A strange gigantic ‘monolith’ iceberg has been spotted by NASA scientists flying over Antarctica.
The rectangular berg was spotted off the east coast of the Antarctic Peninsula, near the Larsen C ice shelf.
NASA experts believe it may have recently broken off the shelf, and say the sharp angles and flat surfaces are evidence the break occured very recently.
The rectangular berg was spotted near the Larsen C ice shelf, and NASA experts believe it the sharp edges are evidence it may have recently broken off the shelf
WHAT IS A TABULAR ICEBERG?
Tabular icebergs split off the edges of ice shelves in the same way a fingernail that grows too long ends up cracking off.
This is why they have sharp edges.
The strange, angular berg is known as a tabular iceberg.
‘A tabular iceberg can be seen on the right, floating among sea ice just off of the Larsen C ice shelf,’ the space agency said.
‘The iceberg’s sharp angles and flat surface indicate that it probably recently calved from the ice shelf.’
The image was taken during an IceBridge flight—an airborne survey of the planet’s polar ice that gives a 3D view of the ice that makes up the Arctic and Antarctic, providing vital information on how it changes over time.
In an interview with LiveScience, NASA scientist Kelly Brunt said ‘tabular icebergs are rather like fingernails that crack of, giving them sharp edges.
‘What makes this one a bit unusual is that it looks almost like a square,’ she said.
She estimated its size to be about a mile wide.
Scientists have been closely tracking Larsen C since a massive iceberg broke free, and began to spin.
The ‘pizzaberg’: This berg resembles a slice of pizza. The Triangular iceberg surrounded by many different types of sea ice, off the Larsen ice shelf in the Weddell Sea. In the open water, grease ice is forming.
From yesterday’s #IceBridge flight: Mountains in the Shackleton Range, bordering Recovery Glacier, East Antarctica.
From Friday’s #IceBridge flight: A lead (fracture within the sea ice) that is partially refrozen and also continuing to freeze over. New, very thin grease ice is forming.
Experts had previously said the giant area, estimated to be about the size of Delaware, was locked into place, saying it ‘likely got stuck on the sea bed’
‘But now A68 has started to swing northwards,’ said Polar oceanographer Mark Brandon recently, who spotted the movement using temperature data collected by the Suomi NPP satellite.
‘You can see at between 7-12 July 2018 the weather conditions and ocean currents conspire to swing the trillion tonnes of the giant iceberg A68 in an anticlockwise direction,’ he said.
‘My guess is that A68a will continue rotating as it is now around that western point, until what is currently the northern edge collides with the Larsen C ice front.
‘It has a spectacular amount of momentum and it’s not going to stopped easily. I should think we will see some interesting collisions with the ice shelf in the next few months.’
It is believed a ‘temperature anomaly’ on 20 July 2018, when it was almost 20 °C warmer than the mean over the Weddell Sea and Larsen Ice shelf, may have triggered the rotation beginning.
Glaciologist and former Project MIDAS collaborator Martin O’Leary told Earther a collision is ‘certainly possible’ he doubts it would have much of an effect on either the iceberg or shelf given the slow-motion speed at which it would occur.
Eventually, O’Leary says the prevailing ocean currents will push the iceberg northwards and eastwards into the Southern Ocean ‘where it will probably break up and melt.’
Left, a ‘temperature anomaly’ on 20 July 2018, when it was almost 20 °C warmer than the mean over the Weddell Sea and Larsen Ice shelf Right: Sentinel-1 SAR satellite imagery from 29 August 2018 shows that to the north of the iceberg the wind is pushing the sea ice northwards faster than the iceberg is rotating. Iceberg A68 captured from with the Sentinel-1 SAR sensor 29 August 2018 23:58 UTC, showing an area of open water where there is intense sea ice generation happening right now.
last year it was revealed dense ice cover had so far prevented it from drifting far out to sea.
An animation showing its movement over the last few months reveals how the trillion-plus ton Iceberg A-68 has shifted as it’s battered by ocean currents, tides, and winds in the Weddell Sea.
While the huge chunk of ice, estimated to be about the size of Delaware, has moved around some, the experts say its surroundings have kept it somewhat locked into place.
Iceberg A-68 is the sixth largest iceberg on record since scientists began keeping track, and its separation from the ice shelf sparked fears about its future impacts on global sea levels.
Despite all the activity in the Weddell Sea, ‘its northern end has repeatedly been grounded in shallower water near Bawden Ice Rise,’ according to Project Midas researchers, who have been monitoring the iceberg over the last year.
‘These groundings led eventually to further pieces of the iceberg being shattered off in May 2018.
‘Whilst not quite large enough to be given labels themselves, the total area of icebergs lost from A-68 in May was the size of a small city.’
