ENFIM ATÉ COMEÇARMOS A MORRER AFOGADOS JÁ MORREMOS DE MORTE MATADA DURANTE A IV GUERRA ECONÓMICA GLOBAL 1914-2014 CEM ANOS DE GUERRAS ECONÓMICAS EM LARGA ESCALA

Antarctic ice melt has doubled to 159 GIGATONNES (that's 430,000 Empire State Buildings) a year since 2010, satellite reveals

• Esa's CryoSat-2 mission has provided new data on the Antarctic ice sheet
• It surveyed the region from 2010 to 2013 and found losses had doubled
• In total the ice sheet is losing 159 gigatonnes (159 billion tonnes) each year
• That is twice the rate of ice loss found in the last survey from 2005 to 2010
• And just this loss alone will raise sea levels by half a millimetre a year
• But sea levels will rise much more when other factors are considered

Three years of observations show that the Antarctic ice sheet is now losing 159 gigatonnes (159 billion tonnes) of ice each year - twice as much as when it was last surveyed in 2012.

A team of scientists from the UK Centre for Polar Observation and Modelling, led by researchers at the University of Leeds, have produced the first complete assessment of Antarctic ice sheet elevation change.

They used measurements collected by Esa's CryoSat-2 satellite mission, which carries an altimeter, an instrument to measure altitude, specially designed for this task.

+3

A survey from 2010 to 2013 by Esa's CryoSat-2 satellite shows that the Antarctic Ice Sheet is now losing 159 Gigatonnes of ice each year, enough to raise global sea levels by 0.45 millimetres per year. Colour scale ranges in this image from -1 to +1 metres (3.3 feet) per year

In sharp contrast to previous altimeter missions, CryoSat-2 surveys virtually the entire Antarctic continent, reaching to within 135 miles (215 kilometres) of the South Pole.

This has  enabled a fivefold increase in the sampling of coastal regions where today's ice losses are concentrated.

WHAT 159 GIGATONNES IS EQUAL TO

79.5 trillion laptops
2.27 trillion people
14.5 billion Hubble Space Telescopes
381 million International Space Stations
3.06 million Titanics
430,000 Empire State Buildings
397 times the world’s human population
32 teaspoons of neutron star
22% of the mass of carbon stored in Earth’s atmosphere

Overall, the pattern of imbalance continues to be dominated by glaciers thinning in the Amundsen Sea sector of West Antarctica.

However, thanks to the improved capabilities of CryoSat-2, problem areas such as the rugged terrain of the Antarctic Peninsula can now also be surveyed.

 

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.

The polar ice sheets are a major contributor to global sea level rise and, when combined, the Antarctic losses detected by CryoSat-2 are enough to raise global sea levels by 0.45 millimetres each year alone.

+3

The largest loss of ice is occurring at the West Antarctic Ice Sheet, with the Pine Island Glacier shown here. West Antarctica is losing 139 gigatonnes of the total 159 gigatonnes every year, which is double the rate of ice loss from 2005 to 2010

In West Antarctica, ice thinning has been detected in areas that were poorly surveyed by past satellite altimeter missions.

These newly-mapped areas contribute additional losses that bring altimeter observations closer to estimates based on other approaches.

But the average rate of ice thinning in West Antarctica has also increased, and this sector is now losing almost one third (31%) as much ice each year than it did during the five year period (2005 to 2010) prior to CryoSat-2's launch.

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 [13 to 26 feet] per year near to the grounding lines of the Pine Island, Thwaites and Smith Glaciers.'

This sector of Antarctica has long been identified as the most vulnerable to changes in climate and, according to recent assessments, its glaciers may have passed a point of irreversible retreat.

Launched in 2010, CryoSat carries a radar altimeter that can 'see' through clouds and in the dark, providing continuous measurements over areas like Antarctica that are prone to bad weather and long periods of darkness.

The radar can measure the surface height variation of ice in fine detail, allowing scientists to record changes in its volume with unprecedented accuracy.

+3

ESA¿s Earth Explorer CryoSat-2 mission (artist¿s illustration shown) was launched on 8 April 2010 and is dedicated to precise monitoring of changes in the thickness of marine ice floating in the polar oceans and variations in the thickness of the vast ice sheets that blanket Greenland and Antarctica

Professor Andrew Shepherd, also of the University of Leeds, who led the study, added: 'Thanks to its novel instrument design and to its near-polar orbit, CryoSat allows us to survey coastal and high-latitude regions of Antarctica that were beyond the capability of past altimeter missions, and it seems that these regions are crucial for determining the overall imbalance.

'Although we are fortunate to now have, in CryoSat-2, a routine capability to monitor the polar ice sheets, the increased thinning we have detected in West Antarctica is a worrying development.

'It adds concrete evidence that dramatic changes are underway in this part of our planet, which has enough ice to raise global sea levels by more than a metre [3.3 feet].

'The challenge is to use this evidence to test and improve the predictive skill of climate models.'

And Professor David Vaughan of the British Antarctic Survey said: 'The increasing contribution of Antarctica to sea-level rise is a global issue, and we need to use every technique available to understand where and how much ice is being lost.

'Through some very clever technical improvements, McMillan and his colleagues have produced the best maps of Antarctic ice-loss we have ever had.

'Prediction of the rate of future global sea-level rise must begin with a thorough understanding of current changes in the ice sheets - this study puts us exactly where we need to be.'

And finally Dr Ian Joughin at the University of Washington, author of a recent study simulating future Antarctic ice sheet losses, concluded: 'This study does a nice job of revealing the strong thinning along the Amundsen Coast, which is consistent with theory and models indicating this region is in the early stages of collapse.