«The Canadian Ice Service, an arm of Environment Canada, said there is 10 per cent more
ice this year compared to the 30 - year average.
Not exact matches
The
ice bucket challenge has raised more than $ 22 million over the past three weeks,
compared to $ 1.9 million during the same period last
year.
«Those [investments] enable us to make better
ice cream,
compared to the locals that have been making [the same]
ice cream for 20 - some - odd
years,» he says.
They then
compared each
year's loss with that calculated from readings by the GRACE satellite, which «weighs» the
ice sheet by measuring its gravity.
Whereas most studies look to the last 150
years of instrumental data and
compare it to projections for the next few centuries, we looked back 20,000
years using recently collected carbon dioxide, global temperature and sea level data spanning the last
ice age.
The lobe is an oddity
compared with the rest of Pluto's craggy, crater - pocked, multibillion -
year - old surface, covered in bright
ice that is relatively fresh and crater - free.
The researchers determined from the isotope ratio that the Taylor Glacier samples were 120,000
years old, and validated the estimate by
comparing the results to well - dated
ice core measurements of atmospheric methane and oxygen from that same period.
The
ice core data also shows that CO2 and methane levels have been remarkably stable in Antarctica — varying between 300 ppm and 180 ppm — over that entire period and that shifts in levels of these gases took at least 800
years,
compared to the roughly 100
years in which humans have increased atmospheric CO2 levels to their present high.
To piece together this puzzle, Yale University historian Joseph Manning and his colleagues first
compared records of Nile River heights dating back to A.D. 622 with volcanic eruptions recorded in
ice cores from Greenland and Antarctica that date back 2,500
years.
Responses to climate - linked factual questions, such as whether Arctic sea
ice area has declined
compared with 30
years ago, were politicized as if we were asking for climate - change opinions.
The study
compared weather patterns during low sea
ice conditions as seen in recent
years to weather patterns during high sea
ice conditions typical of the late 1970s.
NSIDC will issue a formal announcement at the beginning of October with full analysis of the possible causes behind this
year's
ice conditions, particularly interesting aspects of the melt season, the set up going into the winter growth season ahead, and graphics
comparing this
year to the long - term record.
A composite image shows how the extent of Arctic sea
ice in September 2016
compared with a 30 -
year average for the month (yellow line).
Satellites show the extent of Arctic sea
ice on Sept. 16, 2012 as
compared to the average minimum from the past 30
years (yellow line).
Ocean levels rose 50 percent faster in 2014 than in 1993, with meltwater from the Greenland
ice sheet now supplying 25 percent of total sea level increase
compared with just five percent 20
years earlier, researchers reported...
We know that the magnitude of
year - to -
year variability of sea
ice in Antarctica is very high
compared to the long term trend [Fig 1].
After the September low,
ice began to build up again in the Arctic; rapidly at first,
compared to other
years, then slowing during October and November as the region experienced a spell of exceptionally high temperatures.
The dataset revealed that Antarctica gained 272 billion tons more
ice per
year in the first decade of the 21st century
compared with the first decade of the 19th.
Ice core paleoclimate isotope data are indirect indications of temperature (proxies) over millions of
years compared to instrumental temperature measurements with high resolution of hours, days and decades.
That's tiny
compared with the several millimeters a
year of sea level rise coming from Antarctica's melting
ice each
year, but it ain't nothing.
That's actually a small number
compared with Antarctica's total annual
ice flow — about 2,000 billion tons a
year — most of which is replenished by precipitation.
you want to get passed every now and again just so that you can come back and have a good old tussle with your rivals.i did enjoy this and you guys are right this is the best motorbike sim out there for consoles atm but still far from perfect on the graphics level which is a shame because backgrounds here are dull and seem like last century
compare to other awarding winning sports titles like 2k NBA 11 or the brilliant EA Nhl
ice hockey games.It is pure speed and control here though so you will be concentrating on the road more then the back drops.anyways im out of here but nice work blackbean hopefully step it up another notch in the graphics department next
year yeh!
Compared to other exhibitions over the last few
years; Pompei and Herculaneum,
Ice Age Art, The Vikings - this exhibition fell short of the usual gold standard that The British Museum does so well.
If you understand the links above, volume is wholesale a lot less
compared to 1996, along with open water, with very little multi
year ice in the archipelago.
But a Upper air profile from a land station may differ low over sea
ice, for the lower atmosphere may be warmer over thinner
ice compared with previous
years.
Check out the difference in extent of most mountain glaciers
compared to 30
years ago, or the extent of sea
ice in the arctic ocmpared to a few decades ago.There are many manifestations all around us.
