What is also stunning are sea - ice daily extent figures
averaging ice loss of more than 100,000 square kilometres per day for the last four days.
Satellite images — comparing
average ice loss from 2003 to 2007 with the 2003 - 2009 average — show rapid loss around the perimeter of the ice sheet, reflecting the melting of outlet glaciers.10
Not exact matches
The work by Mark Jacobson, director of Stanford University's Atmosphere / Energy program and a fellow at the university's Woods Institute, argues that cutting emissions of black carbon may be the fastest method to limit the ongoing
loss of
ice in the Arctic, which is warming twice as fast as the global
average.
These two competing effects cancel each other out, meaning little change in the
average temperature of European winters as a consequence of sea -
ice loss».
On
average West Antarctica lost 134 gigatonnes of
ice, East Antarctica three gigatonnes, and the Antarctic Peninsula 23 gigatonnes in each year between 2010 and 2013 — a total
loss of 159 gigatonnes each year.
Ice loss from Greenland and Antarctica and their peripheral ice caps and glaciers averaged 385 billion tons (100 cubic miles) a ye
Ice loss from Greenland and Antarctica and their peripheral
ice caps and glaciers averaged 385 billion tons (100 cubic miles) a ye
ice caps and glaciers
averaged 385 billion tons (100 cubic miles) a year.
The team also compared the
ice loss up until the mid-1980s to that observed by satellites over roughly the last decade and found that today the rate of
ice loss is twice the 20th century
average, mostly because of increased water runoff from the
ice sheet's surface.
About a quarter of the
average annual
ice loss came from glaciers and
ice caps outside of Greenland and Antarctica (roughly 148 billion tons, or 39 cubic miles).
The bottom line though is permanent
ice melting or
ice loss generally requires yearly
averaged temperatures above 0C.
The comet appears to have undergone visible changes, including the changes in the size and number of surface features such as smooth patches, pits, and craters, and the
loss of
ice vaporized by the Sun or blasted off its surface by the Solar Wind into its tail as well as failing back on the object like snow, so that it appears to shrink, on
average, by 25 to 50 centimeters (9.2 to 19.7 inches) with each orbit around the Sun.
You wrote «The bottom line though is permanent
ice melting or
ice loss generally requires yearly
averaged temperatures above 0C.
So unless the perimeter of the Greenland
ice sheet is the exact same thickness as the entire
ice sheet (say 3 km on
average), an area
loss there, of 15 %, will produce a much smaller % volume
loss, than say if this area
loss were smack dab in the middle of the Greenland
ice sheet.
For Greenland to lose 285,000 km ³ of
ice in 89 years, the
AVERAGE rate of
loss would have to be more than 3,200 km ³ / yr, or nearly 12 times faster than the current
loss rate (273 km ³ / yr).
Average winter sea
ice volume over the period, weighted by a
loss of ∼ 3000 km3 between 2007 and 2008, was ∼ 14,000 km3.
In any case, any changes in
average volume over the course of the year have been minimal compared to the Antarctic
ice loss.
However, despite near normal rates of
ice loss during the month, June 2015 was a relatively warm month (Figure 7) with 925 hPa air temperatures up to 2.5 C higher than
average near the North Pole and East Siberian Sea, with even warmer air temperatures in the Kara Sea (up to 4.5 C).
«For example... the
average personal CO2 emissions of several metric tons per year can be directly linked to the
loss of tens of [square meters] of Arctic sea
ice every single year.»
Since 2008,
ice loss from West Antarctica's unstable glaciers doubled from an
average annual
loss of 121 billion tons of
ice to twice that by 2014, the researchers found.