Scientists tracking a massive iceberg that broke free from Antarctica’s Larsen C Ice Shelf last year say dense sea-ice cover has so far prevented it from drifting far out to sea. It is shown above in July, 2018
While the huge chunk of ice, estimated to be about the size of Delaware, has moved around some, the experts say its surroundings have kept it somewhat locked into place. Its position back in November, 2017 is shown
Earlier this year, scientists released the first-ever footage of ‘A-68’, a trillion-ton iceberg the size of Delaware that has broken off from Antarctica.
Stunning aerial clips capture the huge crack in Antarctica’s Larsen C ice shelf that led to the third largest iceberg ever recorded breaking off from the continent last July.
When A-68 separated from Larsen C, it revealed an ocean hidden under the ice shelf for 120,000 years, and a team of scientists are now studying the region to uncover some of the hidden ecosystem’s mysteries.
Led by the Cambridge-based British Antarctic Survey (BAS), the group will study tiny animals, microbes and plankton on the seafloor to see how they cope with severe changes to their environment.
As part of preliminary research for the trip, the team have taken aerial footage of the iceberg to monitor how far it has drifted to sea – the very first video captured of the berg since it calved from Larsen C last year.
Marine biologist Dr Katrin Linse, the BAS researcher leading the mission, said: ‘The calving of A-68 provides us with a unique opportunity study marine life as it responds to a dramatic environmental change.
‘It’s important we get there quickly before the undersea environment changes as sunlight enters the water and new species begin to colonise.
‘We’ve put together a team with a wide range of scientific skills so that we can collect as much information as possible in a short time. It’s very exciting.’
The scientists are travelling by ship to collect samples from the newly exposed seabed, which covers an area of around 2,250 square miles (5,800 square kilometres).
WHAT IS THE A-68 ICEBERG AND WHAT CAUSED IT TO BREAK AWAY FROM ANTARCTICA?
In July 2017, a huge crack in Antarctica’s Larsen C ice shelf caused a trillion ton iceberg – the third biggest ever recorded – to break off from the icy southern continent.
The huge chunk of ice, dubbed iceberg A-68, measures 5,800 square kilometres (2,240 square miles), making it around the size of Delaware, or four times the area covered by Greater London.
Since A-68 broke away, it has remained unclear what will happen to the giant mass, with fears it could break up into pieces too small to track on satellite, and drift into shipping lanes.
In July 2017, a huge crack in Antarctica’s Larsen C ice shelf caused a trillion ton iceberg – the third biggest ever recorded – to break off from the icy southern continent. These detailed images were captured by instruments aboard Nasa’s Landsat 8 satellite
Experts have found that cracks are still growing on Larsen C, and if they continue to grow, it’s possible that the ice shelf could collapse.
If all of Larsen C collapses, the ice it holds back might add another 4 inches (10 cm) to global sea levels over the years.
Many scientists argue that a calving event was not necessarily due to climate change.
Instead, it may simply reflect the natural growth and decay cycle of an ice shelf.
The team says their mission is urgent because the ecosystem that’s likely hidden beneath the ice for thousands of years may change as sunlight starts to alter the surface layers of the sea.
The team will investigate the area previously under the ice shelf by collecting seafloor animals, microbes, plankton, sediments and water samples using a range of equipment including video cameras and a special sledge pulled along the seafloor to collect tiny animals.
They will also record any marine mammals and birds that might have moved into the area. Their findings will provide a picture of what life under the ice shelf was like so changes to the ecosystem can be tracked.
A-68 is 620 feet (190 meters) thick from top to bottom, with just 100 feet (30 meters) of it is visible above the ocean.
The iceberg was formed by a single crack along Larsen C, its parent ice shelf, and makes up a little over 10 per cent of the shelf.
BAS researchers flew around the iceberg to get a better view of it as it drifts into the Weddell sea.
This newly exposed marine area is the first to benefit from an international agreement made in 2016 by the Commission for the Conservation of Antarctic Marine Living Resources (CCAMLR).
The edge of A-68, the iceberg the calved from the Larsen C ice shelf. Nasa took this image in November during a flight that was part of its IceBridge program, which will help researchers understand the bedrock under the ice
This agreement designates Special Areas for Scientific Study in newly exposed marine areas following the collapse or retreat of ice shelves across the Antarctic Peninsula region.
The agreement came following a European Union proposal to CCAMLR, led by BAS scientists.
Professor David Vaughan, Science Director at BAS, said: ‘The calving of A-68 offers a new and unprecedented opportunity to establish an interdisciplinary scientific research programme in this climate sensitive region.
‘Now is the time to address fundamental questions about the sustainability of polar continental shelves under climate change.
‘We need to be bold on this one. Larsen C is a long way south and there’s lots of sea ice in the area, but this is important science, so we will try our best to get the team where they need to be.’