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Showing posts with label CryoSat. Show all posts
Showing posts with label CryoSat. Show all posts

Friday, August 31, 2012

Fen Montaigne: Arctic Tipping Point: A North Pole Without Ice


Arctic Tipping Point:
A North Pole Without Ice

Scientists say this year’s record declines in Arctic sea ice extent and volume are powerful evidence that the giant cap of ice at the top of the planet is on a trajectory to largely disappear in summer within a decade or two, with profound global consequences.


by fen montaigne, yale360, August 30, 2012


As the northern summer draws to a close, two milestones have been reached in the Arctic Ocean — record-low sea ice extent, and an even more dramatic new low in Arctic sea ice volume. This extreme melting offers dramatic evidence, many scientists say, that the region’s sea ice has passed a tipping point and that sometime in the next decade or two the North Pole will be largely ice-free in summer.

NASA and U.S. ice experts announced earlier this week that the extent of Arctic sea ice has dropped to 4.1 million square kilometers (1.58 million square miles) — breaking the previous record set in 2007 — and will likely continue to fall even farther until mid-September. As the summer melt season ends, the Arctic Ocean will be covered with 45 percent less ice than the average from 1979 to 2000.

NASA
On August 26, 2012, Arctic sea ice reached a new record-low summer extent.
Even more striking is the precipitous decline in the volume of ice in the Arctic Ocean. An analysis conducted by the University of Washington’s Pan Arctic Ice Ocean Model Assimilation System (PIOMAS) estimates that sea ice volumes fell in late August to roughly 3,500 cubic kilometers — a 72-percent drop from the 1979-2010 mean.

Peter Wadhams, who heads the Polar Ocean Physics Group at the University of Cambridge and who has been measuring Arctic Ocean ice thickness from British Navy submarines, says that earlier calculations about Arctic sea ice loss have grossly underestimated how rapidly the ice is disappearing. He believes that the Arctic is likely to become ice-free before 2020 and possibly as early as 2015 or 2016 — decades ahead of projections made just a few years ago.

Mark Drinkwater, mission scientist for the European Space Agency’s CryoSat satellite and the agency’s senior advisor on polar regions, said he and his colleagues have been taken aback by the swiftness of Arctic sea ice retreat in the last 5 years. “If this rate of melting [in 2012] is sustained in 2013, we are staring down the barrel and looking at a summer Arctic which is potentially free of sea ice within this decade,” Drinkwater said in an e-mail interview.

A small number of climate scientists say that natural variability may be playing a significant role in the rapid retreat of Arctic sea ice, intensifying human-caused climate change, and they caution against predicting the imminent demise of the region’s summer sea ice. But an 
Extraordinarily low ice levels indicate the summer sea ice has passed a point of no return.
overwhelming majority of Arctic ice experts say that recent data offer powerful evidence that summer sea ice has passed a point of no return.

The dramatic ice loss is being driven by a several key factors, scientists say. Chief among them is that decades of warming have so extensively melted and thinned Arctic sea ice that rapidly expanding areas of dark, open water are absorbing ever-greater amounts of the sun’s radiation, further warming the region in a vicious cycle.

Second, swiftly warming air and ocean temperatures in the Arctic have, for now at least, altered atmospheric activity, with two consequences: Warmer air is being pulled into the Arctic, and increased storms and cyclones in summer are not only driving ice out of the Arctic basin, but also breaking up the ice pack and further exposing more dark water.

And finally there is the inescapable reality that steadily rising levels of carbon dioxide being pumped into the atmosphere by human activity are continuing to warm the Arctic and the rest of the globe, further hastening the loss of Arctic Ocean ice. Several experts say that the only thing that could slow this disappearance — and then only for a few years — would be a major volcanic eruption that reduces the amount of the sun’s energy striking the earth.

“It’s sobering to see the Arctic change so rapidly,” said Ted Scambos, senior research scientist at the National Snow & Ice Data Center in Colorado. “Simply staring at the satellite data that we’re seeing every day is awesome, but in a sad sort of way. It doesn’t look like the Arctic anymore. The summer ice used to look like a cap that nearly filled the Arctic basin. It now looks like a raft with room on every side. You can imagine what it’s going to 
‘The summer ice used to look like a cap…. It now looks like a raft with room on every side.’
look like when the North Pole is open water, when there is only a tiny amount of ice left in August and September. The planet will look a lot different.”

The loss of the great white dome of ice at the top of the world in summer will have profound effects, scientists say. These include a reduction of the amount of solar radiation reflected back into space by the ice, significant changes to the jet stream and Northern Hemispheric weather patterns, and even-more rapid warming in the far north, speeding the melting of Greenland’s massive ice sheets and increasing global sea levels.

