This year, we attempted to account for a lower rate of first -
year ice loss near the pole, but our outlook was still significantly lower than the actual minimum.
Not exact matches
The team found that, for the last 20
years, the glacier and
ice cap mass
loss has been exactly equal to the amount of meltwater runoff lost to the sea.
The Maggie Beer Products operations make a range of
ice - creams, pate, quince pastes, and sauces and also suffered a painful slide into the red in the previous full financial
year, posting an annual
loss of $ 2.13 million for the 12 months ended June 30, 2017.
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.
Michiel van den Broeke of Utrecht University in the Netherlands and colleagues began by modelling the difference in annual snowfall and snowmelt in Greenland between 2003 and 2008 to reveal the net
ice loss for each
year.
The
ice loss found in northeast Greenland is accelerating, and it is uncertain how many
years it will continue, he said.
For
years, floating
ice in the bay abutting the
ice sheet in the northeast acted as a barrier to
ice loss.
Within a few
years, the main outlet glacier draining the region — Zachariae Isstrom — retreated about 20 kilometers, and regional
ice mass
loss jumped from zero to roughly 10 metric gigatons a
year.
They describe the West Antarctic
Ice Sheet (WAIS) as having experienced significant and sustained ice loss until 7,500 years ago, driven by warm water incursio
Ice Sheet (WAIS) as having experienced significant and sustained
ice loss until 7,500 years ago, driven by warm water incursio
ice loss until 7,500
years ago, driven by warm water incursions.
Ice loss from northeast Greenland into the Fram Strait abutting the Arctic Ocean is now closer to 15 to 20 metric gigatons a
year and is still increasing, said Khan.
This
year's Arctic sea
ice cover currently is the sixth - lowest on modern record, a ranking that raises ongoing concerns about the speed of
ice melt and the effects of
ice loss on global weather patterns, geopolitical fights, indigenous peoples and wildlife, scientists said yesterday.
That corresponds to a roughly 3 1/2 week shift at either end — and seven weeks of total
loss of good sea
ice habitat for polar bears — over the 35
years of Arctic sea
ice data.
«The
loss of sea
ice in the Arctic and changes to heat storage will lead to changes in weather patterns that could bring extreme heat and cold events to the continental United States similar to those seen in recent
years, and possibly even more intense.»
From 1994 to 2003, the overall
loss of
ice shelf volume across the continent was negligible: about 25 cubic kilometers per
year (plus or minus 64).
Pine Island Glacier and the neighbouring Thwaites Glacier are responsible for nearly a third of total
ice loss from the West Antarctic Ice Sheet, and this contribution has increased greatly over the past 25 yea
ice loss from the West Antarctic
Ice Sheet, and this contribution has increased greatly over the past 25 yea
Ice Sheet, and this contribution has increased greatly over the past 25
years.
Velicogna and her colleagues also measured a dramatic
loss of Greenland
ice, as much as 38 cubic miles per
year between 2002 and 2005 — even more troubling, given that an influx of fresh melt water into the salty North Atlantic could in theory shut off the system of ocean currents that keep Europe relatively warm.
In comparison, global sea levels are rising by about 3 millimetres a
year, and a recent study estimated that one - third of that comes from
ice loss in Antarctica and Greenland.
They then used the satellite record of Arctic sea
ice extent to calculate the rates of sea
ice loss and then projected those rates into the future, to estimate how much more the sea
ice cover may shrink in approximately three polar bear generations, or 35
years.
WITH all the attention given to the
loss of sea
ice in the Arctic, it's easy to forget that some
ice will persist for many
years yet.
The next step is to use estimates of future sea
ice loss to make predictions of how further melting could influence summer rainfall in Europe in the
years to come.
In 2008 a satellite study based on rates of snowfall and
ice movement estimated a
loss of 210 cubic kilometers of
ice per
year — a 59 percent increase in the past decade.
Overall, the amount of melting wasn't a blockbuster — 2012 was a more impressive
year for
ice loss.
«Warming greater than 2 degrees Celsius above 19th - century levels is projected to be disruptive, reducing global agricultural productivity, causing widespread
loss of biodiversity and — if sustained over centuries — melting much of the Greenland
ice sheet with ensuing rise in sea levels of several meters,» the AGU declares in its first statement in four
years on «Human Impacts on Climate.»
