When
seasonal ice retreat occurs early, low - albedo open water areas are exposed early, which gain a lot of energy from the sun.
At the same time, as the melt season advances, the importance of solar heating, one of the main drivers of
seasonal ice retreat, starts to wane due to increasing cloudiness and lower solar elevations.
With lack of multiyear ice, a normal or slightly below - normal thickness offshore ice cover (based on ice thickness flights earlier in the season) and coastal ice vulnerable to early break - up, ice conditions would favor a normal or somewhat early
seasonal ice retreat.
But will probably end up as the third - or fourth - greatest
seasonal ice retreat on record.
Arctic researchers caution that there is something of a paradox in Arctic trends: while the long - term fate of the region may be mostly sealed, no one should presume that the recent sharp warming and
seasonal ice retreats that have caught the world's attention will continue smoothly into the future.
Not exact matches
«This study was the first to quantitatively elucidate that
ice - ocean albedo feedback is a primary driver of
seasonal and yearly variations in Arctic sea
ice retreat,» says Kay I. Ohshima.
, then at the
seasonal cycle (what does the sea
ice advance and
retreat look like?
And as technology improves, oil prices rise and the
seasonal ice cap
retreats, countries like Norway and Russia are acting with startling speed.
Variability, trends, and predictability of
seasonal sea
ice retreat and advance in the Chukchi Sea.
27 January 2000: The Hektoria Glacier system is stable, but increased summer melting from climate warming in the 1980s and 1990s affected the glacier system in two ways: (1) a
seasonal speedup from summer melt water percolating through the glacier
ice to its base, and (2) initial retreat of the Larsen Ice Shelf due to the effects of melt ponds (downstream from this imag
ice to its base, and (2) initial
retreat of the Larsen
Ice Shelf due to the effects of melt ponds (downstream from this imag
Ice Shelf due to the effects of melt ponds (downstream from this image).
Seasonal sea
ice retreat in 2012 began with a major reduction event in early June (Figure 2) associated with persistent high pressure over the Beaufort Sea and low pressure over the Kara Sea, now referred to as the Arctic Dipole (AD) weather pattern (see discussion of the AD in previous Outlooks).
A recent study by NSIDC scientists Mark Serreze, Julienne Stroeve, and Alexander Crawford, along with University of Washington scientist Rebecca Woodgate, demonstrates strong links between
seasonal sea
ice retreat and advance in the Chukchi Sea and the inflow of ocean heat into the region through the Bering Strait.
It is undergoing dramatic change with
retreat of the permanent, as well as
seasonal,
ice.
Record
seasonal retreats of sea
ice northward into the Chukchi and Beaufort seas were reported for 2002 - 2005 [258], but they were exceeded by
ice retreats in 2007 and 2008 [255].
Interestingly, in the Seasonally
Ice - free Zone (SIZ, the band located between the winter and summer sea ice edge), this production is highly stimulated by increased iron availability due to the seasonal sea ice retre
Ice - free Zone (SIZ, the band located between the winter and summer sea
ice edge), this production is highly stimulated by increased iron availability due to the seasonal sea ice retre
ice edge), this production is highly stimulated by increased iron availability due to the
seasonal sea
ice retre
ice retreat.