At Hydro International, we often receive permission requests to use our articles for republishing purposes. O’Hare, Dieter Mach, John W. Holt, Donald D. Blankenship, David L. Morse, Duncan A. In the older images, rises in the ice’s surface can be identified at precisely those points where the peaks of the ridge are directly under the ice shelf. David G. Vaughan, Hugh F. J. Corr, Fausto Ferraccioli, Nicholas Frearson, Aidan The figure here shows how this might happen as warming water melt the ice from below. Pine Island Glacier: Satellite animation mid-2017 to Feb-2020 Date: February 11, 2020 Author: adrianluckman Updated animation showing the last three calving events as seen by ESA’s Sentinel-1 synthetic aperture radar. NASA Earth Observatory animation by Lauren Dauphin, using MODIS data from NASA EOSDIS/LANCE and GIBS/Worldview. In the austral summer of 2012-2013 scientists and support staff spent 6 weeks camped on Antarctica's Pine Island Glacier. In the older images, rises in the ice’s surface can be identified at precisely those points where the peaks of the ridge are directly under the ice shelf. Washington, DC, American Geophysical Union, 237 – 256. 18]). Why is Pine Island Glacier important? Banking over the edge of Pine Island Glacier ice shelf (6305643431).jpg 5,184 × 3,456; 2.59 MB Location map of Pine Island and Thwaites glaciers, in West Antarctica. That must be what happened during a calving event in 2007. PIG) The area of the iceberg poised to calve off the Pine Island Glacier is about 115 square miles, or 300 square kilometers. Observations from geophysical surveys and long-term oceanographic instruments deployed down bore holes into the ocean cavity reveal a buoyancy-driven boundary layer within a basal channel that melts … (A) Map of the Amundsen Sea Embayment, showing location of the study area. (b) Pine Island Glacier ice shelf draft calculated from a surface digital elevation model derived from Worldview satellite stereoscopic optical imagery [Moratto et al., 2010; Shean et al., 2016] assuming hydrostatic equilibrium. Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung Stabsstelle Kommunikation und Medien Am Handelshafen 12 27570 Bremerhaven 60, p. 123. The Pine Island Glacier flows out of Antarctica’s Hudson Mountains and floats over the ocean. Pine Island Glacier Data Set Map Midpoint location for each velocity vector in the data set, plotted on December 18, 1988 Landsat image. "The Pine Island glacier recently spawned an iceberg over (115 square miles) that very quickly shattered into pieces," the European Space Agency (ESA) said in a statement.. The Pine Island Glacier is the largest discharger of ice in Antarctica and the continent's fastest moving glacier. Ein solcher Vorgang ist bei einem solchen Gletscher allerdings nicht ungewöhnlich und nicht notwendigerweise auf die Erderwärmung zurückzuführen. As the satellite images show, back then the edge of the Pine Island Glacier’s ice shelf collided with one of the newly discovered mountains, hitting it so hard that rifts formed in the surface of the ice. Then in 2015, a calving event shifted the edge of the ice shelf 20 kilometres nearer the coast and reduced the floating ice tongue’s total area to roughly 470 square kilometres. In the austral summer of 2012-2013 scientists and support staff spent 6 weeks camped on Antarctica's Pine Island Glacier. When one of the rifts finally became too large, the entire face of the ice shelf broke off. Jan Erik Arndt, Robert D. Larter, Peter Friedl, Karsten Gohl, Kathrin Höppner, and The Science Team of Expedition PS104: Bathymetric Controls on Calving Processes at Pine-Island Glacier. With nothing left to stop them, the ice masses rapidly flow out to sea – at least that’s the theory. Images and Data for Pine Island Glacier measured between 05.10.2015 and 11.04.2020. CrossRef; Google Scholar; Wang, Xianwei Cheng, Xiao Gong, Peng Shum, C.K. Simply search for Hydro International