One of the lessons drawn from
comparing Greenland to Antarctica and many other places is that some of the temperature changes (the
ice - age cycling) are very widespread and shared among most records, but other of the temperature changes (sometimes called millennial, or abrupt, or Younger - Dryas - type) are antiphased between Greenland and the south, and still other temperature changes may be unrelated between different places (one anomalously cold
year in Greenland does not tell you the temperature anomaly in Australia or Peru).
The most exciting thing is we'll get a chance to see the relative strength of all of these over the next few
years, and it will most interesting to
compare the total decade of 2010 - 2019 to previous decades in terms of the trends in Arctic Sea
ice, Global Temps, and of course, OHC.
The key issue is that since last
year's dramatic summer
ice anomaly, the winter
ice that formed in that newly opened water is relatively thin (around 1 meter),
compared to multi-
year ice (3 meters or so).
And that demonstrates how dangerous it potentially is for us to do something that's never happened in the history of the planet... to very dramatically change the CO2 concentration, in a matter of mere decades as
compared to the usual centuries or millenia involved in an
ice age feedback scenario, through a mechanism never found in nature — uncovering plant matter that's been buried for hundreds of millions of
years, and burning it for energy.
The article in The Independent makes its predictions based on the increased speed of reduction of the Sea
Ice Area
compared to last
year.
In early September, I noted that this
year's sea
ice track was «decent»
compared to 2012.
There'll be another round of «Sea
Ice Outlook» this year, aimed at comparing predictions of ice behavior by different groups using different methods as a way to build understandi
Ice Outlook» this
year, aimed at
comparing predictions of
ice behavior by different groups using different methods as a way to build understandi
ice behavior by different groups using different methods as a way to build understanding.
So that, while the surface area may be greater this
year compared with last
year, the volume of
ice in the Arctic this
year is probably already less than at the same time last
year.
You can
compare the current
ice conditions with predictions made earlier in the year through the Sea Ice Outlook effort, a project of the Arctic Research Consorti
ice conditions with predictions made earlier in the
year through the Sea
Ice Outlook effort, a project of the Arctic Research Consorti
Ice Outlook effort, a project of the Arctic Research Consortium.
Technology for «seeing» into the oceans, finding fish stocks, tracking them, catching them and hauling them, and preserving them with
ice has increased astronomically
compared to the Fishing Methods that were in use just fifty or sixty
years ago.
The graph below (high - resolution copy) shows the range of the forecasts for early September, the point when the sea
ice typically reaches its minimum extent,
compared to recent
years and the average over the period of precise satellite measurement.
Scientists now know there was a substantial jump in
ice loss from 2002 through 2004
compared to previous
years.»
If you look at our climate, and
compare it to a machine that has a vibration problem, you hear the vibration build up and then die away, build up and die away — the big build up and die away is the hundreds of millions of
years climate shift, and the individual vibrations that make up the fine grain are the 100k
year switches between
ice age and warm spell.
Any curve that represents the sea
ice extent this
year can not be
compared to last
year's curve — it would be
comparing apples to oranges.
We've preserved a fair amount of first -
year ice and second -
year ice after this summer
compared to the past couple of
years.
Figure 1 shows the concentration of multi-
year ice (MYI) in the western channel of the Northwest Passage at the end of May this
year and for the past four
years compared to the 1981 - 2010 climatology.
This increase was based on the June
ice extent remaining within 1 sigma of the 1981 - 2010 long - term mean and nearly average melt pond coverage
compared to recent
years.
The little
ice age came and went, visibly but insignificant
compared to the scale of the warming we've seen in the last 140
years.
Compared to spring 2011, the old
ice in the Beaufort Sea in May 2012 appears to be somewhat more consolidated and older overall (which typically implies thicker
ice), with more
ice of three
years of age or greater and less first -
year ice mixed in.
Although that's really all that needs be said, I should add that jetfuel is trying to
compare cumulative
year - over-
year land
ice mass loss in Antarctica with (cyclical) seasonal river / lake
ice volume gain in Canada - and ignoring the inevitable melt - away of the latter.
In any case, any changes in average volume over the course of the
year have been minimal
compared to the Antarctic
ice loss.
Research indicates that the Arctic had substantially less sea
ice during this period
compared to present Current desert regions of Central Asia were extensively forested due to higher rainfall, and the warm temperate forest belts in China and Japan were extended northwards West African sediments additionally record the «African Humid Period», an interval between 16,000 and 6,000
years ago when Africa was much wetter due to a strengthening of the African monsoon While there do not appear to have been significant temperature changes at most low latitude sites, other climate changes have been reported.
Compared to the last ten
years of climatology, the sea
ice probability (SIP) values from Blanchard - Wrigglesworth et al (Figure 4) tend to be higher in the Beaufort Sea, and slightly lower in the Laptev Sea.
The twenty
year cumulative 1620 GT loss of Antarctic Land
Ice, when
compared to the 26450000 GT on Antarctica is.00006 or.000003 per
year on avg.