Not exact matches
Further the glacier data suggests we did not at least for a portion
of the LGM, since there is no way to note how long the glaciers were at the depressed
snowline location.
[Response: You're absolutely right to point out that the mountain
snowline data was a critical part
of unraveling the tropical LGM puzzle.
The result: more winter precipitation falling as rain instead
of snow, two - tenths
of an inch to more than half an inch a day, pushing the
snowline in the mountains up from 3,000 feet to higher than 4,000 feet.
No matter what your reasons for visiting,
Snowline is trully central to all the attractions
of the area.
Peppers Rundells Alpine Lodge is located above the
snowline at 1565m altitude in the heart
of the Victorian Alps surrounded by the Alpine National Park and centrally positioned just 10 minutes from both Mount Hotham Airport and Mount Hotham Ski Resort.
For example, the uniform lowering
of tropical
snowline by about 900 meters during the Last Glacial Maximum is generally attributed to cooling [Porter 2001], and indeed provided the first indication that something was wrong with plankton - based estimates
of tropical cooling during the glacial period.
[Response: You're absolutely right to point out that the mountain
snowline data was a critical part
of unraveling the tropical LGM puzzle.
Is there enough ice, and is the
snowline likely to rise fast enough for the rate
of iceloss to significantly decrease the pressure on underground magma?
Further the glacier data suggests we did not at least for a portion
of the LGM, since there is no way to note how long the glaciers were at the depressed
snowline location.
Amount
of advance or retreat
of the glacier snout is as much about snow accumulation above the permanent
snowline as temperature.
The albedo change resulting from the
snowline retreat on land is similarly large as the retreat
of sea ice, so the combined impact could be well over 2 W / sq m. To put this in context, albedo changes in the Arctic alone could more than double the net radiative forcing resulting from the emissions caused by all people
of the world, estimated by the IPCC to be 1.6 W / sq m in 2007 and 2.29 W / sq m in 2013.»