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pine island glacier map

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An expedition to the ice shelf of the remote Pine Island Glacier, a major outlet of the West Antarctic Ice Sheet that has rapidly thinned and accelerated in recent decades, has been completed. [3], Derzeit (2014) ist der Pine-Island-Gletscher für 20 % des Masseverlusts des Westantarktischen Eisschilds verantwortlich. Pine Island Glacier Data Set Map Midpoint location for each velocity vector in the data set, plotted on December 18, 1988 Landsat image. View Pine Island Glacier in a larger map. The catchments of Pine Island Glacier and Thwaites Glacier in the Amundsen Sea Embayment are two of the largest, most rapidly changing, and potentially unstable sectors of the West Antarctic Ice Sheet. The story was similar, albeit less dramatic, with the iceberg that calved in 2015, breaking into several pieces just a few weeks later. The Pine Island Glacier is visible stretching from the right of the image to the centre. 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). Stay tuned for the latest approaches to hydrographic data acquisition and processing, with a special focus on automatization and digitalization. We map the detailed chan-nel network and conduct a quantitative morphometric com-parison between the channels in Pine Island Bay and the ter-restrial channels comprising the Labyrinth. Presence of one currently erupting subglacial volcano beneath the Pine Island Glacier . [10][11] Schon im Jahr 1993 war auf einen möglichen Einfluss der dortigen vulkanischen Aktivität auf die Stabilität des Eisschildes hingewiesen worden.[12]. (Courtesy of NASA) This month, an iceberg nearly the size of Atlanta broke off in Antarctica. Using the time series of satellite images for the Pine Island Glacier, the researchers were now able to test this thesis step by step. August 2020 um 09:48 Uhr bearbeitet. Posted February 13, 2020 15:06:44 Top Stories. The Pine Island Glacier is the largest discharger of ice in Antarctica and the continent's fastest moving glacier. O’Hare, Dieter Mach, John W. Holt, Donald D. Blankenship, David L. Morse, Duncan A. Image. Questions about using the RSS feed? Pine Island Glacier’s Newest Iceberg. 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 … Images and Data for Pine Island Glacier measured between 05.10.2015 and 11.04.2020. Damit ist der Gletscher, was den Gesamtmasseverlust betrifft, auch der am stärksten schwindende weltweit. With nothing left to stop them, the ice masses rapidly flow out to sea – at least that’s the theory. Location of study area. Find local businesses, view maps and get driving directions in Google Maps. The figure here shows how this might happen as warming water melt the ice from below. As a first application, we shall derive an elevation map of Walgreen Coast, Antarctica, the region that encompasses Pine Island Glacier, from GLAS data. [5], Im Oktober 2011 zog der Gletscher die Aufmerksamkeit auf sich, als sich 20 km hinter der Kalbungsfront ein etwa 30 km langer Riss im Schelfeis gebildet hatte. The Pine Island Glacier in Western Antarctica is not only one of the fastest-flowing ice streams in the Southern Hemisphere; over the past eleven years, four major icebergs have calved from its floating tongue. Dabei ist zu beachten, dass der im Rückzugsgebiet zunehmend steiler abfallende Meeresboden einem Rückzug der Grounding Line eigentlich entgegenwirkt haben sollte. 53, Issue. In this example, the main goal is to parameterize and model a real glacier. Mit diesem prognostizierten Masseverlust verursacht allein dieser Gletscher einen Meeresspiegelanstieg von 3,5 bis 10 mm innerhalb der nächsten 20 Jahre. Watch the glacier’s ice front as it retreats and sheds some notable icebergs over the past two decades. news, Proven Source for Hydrographic Professionals, Sonardyne’s Solstice MCM Sonar Now MINTACS-compatible for Royal Australian Navy, New Charity to Support Global Maritime Safety and Education, Sea-level Monitoring Satellite First Results Surpass Expectations, Ocean Infinity Selects Sonardyne for Pioneering Armada Fleet, New Partnership Between Schmidt Ocean Institute and Intergovernmental Oceanographic Commission of UNESCO, www.hydro-international.com/content/rss/news, www.hydro-international.com/content/rss/articles, Researchers Map Seafloor Near Pine Island Glacier. [4] Man geht davon aus, dass die Schmelzvorgänge im Meer und das Ausdünnen des Eisschelfs dazu führen, dass das Gletscherende dem Eisstrom weniger Widerstand entgegensetzt und somit ebenfalls für das Ausdünnen des kontinentalen Teils des Gletschers verantwortlich ist. Pine Island Glacier in Antarctica spawns new iceberg on February 11, 2020. The Pine Island Glacier flows out of Antarctica’s Hudson Mountains and floats over the ocean. