Latest images
reveal that the A-68A iceberg has shattered into multiple pieces, with two
large fragments of ice breaking off from the main berg and floating away in the
open ocean. Scientists using satellite data have not only been monitoring the
iceberg’s journey across the South Atlantic Ocean, but have been studying the
iceberg’s ever-changing shape.
The colossal A-68A iceberg –
one of the largest bergs of all time – has drifted slowly northwards since it
broke free from the Larsen-C ice shelf in July 2017, and has been floating
perilously close to South Georgia for the past month.
Marine scientists are
concerned that its presence will harm the fragile ecosystem that thrives around
the island, either through scraping of the iceberg’s keel on the seabed or through
the massive release of cold freshwater into the surrounding ocean. Just how
close the berg will reach depends on how deep its keel is, but only with
measurements of the berg’s changing shape, this has been impossible to
determine with confidence.
Using data from four
different satellites, scientists from the Centre for Polar Observation and
Modelling at the University of Leeds have produced the first assessment of the
iceberg’s changing shape.
The team first built a map of
the icebergs initial thickness from measurements recorded by ESA’s CryoSat satellite radar altimeter in the 12
months before it calved. This detailed map reveals that A-68 was
originally, on average, 232 m thick, and 285 m at its thickest point. The berg
has 30 m deep channels oriented parallel to its narrow side following the
direction Larsen ice shelf was flowing out to sea before it snapped – a common
feature related to ocean melting.
Since it has been drifting in
the ocean, the iceberg’s position and shape have been captured in a sequence of
11 images taken by two different satellites – the Copernicus Sentinel-1 mission, which has an all-weather and year-round
imaging radar, and NASA’s MODIS, which records images that are visible to the
naked eye.
The imagery shows that the
iceberg has halved in size from an initial area of 5664 sq km to its present
extent of just 2606 sq km. A large proportion of this loss has been through the
creation of smaller bergs, some of which are still afloat.
Profiles of the iceberg’s
height have also been recorded on eight separate occasions as it has drifted
and rotated in the ocean by CryoSat and by NASA’s ICESat-2 laser altimeter,
which has been in orbit since September 2018. The coincident satellite imagery
made it possible to orientate the altimeter height profiles relative to the
icebergs initial position and calculate its change in thickness over time.
ESA
- Area, thickness and volume of A-68A
Area, thickness and volume of A-68A
On average, the
iceberg has thinned by 32 m, and by over 50 m in places – around a quarter of
its initial thickness. When combined, the change in thickness and area amount
to a 64% reduction in the iceberg’s volume from 1467 to 526 cubic kilometres.
The iceberg’s future
trajectory depends on how deep its keel is relative to the surrounding ocean.
Although South Georgia lies in a remote spot of the South Atlantic Ocean, it is
surrounded by relatively shallow shelf waters that extend tens of kilometres
beyond its coastline.
At its thickest section, the
A-68A iceberg currently has a 206 m deep keel, and so the main section is
unlikely to travel much closer to the island until it thins or breaks apart.
However, two relatively large fragments which broke away on 21 December are
considerably thinner, with keels that are up to 50 m shallower, and so these
pose the greatest immediate threat.
Since it broke free, the
average melting rate of A-68 has been 2.5 centimetres per day and the berg is
now shedding 767 cubic metres of freshwater per second into the surrounding ocean
– equivalent to 12 times the outflow of the River Thames.
The team will continue to
monitor A-68A and its remnant parts as part of their ongoing assessment of
Earth’s polar regions.
Anne Brackmann-Folgmann, PhD
student at the University of Leeds, said, “Icebergs can have major
environmental impacts, including disturbing ocean circulation, marine
ecosystems, and could block the route between penguin colonies and their
feeding grounds during the breeding season. Thanks to CryoSat, we can track
changes in their thickness, providing advance warning of when and where they
might run aground.”
Jamie Izzard, postgraduate
researcher at the University of Leeds, said, “Satellite altimeters allow us to
measure iceberg terrain with incredible precision, allowing us to detect subtle
features like the shallow surface depression above the basal channel which was
the line of weakness along which the latest bergs calved.”
ESA’s CryoSat Mission
Manager, Tommaso Parrinello, said, “It’s fantastic to know that even in the
remotest parts of our planet, satellites like CryoSat are able to shed light on
events like this and help us to monitor our environment and thanks to the
recent change of CryoSat orbit to sync with ICESat-2, we will see more results
in the future coming from the combination of the two satellite measurements.”
Source: ESA
No comments:
Post a Comment