In addition to these impacts, said Drinkwater, “Increased storminess will generate ocean wave systems which, un-damped by the presence of sea ice, will pound the circumpolar north coastlines. Current rates of coastal permafrost degradation will be accelerated, leading to significant coastal erosion and reconfiguration of the high-latitude shoreline. Meanwhile, we have also recently heard about the potential for release of sub-sea methane deposits and thereby an acceleration of the current greenhouse effect.”

The record low sea ice extent in 2007 of 4.2 million square kilometers was due to some unusual circumstances, including a sunny summer in the Arctic and higher temperatures. Summer sea ice extent rebounded somewhat in the next several years, rising to 5.3 million square kilometers in 2009, giving some hope to mainstream scientists that Arctic sea ice was not in a “death spiral.”

But Scambos and other experts say that recent data on plummeting ice extent and volume show that the Arctic has entered a “new normal” in which ice decline seems irreversible. Because of thinning ice and swiftly expanding areas of open water, the Arctic Ocean will no longer be kept frigid in summer by the reflectivity of snow and ice — the so-called ice-albedo effect, in which ice and snow reflect a high percentage of the sun’s energy back into space.

Arctic Sea Ice NASA
NASA
Melting Arctic sea ice.
Thick sea ice that formed over many years is increasingly rare in the Arctic. In the 1960s, submarines routinely encountered 12-foot-thick ice around the North Pole and 20-foot-thick ice in some other areas; now those regions often contain ice that is only three to four feet thick. Many parts of the Arctic Ocean are now covered with thin, year-old ice that melts quickly in spring and summer.

This spring, noted Scambos, extensive late winter snow cover on land melted unusually rapidly, reaching record low levels by June. Sea ice across much of the Arctic began to melt 10 to 14 days earlier than in the preceding few decades. Relatively clear skies from late May through June further hastened the melting of sea ice, but even as cloudier weather prevailed in July and August, the record sea ice retreat continued.

“The sensitivity of the Arctic to a warm summer is much higher now than it was in the 1990s or early 2000s,” said Scambos. “What we’re seeing last year and this year is that 2007 wasn’t a fluke. As we’ve gone forward a few years, we’re seeing that many different patterns of weather lead to significant sea ice loss in the Arctic.”

Scambos does not foresee summer sea ice in the Arctic largely disappearing this decade, estimating that such an event could occur around 2030, “plus or minus a decade.” He said the “endgame” of Arctic summer sea ice will probably mean that around 1 million square kilometers — about 15% of what existed in the mid-20th century — will remain in the Canadian High Arctic and some other regions, leaving the North Pole generally ice-free in August and September.

Drinkwater said that changing weather patterns, related to more heat and moisture being released into the Arctic atmosphere, have played a significant role in accelerating sea ice loss. Sea ice retreat in the past decade has been accompanied by a trend toward lower atmospheric pressure and more storms and cyclonic activity, which in turn breaks up
Changing weather patterns have played a significant role in accelerating sea ice loss.
the pack ice and exposes more open water. A powerful Arctic storm earlier this month did just that, Drinkwater noted.

He said that Arctic sea ice could conceivably rebound for some period of time if atmospheric circulation changes and a pattern known as the Arctic Oscillation — currently in a positive phase — moves into a negative phase and ushers in a period of prolonged high atmospheric pressure and fewer storms. This, said Drinkwater, would enable sea ice to remain trapped in the Arctic basin and thicken.

“However,” added Drinkwater, “this seems like blind hope in a system whose feedbacks all appear geared to getting rid of sea ice.”

Judith Curry [snip].

MORE FROM YALE e360
Linking Weird Weather to
Rapid Warming of the Arctic
The loss of Arctic summer sea ice and the rapid warming of the Far North are altering the jet stream over North America, Europe, and Russia. As Jennifer Francis writes, scientists are now just beginning to understand how these profound shifts may be increasing the likelihood of more persistent and extreme weather.
READ MORE
Jay Zwally, chief cryospheric scientist at NASA’s Goddard Space Flight Center and an observer of Arctic ice for 40 years, places little stock in the likelihood of a reversal of disappearing Arctic ice. New satellite technology has given scientists the ability to measure the height of sea ice above the water, and hence ice volume. Those measurements, he said, have vividly underscored that Arctic sea ice is in a swoon.

For example, a recent analysis of data from CryoSat and NASA’s ICESat satellite estimates that the volume of sea ice in a large area of the central Arctic Ocean has plummeted in late winter — February and March — by nearly half in just eight years, from an estimated 13,000 cubic kilometers in 2004 to 7,000 cubic kilometers in 2012.

