However, I want to call your attention to the underlying structure of
the the ice area data.
[3] An implementation of the diff - of - gaussian filter is presented here: https://climategrog.wordpress.com/2016/09/18/diff-of-gaussian-filter/ [4] The sea -
ice area data used in the decadal trend analysis are provided by Cryosphere Today team at U. Illinois.
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.
Overland recently co-authored a study predicting an
ice - free Arctic summer in the first half of this century and said he will soon be releasing additional
data projecting that an
area 100 miles north of Alaska will witness open water five months out of the year by 2030, as opposed to the current two months.
Their field - based
data also suggest that during major climate cool - downs in the past several million years, the
ice sheet expanded into previously
ice - free
areas, «showing that the
ice sheet in East Greenland responds to and tracks global climate change,» Bierman says.
These
data were used to quantify changes in the
ice cover's composition, revealing a substantial reduction of about 14 percent in the
area of multiyear
ice in winter during the period from 1978 to 1998.
«We analysed the satellite
data to determine how far the
ice in that particular
area has travelled,» says AWI biologist and co-author of the study, Hauke Flores.
An image of an
area of the Arctic sea
ice pack well north of Alaska, captured by the MODIS instrument on NASA's Aqua satellite on Sept. 13, 2013, the day before the National Snow and Ice Data Center estimated Arctic sea ice to have reached its minimum extent for the ye
ice pack well north of Alaska, captured by the MODIS instrument on NASA's Aqua satellite on Sept. 13, 2013, the day before the National Snow and
Ice Data Center estimated Arctic sea ice to have reached its minimum extent for the ye
Ice Data Center estimated Arctic sea
ice to have reached its minimum extent for the ye
ice to have reached its minimum extent for the year.
Data suggest that although the
ice - rich rings have only 15 % of Chariklo's surface
area, they reflect almost three times as much light on an
area - to -
area comparison.
The trends revealed by the
data were clear: The average albedo in the northern
area of the Arctic Ocean, including open water and sea
ice, is declining in all summer months (May - August).
Satellite
data show that the annual minimum for Arctic sea
ice area fell 7 percent per decade between 1980 and 2000 — but since 2000 it has fallen 14 percent per decade.
The problem with those measurements, Morlighem said, is that they were scattered, and the
data were limited to
areas where there were flights over the
ice sheet.
Previous research estimated that it covered much of western Canada as late as 12,500 years ago, but new
data shows that large
areas in the region were
ice - free as early as 1,500 years earlier.
New
data indicate that substantial
areas throughout westernmost Canada were
ice free prior to 12.5 ka and some as early as 14.0 ka, with implications for climate dynamics and the timing of meltwater discharge to the Pacific and Arctic oceans.
The extent of global sea
ice coverage reached its smallest
area ever recorded in 2016, new
data show.
For example, few
data are available for the polar winter, and it is not known whether aragonite - undersaturated
areas decrease in size with the seasonal freezing of sea
ice.
Conservative tracer studies using stable oxygen isotopic
data from 307 sites show that while the entire surface of this
area receives abundant freshwater from meteoric sources, freshwater from sea
ice melt is most closely linked to the
areas of carbonate mineral undersaturation.
In addition to gaining an intimate understanding of life formerly under the
ice, the
data will serve as a baseline to see how the
area changes as sunlight and open water alters the chemistry and new species migrate in.
The
data presented here indicate that the
area of undersaturation presently extends to approximately 20 % of the Canadian Basin in the late summer months, when sea
ice is near its minimum extent.
These
data link the Arctic Ocean's largest
area of aragonite undersaturation to sea
ice melt and atmospheric CO2 absorption in
areas of low buffering capacity.
Although you really can't check this assertion since the
data is not really available anywhere — the Cryosphere has some charts of sea
ice area but where are the numbers — where are the sea
ice extent numbers.
What makes the
ice - out
data a good metric is that it arguably has less bias with respect to urban
areas that temperature stations.
I know many people are touting the PIOMAS
data, but the sea
ice minimum
area is still more than half what it was 30 years ago.
Instead, a rather casual article in the Independent showed the latest thickness
data and that quoted Mark Serreze as saying that the
area around the North Pole had 50/50 odds of being completely
ice free this summer, has taken off across the media.
``... sea
ice concentration (SIC)
data * of AMSR - E standard products are used for
area calculation.
Remote sensing
data shows that the
area covered by
ice lakes within the Qomolangma National Nature Reserve in Tibet increased to 114 square kilometres in 2013, up from 100 square kilometres in 1990.
In May 2007, a team of scientists from NASA and the University of Colorado reported satellite
data showing widespread snow - melt on the interior of the Antarctic
ice sheet over an
area the size of California.
Is anyone collecting real time
data in the
area where the
ice cores were taken?