and fill in the article you are looking for. Image. As scientists map the contours of the seafloor in the Amundsen Sea region, they are forming a clearer picture of what the glaciers are doing. Share on Facebook; Share on Twitter; Share on Reddit; Share on Google+; Share on Pinterest; Embed; www.youtube.com. Während im Jahr 2010 der Gletscher ungefähr 69 Kubikkilometer Eis als Schmelzwasser ins Meer transportierte, gab er 2012 mit etwa 35 Kubikkilometern nur etwa die Hälfte an Schmelzwasser ab. That’s slightly larger than the iceberg that previously separated from the glacier in September 2017. M. Holland, David and Li, Xiaowen 2014. Latest ITS UK scientists are about to set out for Antarctica to investigate the huge Pine Island Glacier - the stream of ice that is now contributing more to sea level rise than any other on the planet. Image Information. Pine Island Glacier (PIG) is a large ice stream flowing west-northwest along the south side of the Hudson Mountains into Pine Island Bay, Amundsen Sea, Antarctica. Also in May 2007, a crack in Pine Island becomes visible. Pine Island Glacier is one of the fastest-retreating glaciers in Antarctica. Questions about using the RSS feed? Der Pine-Island-Gletscher (englisch Pine Island Glacier, abgekürzt PIG) ist ein bedeutender Eisstrom im Ellsworthland in Westantarktika. Presence of one currently erupting subglacial volcano beneath the Pine Island Glacier . Der Gletscher gilt als destabilisiert; im Jahr 2017 ist seine Fließgeschwindigkeit auf 2,5 Meilen pro Jahr gestiegen. Laut diesen Simulationen wird der jährliche Masseverlust des Gletschers, der von 1992 bis 2011 noch bei 20 Gigatonnen pro Jahr gelegen hatte, in den nächsten 20 Jahren 100 Gigatonnen pro Jahr betragen – dies entspricht einem Meeresspiegelanstieg von 3,5 bis 10 mm in diesem Zeitraum. It is possible that a retreat of the PIG may accelerate ice discharge from the WAIS interior. Der beschleunigte Verlust an Mächtigkeit, der seit den 1980er Jahren beobachtet wird, wird auf subglaziales Schmelzen am Grund des Eisschelfs zurückgeführt, welches sich durch die kürzliche Intensivierung der Zirkulation des Zirkumpolaren Tiefenwassers verstärkt hat. View the forecasted snow maps for the region around Pine Island Glacier. 1. The Pine Island Glacier (PIG) transports 69 cubic kilometers of ice each year from ∼10% of the West Antarctic Ice Sheet (WAIS). Da der Gletscher in den letzten Jahren eine deutlich negative Massenbilanz aufwies, ist dieser Beitrag gestiegen. The Pine Island Glacier’s more than 400-metre thick ice shelf must have been grounded on the ridge for several decades, as the satellite images of the glacier gathered by the researchers – dating back to 2002 – confirm. Der Pine-Island-Gletscher (englisch Pine Island Glacier, abgekürzt PIG) ist ein bedeutender Eisstrom im Ellsworthland in Westantarktika. Die Abbruchskante verschiebt sich seit langem immer mehr in Richtung Land. Much to their surprise, in the process they determined that submarine highs not only stabilise ice shelves like giant brakes; in some cases, these mountains can also set off calving events – for instance, when the calving front advances, causing it to crash into a mountain with full force. In addition to the two researchers from the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research a member of the British Antarctic Survey and experts from the German Aerospace Center (DLR) took part in the new study. Researchers on board the German research icebreaker 'Polarstern' successfully mapped an area of seafloor previously covered by shelf ice. In February 2017, researchers on board the German research icebreaker Polarstern successfully mapped an area of seafloor previously covered by shelf ice. Retreat of Pine Island Glacier since 1947. Stay tuned for the latest approaches to hydrographic data acquisition and processing, with a special focus on automatization and digitalization. (Courtesy of