“We’ve gone through a tipping point, and of all the things a tipping point applies to, sea ice is the most appropriate, because the idea is when it goes below a certain thickness it doesn’t go back under present conditions,” said Zwally. “People can get hung up on the specifics and lose track of the big picture, which is that it’s getting worse and it’s going to get [even] worse.”

http://e360.yale.edu/feature/tipping_point_arctic_heads_to_ice_free_summers/2567/

Tuesday, June 21, 2011

Cryosat mission delivers first sea-ice map: Arctic sea ice thickness Jan-Feb 2011


Cryosat mission delivers first sea-ice map

Map showing ice thickness in the Arctic

Related Stories

This is the best view we have yet had of the thickness of sea-ice across the entire Arctic Ocean basin.
It is the first fully processed map from Europe's new Cryosat spacecraft.
It only covers the months of January and February, but the UK team behind the data says it can now roll out the information on a continuous basis.
The extent of Arctic sea-ice has become a major issue in recent years, with summer melting appearing to outstrip what many climate models had predicted.
But a proper assessment of the status of the sea-ice requires knowledge also about its thickness - something scientists have only recently had the tools to measure from space.
Sea-ice (S.Laxon)The old ice in the Arctic tends to have rough ridges
"Some years the wind will push the ice out of the way or pile it up, and it may look from the area coverage like it's all melted," explained the Cryosat mission's principal investigator, Professor Duncan Wingham.
"But it's only when you combine the area coverage information with the thickness information that you get the product - volume. And that's what you really need to know to answer the question about melting," he told BBC News.
Professor Wingham presented Cryosat's first ice map here at the Paris Air Show in Le Bourget, a major event in the space calendar.
The European Space Agency (Esa) launched its "ice explorer" last year. It carries one of the highest resolution synthetic aperture radars ever put in orbit.
The instrument sends down pulses of microwave energy that bounce off both the top of the Arctic sea-ice and the water in the cracks, or leads, which separate the floes.
By measuring the difference in height between these two surfaces, the Cryosat team is able, using a relatively simple calculation, to work out the overall volume of the marine ice cover in the far north.
Wingham's group at the Centre for Polar Observation and Modelling, University College London, has spent the past year learning how to interpret the radar data and turn it into a form that the research community can use.

How to measure sea-ice thickness from space

Infographic (BBC)
  • Cryosat's radar has the resolution to see the Arctic's floes and leads
  • Some 7/8ths of the ice tends to sit below the waterline - the draft
  • The aim is to measure the freeboard - the ice part above the waterline
  • Knowing this 1/8th figure allows Cryosat to work out sea ice thickness
This has involved calibrating the instrument and then validating its output by comparing it with independent assessments.
One such assessment employed a German Alfred Wegener Institute (AWI) aeroplane.
It obtained thickness information by flying a laser altimeter to record the distance to the top of the ice and a conductivity sensor to identify the location of seawater on the underside of the floes. Being an aeroplane, it could only record limited lines of data, but these strongly correlated with the Cryosat observations.
Another independent assessment called on a different type of radar satellite instrument known as a scatterometer, which, as its name suggests, looks at how much of the energy beamed down from space is reflected back or scattered away. This type of instrument can discern the thin flat seasonal ice from the rough terrains associated with floes that have been around for many years.
Again, what the scatterometer saw with its approach was an excellent match for the Cryosat map.
Validation of ice dataThe Cryosat team has been "in the field" to validate the satellite's measurements
"We're now processing the rest of the Cryosat data to get it to the same standard as we're showing you here," said CPOM researcher Dr Katharine Giles. "Then we will use that data to look at how the ice cover is changing. This is only two months of data - and we're very excited to have our first map - but we need to compare year-on-year changes."
Scientists already have a number of insights on sea-ice thickness in the Arctic - from buoys, from submarine sonar data, from field expeditions, from aircraft sorties such those by the AWI, and from previous generations of satellite radar and laser altimeters. But Cryosat should be a big boost to that data haul, not least because it sees the entire Arctic basin, right up to two degrees from the pole.
In addition to its sea-ice mission, Cryosat is also tracking changes in land-ice.
For this, the radar instrument carries a second antenna. By listening to the radar echoes with an additional device offset from the first by about a metre, the satellite can sense much better the shape of the ice below, returning more reliable information on slopes and ridges.
This is especially important in Greenland and Antarctica where past missions have struggled to discern events at the edges of the ice sheets - the very locations where some of the biggest, fastest changes have been taking place.
Here at Le Bourget, an elevation model built from Cryosat data was displayed of Antarctica. Again, this covered just the months of January and February this year.
Antarctica (CPOM/UCL/A.Shepherd/Esa/Planetaryvisions)
• As with the Arctic sea-ice map, this height model of Antarctica incorporates just two months of data at the start of the year
• The outer ring shows the closest older satellites could get to the pole. The inner hole is the only portion unseen by Cryosat
• The exaggerated model has been sliced open like a cake to show the position of the Antarctic bedrock under the ice
• By subtracting ice-surface height from bedrock height, Cryosat can derive ice thickness across the entire continent
Cryosat was given an initial mission plan to 2013, but engineers fully expect it to keep working until perhaps 2017. To pay for that extension, Esa will need to get new funding from Europe's space ministers when they meet for their big conference in Italy next year.
Dr Volker Liebig, the director of Earth observation at the agency, said Cryosat had already made a compelling case for the additional support - and perhaps for something even bigger down the line.
"Cryosat is a science mission that is part of Esa's Envelope Earth observation programme. I think it has the makings of a [on-going] operational mission," he told the air show presentation.
"The need for this data will not stop when we retire this mission. The first step is to run Cryosat for as long as possible, but then we have a couple of missions that have the potential to become operational - and Cryosat is one of them."

