{"id":8466,"date":"2016-04-15T08:58:28","date_gmt":"2016-04-15T08:58:28","guid":{"rendered":"http:\/\/revoscience.com\/en\/?p=8466"},"modified":"2016-04-15T08:58:28","modified_gmt":"2016-04-15T08:58:28","slug":"nansen-give-birth-to-two-icebergs","status":"publish","type":"post","link":"https:\/\/www.revoscience.com\/en\/nansen-give-birth-to-two-icebergs\/","title":{"rendered":"Nansen give birth to two icebergs"},"content":{"rendered":"
\n
\"Birth
<\/span><\/a><\/span> Birth of two icebergs<\/span><\/figcaption><\/figure>\n

Multiple satellites, including Europe\u2019s Sentinels, have captured images of two large icebergs that broke away from Antarctica\u2019s Nansen ice shelf on 7 April.<\/span><\/p>\n

The icebergs are drifting to the northeast, propelled by wind, tides and currents. Experts say they do not pose any immediate threat of blocking supply routes to research stations such as the Italian Mario Zucchelli and South Korean Jang Bogo Stations in Terra Nova Bay.<\/span><\/p>\n

Nonetheless, the icebergs may pose a threat to sea-floor moorings in the region that have been used by Italy\u2019s National Antarctic Programme since the 1990s, and more recently by New Zealand ocean scientists.<\/span><\/p>\n

The Nansen ice shelf, around 50 km long and 25 km wide, developed a fracture over recent years. Ice shelves are particularly sensitive to climate change because they can melt from warm air at the surface and warming ocean waters below.<\/span><\/p>\n<\/div>\n

\n

\u201cThe crack was first observed during fieldwork in 1999 and was progressively growing, and then accelerating during 2014,\u201d said Massimo Frezzotti from Italy\u2019s ENEA research organisation.<\/span><\/p>\n

\u201cThe events following were typical for a cycle of ice-shelf calving. Last century, a first calving event is known to have occurred between 1913 and the 1950s, with a second between 1963 and 1972.\u201d<\/span><\/p>\n

\"East
<\/span><\/a><\/span> East Antarctica<\/span><\/figcaption><\/figure>\n

As winter weather began to set in during early March this year, optical images from Europe\u2019s Sentinel-2A satellite and radar images from Sentinel-1A, together with images from the Italian Cosmo-Skymed mission, indicated that the ice front was only tenuously attached to the shelf.\u00a0<\/span><\/p>\n<\/div>\n

\n

By 6 April, the fracture had reached about 40 km long before it severed the portion of the ice front between Inexpressible Island to the north and the Drygalski Ice Tongue \u2013 the floating end of the David Glacier \u2013 to the south.<\/span><\/p>\n

Verified by NASA\u2019s Terra satellite, the calving took place on 7 April during persistent strong offshore winds. Two days later, Sentinel-1A\u2019s radar confirmed the separation.<\/span><\/p>\n

\u201cThe area of the fracture was still negligible at the beginning of 2014, but between April 2015 and March 2016 it expanded from 11.68 sq km to 25.87 sq km, signalling a coming calving,\u201d said Flavio Parmiggiani of Italy\u2019s ISAC-CNR research organisation.<\/span><\/p>\n<\/div>\n

\n

The fracture split the ice shelf along its length, resulting in two large icebergs measuring about 10 km and 20 km in length and 5 km across. Published research indicates that the bergs are likely to be around 250\u2013270 m thick.<\/span><\/p>\n

\"Nansen<\/a>
Nansen fracture<\/figcaption><\/figure>\n

Massimo Frezzotti explained, \u201cHistory has shown that major calving typically occurs about every 30 years. The crack opened because of a difference in the velocity of ice between the northern Priestley Glacier and southern Reeves Glacier fed portions of the ice shelf, caused by the southern part being hooked and pulled along by the faster moving Drygalski Tongue.\u201d<\/span><\/p>\n

\n

The Sentinels are a fleet of satellites for Europe\u2019s Copernicus environment monitoring programme. The second in the Sentinel-1 constellation, Sentinel-1B, is set for launch on 22 April.<\/span><\/p>\n

\u201cThis event illustrates the complexity of the constantly evolving Antarctic icescape,\u201d said ESA\u2019s Mark Drinkwater and Chair of the Polar Space Task Group.<\/span><\/p>\n

\u201cCopernicus data already provide a critical source of sustained data for studying the impact of the climate on the polar cryosphere over the next decades.\u201d<\/span><\/p>\n

This unique combination of Sentinel high-resolution optical and radar images, together with information from other missions, demonstrates how satellites are invaluable sources of data to the study of ice shelf calving. This allows researchers to monitor the future response of the glaciers to the removal of the ice shelves, improving ice sheet modelling and predictions.<\/span><\/p>\n

Enrico Brugnoli, Director of Italy\u2019s CNR National Research Council Earth and Environment Department, commented, \u201cThis event has happened so close to our Mario Zucchelli coastal station and it is the first time satellites have captured an event of this size since Italy has been operating in the area in 1985.\u201d<\/span><\/p>\n

\n<\/div>\n

\n<\/div>\n","protected":false},"excerpt":{"rendered":"

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