; North Pole Cam 1 & 2; Arctic Sea
Ice Extent Averaging Below 2007 Anomaly; Paleoclimate Implications for Human - Made Climate Change; UN Security Council Addresses Considers Global Security and Climate Change; New study details glacier ice loss following ice shelf collapse; Climate Change To Spawn More Wildfires; Gingrich Says 2006 Climate Change Ad He Starred In Was «Misconstrued&raq
Ice Extent
Averaging Below 2007 Anomaly; Paleoclimate Implications for Human - Made Climate Change; UN Security Council Addresses Considers Global Security and Climate Change; New study details glacier
ice loss following ice shelf collapse; Climate Change To Spawn More Wildfires; Gingrich Says 2006 Climate Change Ad He Starred In Was «Misconstrued&raq
ice loss following
ice shelf collapse; Climate Change To Spawn More Wildfires; Gingrich Says 2006 Climate Change Ad He Starred In Was «Misconstrued&raq
ice shelf collapse; Climate Change To Spawn More Wildfires; Gingrich Says 2006 Climate Change Ad He Starred In Was «Misconstrued»
Millions of square kilometers sea
ice extent Month — last 5 years — baseline End July — 8.73 — 10.10 End Aug — 6.04 — 7.67 End Sep — 5.02 — 7.04
Average — 6.60 — 8.27 Difference 1.67 million square kilometers (msk) Cumulated
loss = 20 %
The resulting enhanced
loss of summer and winter sea
ice resulted in feedbacks, associated with Arctic Amplification, which has raised Arctic air temperatures at a rate twice the global
average.
As reported in Remote Sensing of Environment, from 1953 to 2010, the
average rate of
ice surface
loss was 18 centimeters (7.1 inches) per year.
It is arguably one of the most advanced of the seven in its impacts, with a 2011 GRL report putting its warming effect as equivalent to around 30 % of atmospheric anthro - CO2, and the recent report putting albedo
loss from arctic sea -
ice decline since»79 as providing a forcing equivalent on
average to that from 25 % of the anthro - CO2 levels during the period.
Results show that the globally and annually
averaged radiative forcing caused by the observed
loss of sea
ice in the Arctic between 1979 and 2007 is approximately 0.1 W m − 2; a complete removal of Arctic sea
ice results in a forcing of about 0.7 W m − 2, while a more realistic
ice - free - summer scenario (no
ice for one month, decreased
ice at all other times of the year) results in a forcing of about 0.3 W m − 2, similar to present - day anthropogenic forcing caused by halocarbons.
This is a decrease from the
average rate of
ice loss for June 2010 of -85,210 square kilometers per day, and is slower than climatology (
average of -84,050 square kilometers per day for 1979 - 2000).
Furthermore, the Arctic has warmed more than twice as fast as the global
average, a phenomenon known as Arctic amplification, and stimulated by the combined increasing Arctic temperatures and rapid
loss of sea
ice in all seasons along with declining snow cover in the spring and early summer.
From July 1 - July 20, the rate of
ice loss averaged -79,810 square kilometers per day.
After above -
average air temperatures and record
ice loss in May 2010, the
ice extent at the beginning of June fell below the previous record minimum for the same day in 2006.
The sea
ice loss is not 100 % but if it's 1/3 that's still 3 Wm2
averaged over the Earth.
The drastic melt of 2007 remains the record
loss of
ice area in the satellite era, although subsequent years have still been below the long - term
average.
The ongoing
loss of
ice in a region that is on
average not wamer in the latter part of 60 years (1941 - 2000) seems like a good reminder that it does not take a constant yeaer on year increase to cause pronounced natural response over large areas.
In stark contrast to the relatively slow
ice loss during June, July saw quite rapid
ice loss (Figure 6), with rates
averaging over 100,000 km2 per day through the month.
Air temps in arctic are almost precisely the same as the
average for the past 50 years — So it is unlikely air temps have created
ice loss — BUT CONVERSELY — the increased open arctic water SHOULD be affecting the arctic air temp - but is not (large expanses of 1 degree C arctic water make it difficult for air temps to drop to minus ten C — but since that is what is happening, then in fact there must be much more cold air around to create «normal» arctic temps for this time of the year)
This calculation is then correlated with the reported 5 day
average NSIDC
ice extent
loss.
