Recent changes in Arctic sea ice melt onset, freeze - up, and
melt season length.
Not exact matches
Then if we find the winter max and summer minimum each year we can look at the how the
length of the
melting season changes:
This phase change of water causes a powerful local feedback, which, together with moderate global warming, can substantially increase the
length of the
melt season.
Large - scale warming in the Arctic [Johannessen et al., 2004] has resulted in an extension of the
length of the summer
melt season over sea ice [Smith, 1998; Rigor et al., 2000], thawing permafrost [Osterkamp and Romanovsky, 1999], and near - coastal thinning and overall shrinkage of the Greenland ice sheet [Krabill et al., 1999; Lemke et al., 2007, and references therein].
As one goes further north toward the North Pole, the
length of the shortwave radiation
season is shortened with less ability to
melt out multi-year sea ice (D. Perovich, personal communication).
According to the press release: «This trio of images shows changes between 1979 and 2007 in the average date of
melt onset in the spring (left), the first autumn freeze (center), and the total average increase in the
length of the Arctic sea ice
melt season.
According to the press release: «The graph -LSB-...] illustrates how the
length of the
melt season varies significantly from year to year, but the long - term trend is clear.»
The
melting season — i.e. the
length of time in which continuous
melting occurs — has increased on average by 6.4 days for every decade between 1979 and 2007.
Over the past quarter - century, both the extent of
melting and the
length of the
melt season on the Greenland ice sheet have been growing, as local temperatures have risen.6 Satellites measure the extent of
melting by differentiating between areas of the ice mass that are fully frozen and those with surface meltwater.
The Greenland ice sheet is
melting at an accelerating rate, with both the extent of
melting and the
length of the
melt season growing.
Both the extent of
melting and the
length of the
melt season on Greenland are growing.
Every element of the hydrologic cycle, to some degree, is temperature dependent: when it snows versus when it rains; when it
melts, how much evaporates; how much water the plants use; the
length of the growing
seasons.