Those same lakes, along with other evidence from around the world, also points to the shifting of rain belts after a rapid
loss of Arctic sea
ice about 14,600
years ago that saw the Northern Hemisphere heat up faster than the Southern.
For short periods, it peaked at
ice loss rates of over 3000 cubic kilometres per
year.»
The study concluded that there was a net
loss of
ice between 2002 and 2005, adding 0.4 millimetres per
year to sea levels (see Gravity reveals shrinking Antarctic
ice).
Located between Greenland and Russia, Svalbard experienced a near - complete
loss of its vegetation during the last
ice age and was quite sparse even 10,000
years ago, but today it is home to a thriving plant community.
«It's kind of remarkable that it's as low as it is [this
year], given that the weather conditions were not terribly optimal for
ice loss,» Meier said.
Thousands of black - and - white aerial photographs of Greenland taken between 1978 and 1987 are helping scientists reconstruct a 110 -
year - long record of
ice loss in this region.
«We're talking about the potential for centimetres per
year just from [
ice loss in] Antarctica.»
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.
Over the last few
years, research has increasingly suggested that
ice loss in this region is heavily driven by the influence of the warming ocean.
Lead author Dr Malcolm McMillan from the University of Leeds said: «We find that
ice losses continue to be most pronounced along the fast - flowing
ice streams of the Amundsen Sea sector, with thinning rates of between 4 and 8 metres per
year near to the grounding lines of the Pine Island, Thwaites and Smith Glaciers.»
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.
Increased melting of the Greenland
Ice Sheet and other ice losses worldwide have helped to move the North Pole several centimeters east each year since 2
Ice Sheet and other
ice losses worldwide have helped to move the North Pole several centimeters east each year since 2
ice losses worldwide have helped to move the North Pole several centimeters east each
year since 2005
The findings, published yesterday in the journal Nature, show that during the past 11,000
years, wind patterns have driven relatively warm waters from the deep ocean onto Antarctica's continental shelf, leading to significant and sustained
ice loss.
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 reconstructed curve includes isolated rapid events of several decimetres within a few centuries, one of which is most likely related to
loss from the Antarctic
ice sheet mass around 5000
years before present.
Almost half of this came from
ice loss in the Arctic and, of course, more is expected in the coming
years.
The global mean temperature rise of less than 1 degree C in the past century does not seem like much, but it is associated with a winter temperature rise of 3 to 4 degrees C over most of the Arctic in the past 20
years, unprecedented
loss of
ice from all the tropical glaciers, a decrease of 15 to 20 % in late summer sea
ice extent, rising sealevel, and a host of other measured signs of anomalous and rapid climate change.
This
year has seen extensive
losses from Antarctica's
ice shelves.
What they argue is that if the 450ppm is sustained over geologic timescales ie > 1000 - 10000
years then it will lead to the
loss of all
ice.
According to Christner, agricultural
losses from
ice nucleating bacteria, such as Pseudomonas syringae, often exceed $ 1 billion dollars per
year in the United States, so understanding their mode of dispersal is essential for mitigating their impact on crops.
«This is the sixth earliest onset of
ice loss in our 27 -
year record, although there isn't really a large difference from one
year to the next in the top - ranking 17
years,» said climate scientist Peter Langen.
One
year without a net
loss also doesn't buck the long - term trend of Greenland losing
ice, both from surface melt and from ocean waters eating away at glaciers that flow out to sea.
The present - day
ice loss from the Antarctic Peninsula is -41.5 giga - tonnes per
year [16].
And since you have missed this acceleration you have assumed that the rate will remain at 3.3 mm /
year for the rest of this century, despite ongoing observations of increases in
ice mass
loss in Greenland and parts of Antarctica.
The estimated 2010 or 2011 surface mass imbalance (~ 300 Gt / yr) is comparable to the GRACE estimates of the total mass
loss (which includes
ice loss via dynamic effects such as the speeding up of outlet glaciers) of 248 ± 43 Gt / yr for the
years 2005 - 2009 Chen et al, 2011.
I remember only a few
years ago people were talking about end of the century or later for
ice loss — and as events unfold we seem to be rapidly reeling this estimate in closer — prudence would lead me to assume it best to take a pessimistic view in case we continue to shorten our estimates.