In a new study, Box and a team of researchers describe the decline in ice sheet reflectivity and the reasons behind it, noting that if current trends continue, the area of ice that
melts during the summer season is likely to expand to cover all of Greenland for the first time in the observational record, rather than just the lower elevations at the edges of the continent, as is the case today.
Many rivers draining glaciated regions, particularly in the Hindu Kush - Himalaya and the South - American Andes, are sustained by glacier
melt during the summer season (Singh and Kumar, 1997; Mark and Seltzer, 2003; Singh, 2003; Barnett et al., 2005).
Not exact matches
Between 1995 and 2013 — when the Arctic began warming disproportionately fast — extreme undulations over North America
during the
summer and autumn, the
seasons when the Arctic
melts, were 49 and 41 per cent more common than they were between 1979 and 1994.
The reason: until the end of the
melting season the fate of the ice is ultimately determined by the wind conditions and air and water temperatures
during the
summer months.
The lowest extent on record came
during the remarkable
summer melt season of 2012, fueled in part by
summer storms that moved ice into warm waters.
What the scientists think happened was that the traditionally older, thicker ice around Greenland and the Canadian archipelago «just didn't
melt away as much as it usually would»
during the cooler
summer conditions, «and it kind of just remained over the
summer melt season,» Tilling said.
For example, the 2012 record minimum came
during the remarkable
summer melt season of 2012 and was fueled in part by
summer storms that moved ice into warm waters.
Arctic sea ice has been shrinking more rapidly, falling to its lowest volume and second lowest area on record
during the 2011
summer melt season.
Using this approach and taking into consideration that the survivability of ice
during the
summer melt season has changed in recent years, gives us an average estimate of 4.59 106km2, using ice survival rates from the last 5
summers.
Annual net balance on eight North Cascades glaciers
during the 1984 - 1994 period has been determined by measurement, of total mass loss from firn and ice
melt and, of residual snow depth at the end of the
summer season.
Note, that
during Arctic
summer season (May - September) the ice type product is dubious because
melting of the ice surface obscures the ice type signals.
During Arctic
summer season (May - September) the ice type product is dubious because
melting of the ice surface obscures the ice type signals.
If northern Siberia does not heat up, then the necessary depressions may not form in the northern part of the Urals and the coming
melting season could look more like 2007 and 2012 with significant high pressure areas over the sea ice
during summer months.
Hence, especially
during the
summer melting season a different variability is detected, leading to slightly different stability maps of the climatological variables.
Of the 15 million square kilometers (5.8 million square miles) of sea ice that exist
during winter, on average, 7 million square kilometers (2.7 million square miles) remain at the end of the
summer melt season.
The
summer melt season usually begins in March and ends sometime
during September.
Increased surface
melting, loss of ice shelves, and reduction of
summer and autumn sea ice around the Antarctic and Greenland continents
during the warmest interglacials would have a year - round effect on temperature, because the increased area of open water has its largest impact on surface air temperature in the cool
seasons.