Starting with the April Pan-Arctic
Ice Ocean Modeling and Assimilation System (PIOMAS) volume distribution and the April National Snow and Ice Data Center (NSIDC) average ice extent the estimated extent loss for each 10 cm thickness of ice loss is calculat
Ice Ocean Modeling and Assimilation System (PIOMAS) volume distribution and the April National Snow and
Ice Data Center (NSIDC) average ice extent the estimated extent loss for each 10 cm thickness of ice loss is calculat
Ice Data Center (NSIDC)
average ice extent the estimated extent loss for each 10 cm thickness of ice loss is calculat
ice extent the estimated extent
loss for each 10 cm thickness of
ice loss is calculat
ice loss is calculated.
The MDB
average rainfall during the last three decades has been recording a 10 %
loss per decade, I believe this is primarily due to declining solar radiation levels, moving from the highest for 8000 years to presently the lowest for 100 years, this solar decline is expected to continue for at least another 3 decades, maybe 6 decades like it did in the 16th century, brining on the last little
ice age.
Self, if the
average they are using only relates to a warming trend is anything other than
ice loss logical?
Likewise, the effects on
average global temperature and climate of rapidly diminishing albedo evidenced by
loss of Arctic sea
ice and retreating glaciers, is not accurately known.
And the decline has accelerated, becoming far more dramatic, since about the year 2000, leading to annual
average sea
ice loss of around three million square kilometers.
Meanwhile in 2012, we've seen record Arctic
ice loss, and the U.S. has faced two record heat waves, a record drought, an above -
average fire season, and now, an «unprecedented» hurricane.
Fluctuations in the mass of the Greenland and Antarctic
ice sheets are of considerable societal importance as they impact directly on global sea levels: since 1901,
ice losses from Antarctica and Greenland, alongside the melting of small glaciers and
ice caps and thermal expansion of the oceans, have caused global sea levels to rise at an
average rate of 1.7 mm / yr.
Science: satellite data showing Arctic sea
ice between 1979 and The white area shows a moving
average of Arctic sea
ice between 2003 and The darker blue surrounding the white area is the moving
average for the sea
ice between 1979 and Between 1979 and 2005,
average Arctic sea
ice dropped 20 % — a
loss in area about the size of the U.S. state of Texas.
Rennie (Public), 3.20 (2.50 - 3.80), Heuristic Starting with the April PIOMAS volume distribution and the April NSIDC
average ice extent the estimated extent
loss for each 10 cm thickness of
ice loss is calculated.
Current models suggest
ice mass
losses increase with temperature more rapidly than gains due to increased precipitation and that the surface mass balance becomes negative (net
ice loss) at a global
average warming (relative to pre-industrial values) in excess of 1.9 to 4.6 °C.
Thirteen years of GRACE data provide an excellent picture of the current mass changes of Greenland and Antarctica, with mass
loss in the GRACE period 2002 - 15 amounting to 265 ± 25 GT / yr for Greenland (including peripheral
ice caps), and 95 ± 50 GT / year for Antarctica, corresponding to 0.72 mm / year and 0.26 mm / year
average global sea level change.
The rate of
ice loss during July 2016 was slightly below
average at 83,800 square kilometers (32,400 square miles) per day.
In
ice -
loss years, they found an
average of 38 early - summer storms, while
ice - gain years had an
average of 48.
The Concordia Dome
ice core turns out to
average about 0.43 cm of
ice per year, so the
loss of resolution of atmospheric CO2 by diffusion
averaging is about twice the rate of Vostok.
When you put 2012's record high temperatures with other signs like the record amount of extreme weather and this year's record
loss of Arctic sea
ice, or the fact that if you're under age 27, you've never experienced a month that was colder than
average, it's hard to ignore the looming threat of climate change.
However, Greenland's annual
average temperature has risen steadily since 1995, and snowfall has not compensated for the increase in summer
ice loss.