We need further field
data from key
areas of East Antarctica to reject some of the
ice model scenarios — although there are fewer rock outcrops to sample geologically and geodetically in this region there are still large regions where outcrops exist but no, or few,
data have been collected and / or results have been published.
The next year, Rignot and Mouginot published another comprehensive, high - resolution map of Greenland based in radar interferometry
data from 2008 and 2009 showing that Greenland's 100 fastest glaciers drain 66 percent of the
ice sheet
area, and marine - terminating glaciers drain 88 percent of the
ice sheet
area (Rignot and Mouginot 2012).
The European Space Agency's CryoSat - 2 mission has enhanced Antarctic
ice sheet monitoring by including
areas closer to the poles than earlier satellites, and by acquiring better
data in moderately sloping
areas, including
ice sheet margins where most of the
ice loss occurs.
It's easy to get daily up - to - date
data on arctic
ice extent from JAXA, and on arctic
ice area from cryosphere today.
The plan was to make ground observations that could link to the satellite
data showing unexpectedly pronounced
ice loss from the
area.
As reported on Cryosphere Today based on NSIDC
data, sea
ice area today is 2.92 million square kilometres.
Historically, NSIDC scientists have handled the
data gap over the North Pole by assuming it was
ice - filled, and adding that
area to the extent observed outside the
data gap.
The product covers the sea and
ice areas polewards of latitudes 50N and 50S with 3 - minute
data segments in Level 2, with
data processed and archived continuously throughout the day, as they become available (approximately 110 3 - minute segments per day per hemisphere).
Can you provide
data about
ice volume versus
area?
Canada said that in the Arctic it faced the challenge of collecting
data in
areas that are
ice - covered, difficult to access and that, in some instances, had not previously been surveyed.
The Canadian Hydrographic Service and the Geological Survey of Canada have collected a great deal of
data in
areas that are
ice - covered, difficult to access, and that in some instances had not previously been surveyed.
They applied a new method that fills in missing temperatures over sea
ice by combining satellite
data for missing
areas with a method known as «kriging,» which calculates missing
data by checking nearby temperature station readings.
To my readers, Anthony Watts received a comment from our friend Tamino on the
ice data I used for the
area analysis.
The difference is due to University of Bremen's analysis of
data from the newer AMSR - E sensor, which has a higher resolution and shows
areas of open water that are classified as
ice - covered by the lower - resolution sensor that NSIDC relies on.
Werner's observation follows the announcement in September by the National Snow and
Ice Data Center that the surface area of Arctic sea ice had reached a new low in 2012, breaking a previous record reached in 20
Ice Data Center that the surface
area of Arctic sea
ice had reached a new low in 2012, breaking a previous record reached in 20
ice had reached a new low in 2012, breaking a previous record reached in 2007.
Arctic «sea
ice extent has varied naturally over the decades with some Russian
data suggesting similar or even greater
ice loss in some local
areas in the 1930s» — Analysis of Arctic
ice: «Russian
data shows that the [Arctic]
ice was just as thin in 1940 as it is now.
In September 2008, the sea
ice area minimum was less than 5 % larger than the September 2007 sea
ice area minimum as derived from AMSR - E 89 GHz
data.
The
area of Arctic sea
ice was nearly 30 % greater in August than a year ago, according to recent satellite
data, though projections based on longer - term trends suggest the sea
ice will continue its decline over time.
All of these characteristics (except for the ocean temperature) have been used in SAR and TAR IPCC (Houghton et al. 1996; 2001) reports for model -
data inter-comparison: we considered as tolerable the following intervals for the annual means of the following climate characteristics which encompass corresponding empirical estimates: global SAT 13.1 — 14.1 °C (Jones et al. 1999);
area of sea
ice in the Northern Hemisphere 6 — 14 mil km2 and in the Southern Hemisphere 6 — 18 mil km2 (Cavalieri et al. 2003); total precipitation rate 2.45 — 3.05 mm / day (Legates 1995); maximum Atlantic northward heat transport 0.5 — 1.5 PW (Ganachaud and Wunsch 2003); maximum of North Atlantic meridional overturning stream function 15 — 25 Sv (Talley et al. 2003), volume averaged ocean temperature 3 — 5 °C (Levitus 1982).
The
area of the Arctic Ocean covered by some sea
ice was at a record low for the month of October, according to data from the National Snow and Ice Data Center (NSID
ice was at a record low for the month of October, according to
data from the National Snow and Ice Data Center (NSI
data from the National Snow and
Ice Data Center (NSID
Ice Data Center (NSI
Data Center (NSIDC).
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.
Monthly anomalies of Southern Hemisphere sea
ice extent (left panel) and
area (right panel) derived using the newly enhanced SB2
data (black) of Comiso et al. and the older SBA
data (red) prior to the enhancements made by Comiso et al..