NASA) This month, an iceberg nearly the size of Atlanta broke off in Antarctica. Der Pine-Island-Gletscher transportiert mehr Eis ins Meer als jeder andere Gletscher weltweit. Scale: lines x samples = 86km x 90km. The peninsula, which juts out to the north-east of the Pine Island Glacier, is among the fastest-warming regions on the planet. The Pine Island Glacier (maximum velocity measured 2.8 km/yr) and Thwaites Glacier (3.4 km/yr) are faster than most Antarctic ice streams, which generally have velocities less than 1.5 km/yr [Ref. By that time, the ice shelf must have melted so extensively from below that it was either too light to produce any impression on the surface of the ice, or the ice sheet must have already lost contact with the mountains beneath it,” says co-author Dr Karsten Gohl from the AWI. … . Weather maps produced by aq.freemeteo.com. It is a great way to boost corporate knowledge and to stay current on the latest news and developments in the hydrographic industry. Inset shows map extent in Antarctica. Between April and May 2007, the detached iceberg in front of Pine Island moves significantly. They are also neighboring outlets, separated by the topographically unconfined eastern shear margin of Thwaites Glacier and the southwest tributary of Pine Island Glacier. Pine Island Glacier in Antarctica spawns new iceberg on February 11, 2020. Maps for all. Even so, when a large crack formed across the glacier in mid 2000, it was surprising how fast the crack expanded, 15 meters per day, and how soon the resulting iceberg broke off, mid-November, 2001. RSS-feed with news from Hydro International:www.hydro-international.com/content/rss/news, Latest articles published on Hydro International:www.hydro-international.com/content/rss/articles. In a comparison with a map of the same area based on ERS-1 data, we will investigate the mapping capabilites of GLAS for different glacio-morphologic units (section 4). Velocity data were derived from the Landsat scenes listed below. Our progress in getting to the Pine Island Glacier (PIG) drill site has been much better than last season. Get permission to reuse our content quickly and easily with PLS Permissions Request. Young: L. Favier, G. Durand, S. L. Cornford, G. H. Gudmundsson, O. Gagliardini, F. Gillet-Chaulet, T. Zwinger, A. J. Payne, A. M. Le Brocq: J. W. Park, N. Gourmelen, A. Shepherd, S. W. Kim, D. G. Vaughan, D. J. Wingham: Pierre Dutrieux, Jan De Rydt, Adrian Jenkins, Paul R. Holland, Ho Kyung Ha, Sang Hoon Lee, Eric J. Steig, Qinghua Ding, E. Povl Abrahamsen, Michael Schröder: Donald D. Blankenship, Robin E. Bell, Steven M. Hodge, John M. Brozena, John C. Behrendt, Carol A. Finn: Vorlage:Infobox Gletscher/Wartung/Bildbeschreibung fehlt, Riesiger Eisberg löst sich vom Pine-Island-Gletscher in der Antarktis, https://de.wikipedia.org/w/index.php?title=Pine-Island-Gletscher&oldid=202402986, „Creative Commons Attribution/Share Alike“. Pine Island Glacier’s Newest Iceberg. The Pine Island Glacier is located around 1,600 miles from the tip of South America. Pine Island Glacier in Antarctica spawns new iceberg on February 11, 2020. [2] Der Pine-Island-Gletscher erstreckt sich vom Hudson-Gebirge bis zur Pine Island Bay in der südlichen Amundsen-See, wo er einen Eisschelf bildet. The January 2011 Landsat satellite imagery (not shown) showed a series of splits along the western edge of the glacier. Most people will never see Pine Island Glacier in person. Brand awareness can affect every stage of the purchase funnel. Der vergletscherte Einzugsbereich hat eine Fläche von 162.300 km², die Eismassen des Gletschersystems machen rund 10 % des Westantarktischen Eisschilds aus. The Pine Island Glacier’s more than 400-metre thick ice shelf must have been grounded on the ridge for several decades, as the satellite images of the glacier gathered by the researchers – dating back to 2002 – confirm.

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