The
Melting Arctic
From: Roger Greenway, ENN.com
As the Eastern US ends
what seems to have been the most severe winter in memory, it is hard to
remember that the global climate is still warming. A severe winter in a region
doesn't mean that the entire hemisphere had an extreme winter. And it really
doesn't imply much about long term trends. A key indicator of long term trends
is the length of the Arctic melt season.
A new study by researchers from the National Snow and Ice Data Center (NSIDC) and NASA shows that the length of the melt season for Arctic sea ice is growing by several days each decade. An earlier start to the melt season is allowing the Arctic Ocean to absorb enough additional solar radiation in some places to melt as much as four feet of the Arctic ice cap’s thickness.
A new study by researchers from the National Snow and Ice Data Center (NSIDC) and NASA shows that the length of the melt season for Arctic sea ice is growing by several days each decade. An earlier start to the melt season is allowing the Arctic Ocean to absorb enough additional solar radiation in some places to melt as much as four feet of the Arctic ice cap’s thickness.
Arctic sea ice has been
in sharp decline during the last four decades. The sea ice cover is shrinking
and thinning, making scientists think an ice-free Arctic Ocean during the
summer might be reached this century. The seven lowest September sea ice
extents in the satellite record have all occurred in the past seven years.
To study the evolution
of sea ice melt onset and freeze-up dates from 1979 to the present day,
Stroeve’s team used passive microwave data from NASA’s Nimbus-7 Scanning
Multichannel Microwave Radiometer, and the Special Sensor Microwave/Imager and
the Special Sensor Microwave Imager and Sounder carried onboard Defense
Meteorological Satellite Program spacecraft. When ice and snow begin to melt,
the presence of water causes spikes in the microwave radiation that the snow
grains emit, which these sensors can detect.
Results show that
although the melt season is lengthening at both ends, with an earlier melt
onset in the spring and a later freeze-up in the fall, the predominant
phenomenon extending the melting is the later start of the freeze season.
Some
areas, such as the Beaufort and Chukchi Seas, are freezing up between six and
11 days later per decade. Although melt onset variations are smaller, the
timing of the beginning of the melt season has a larger impact on the amount of
solar radiation absorbed by the ocean, because its timing coincides with when
the sun is higher and brighter in the Arctic sky.
Despite large regional
variations in the beginning and end of the melt season, the Arctic melt season
has lengthened on average by five days per decade from 1979 to 2013. Credit:
NASA