Friday, June 10, 2011

CryoSat Greenland camp receives Prince Willem-Alexander of The Netherlands


CryoSat Greenland camp receives royal guest

Wednesday, May 11, 2011

ESA's CryoSat team working on the Greenland ice sheet has been honoured with a visit from a Dutch delegation including HRH Prince of Orange. The visit is part of a tour to learn more about climate change in polar regions and consequences for the environment.

Prince Willem-Alexander's visit to Greenland was at the invitation of the World Wide Fund for Nature-Netherlands. The delegation included Johan van de Gronden, CEO of WWF-NL, Robbert Dijkgraaf, President of the Royal Dutch Academy of Science, Erik Oostwegel, Chairman of the Board of Management of Royal Haskoning, and Dutch scientists involved in polar climate research.

The six-day tour offered the delegation the opportunity to experience the Arctic and learn more from scientists out in the field.

As part of the CryoSat mission, scientists are currently out on the Greenland ice cap making detailed measurements of snow and ice properties required to validate data from the satellite.

This provided an ideal chance for the delegation to learn first hand about how ESA's ice mission will provide key answers to questions such as how fast the Greenland ice cap is melting and how this will contribute to global sea-level rise.
HRH The Prince of Orange visits Greenland
[The prince is the guy in the front row in blue.]
As much of the Netherlands lies below sea level, there is a vested interest in understanding exactly what is happening to polar ice, in particular that lying on land.

Johan van de Gronden, CEO of WWF-Netherlands, said, "Changes in polar ice cover are key indicators of climate change – important not only for the Netherlands, but the whole world.

"It is vital that these changes are monitored very closely so that we have scientific evidence of exactly what is happening.

"This knowledge is crucial to learn more about climate change and to help develop mitigating strategies."

Launched in April 2010, ESA's CryoSat mission was developed to map trends in polar ice thickness with unprecedented accuracy. In doing so, it will provide a clearer understanding of the changing environment in these climate critical regions.

The current CryoSat Validation Experiment campaign has been underway since early April with experiments being carried out in Devon Island and Alert in northern Canada, the Baltic Sea, Svalbard, the Fram Strait and central Greenland. 

The measurements being gathered will be compared with CryoSat's data to ensure that the mission realises the best possible global maps of ice-thickness change. 

This extensive Arctic venture has involved scientists from numerous organisations braving temperatures of –30 °C to take measurements of snow, land ice and sea ice on the ground and from the air while CryoSat passes above. 

Most of the airborne measurements are acquired from a Twin Otter carrying a radar altimeter called ASIRAS, which simulates the instrument on CryoSat and can, therefore, be used directly for validation. 

In addition, NASA has carried out several joint measurement flights for ESA during their IceBridge campaign to survey polar ice. 

The Prince was met in Greenland by Volker Liebig, ESA's Director of Earth Observation Programmes. Prof. Liebig said, "It was an honour for ESA to introduce the CryoSat mission to Prince Willem-Alexander and the Dutch delegation. 

"This provided an opportunity to present ESA's Earth observation missions and CryoSat in particular, and illustrate the importance of satellites to monitor our environment. 

"Through our visit to the scientists working on the ice sheet, we could illustrate the polar environment that CryoSat is now mapping from space. 

"We were also able to show the efforts taken on the ground and from aircraft in this harsh polar environment to ensure that these maps provide ice-thickness information with the highest possible accuracy."