
|

Ice Hazards17 viewsDuring summer, melt ponds posed hazards to the camp. Here, a station member rows an inflatable raft in a melt pond that has formed in the middle of the camp at NP-6. Image credit: EWG.
|
|

Ice Hazards18 viewsWhen a pond melts, a whirlpool forms, emptying the pond in minutes. This photograph of a melt pond whirlpool is from NP-6. Image credit: EWG.
|
|

Scientific Instruments26 viewsInstrument masts were insulated using mounds of hay to help keep them upright and prevent the snow from melting out from around them. Image credit: EWG.
|
|

214 viewsTide cracks in the sea ice around grounded icebergs; the trail made by the front loader used to collect glacier ice for melting runs through the middle.
Image courtesy Andy Mahoney
|
|

886 viewsThese glaciers used to terminate in the sea; now that they terminate on land, it makes traveling by land via dogsled even more difficult.
Image courtesy Andy Mahoney
|
|

91 viewsAn even closer close-up of the wall of the snow pit, showing a couple of layers in the snow. These particular kinds of layers form when big snow storms occur with strong winds that cause the snow to compact at what was then the surface. Other layers may be caused by melting and refreezing of snow. Photo by John Maurer, CIRES/NSIDC, University of Colorado.
|
|

67 viewsRob Bauer melting down snow for the team.
Image Credit: NSIDC courtesy Ted Scambos and Rob Bauer.
|
|

208 viewsAn in-flight view shows the surface of an iceberg and the melt ponds atop it.
Photo Credit: Courtesy Ted Scambos and Rob Bauer, NSIDC
IceTrek Web site
|
|
|
|