Not exact matches
«The fact that now a large,
ice - free
area can be
observed in the Weddell
Sea confirms our theory and gives us another data point for further model studies,» says Dr. Martin.
While climate models also simulate the
observed linear relationship between
sea ice area and CO2 emissions, they usually have a much lower sensitivity of the
ice cover than has been
observed.
AWI researchers
observed a considerable decrease in the thickness of the
sea ice as early as the late summer of 2015, even though the overall
ice covered
area of the September minimum ultimately exceeded the record low of 2012 by approximately one million square kilometres.
Complementary analyses of the surface mass balance of Greenland (Tedesco et al, 2011) also show that 2010 was a record year for melt
area extent... Extrapolating these melt rates forward to 2050, «the cumulative loss could raise
sea level by 15 cm by 2050 ″ for a total of 32 cm (adding in 8 cm from glacial
ice caps and 9 cm from thermal expansion)- a number very close to the best estimate of Vermeer & Rahmstorf (2009), derived by linking the
observed rate of
sea level rise to the
observed warming.
The total
area of
sea ice in both hemispheres, by the
ice center's accounting, was «near or slightly lower than»
area observed at a similar time of year in 1979, not equal to it.
If this thinning would have eliminated
ice from
areas observed to have
sea ice, a minimum thickness of 20 cm was left in place for the
ice initial condition.
Ice around Iceland (the number of weeks when ice was observed in this case) must correlate very well with the arctic sea ice extent / area, at least with the annual maxim
Ice around Iceland (the number of weeks when
ice was observed in this case) must correlate very well with the arctic sea ice extent / area, at least with the annual maxim
ice was
observed in this case) must correlate very well with the arctic
sea ice extent / area, at least with the annual maxim
ice extent /
area, at least with the annual maximum.
The scientists have measured average
sea ice thickness to less than a meter in the
area, and
observed a late start of the freeze up period.
For example, although the sample size has been very small, studies of radio - collared seals in the Bering and Chukchi
Seas observed those seals rarely hauled out at all, on land or
sea ice, even when occupying
ice covered
areas.
In 2017, maximum winter
sea ice area, measured each March, was the lowest ever
observed.
If this thinning would have eliminated
ice from
areas observed to have
sea ice, a minimum thickness of 20 cm was left in place.
I suspect ExxonMobil may have been heavily influenced by the drop in the
sea ice summer surface
area observed in 2012.
Since 1950, Arctic
sea ice has lost half its
area and half its thickness, helping to cause the phenomenon of Arctic amplification − the greater temperature rise (approaching 3 °C)
observed in the Arctic than anywhere else on Earth.
Mean
sea level (MSL) evolution has a direct impact on coastal
areas and is a crucial index of climate change since it reflects both the amount of heat added in the ocean and the mass loss due to land
ice melt (e.g. IPCC, 2013; Dieng et al., 2017) Long - term and inter-annual variations of the
sea level are
observed at global and regional scales.
That's the case in Antarctica, which is geographically very different to the Arctic, where an increase in surface
sea ice area, but not total volume, is currently being
observed due to increased precipitation and increased surface water run off.
In late August, just 1.58 million square miles of
sea ice covered the Arctic Ocean, the smallest such
area ever
observed by NASA satellites since the space agency began monitoring the Earth's polar
ice caps 30 years ago.
pdf cited by Will ««
Observed global sea ice area, defined here as a sum of N. Hemisphere and S. Hemisphere sea ice areas, is near or slightly lower than those observed in late 1979
Observed global
sea ice area, defined here as a sum of N. Hemisphere and S. Hemisphere
sea ice areas, is near or slightly lower than those
observed in late 1979
observed in late 1979.»
The
observed effects of cryosphere reduction include modification of river regimes due to enhanced glacial melt, snowmelt advance and enhanced winter base flow; formation of thermokarst terrain and disappearance of surface lakes in thawing permafrost; decrease in potential travel days of vehicles over frozen roads in the Arctic; enhanced potential for glacier hazards and slope instability due to mechanical weakening driven by
ice and permafrost melting; regional ocean freshening;
sea - level rise due to glacier and
ice sheet shrinkage; biotic colonisation and faunal changes in deglaciated terrain; changes in freshwater and marine ecosystems affected by lake -
ice and
sea -
ice reduction; changes in livelihoods; reduced tourism activities related to skiing,
ice climbing and scenic activities in cryospheric
areas affected by degradation; and increased ease of ship transportation in the Arctic.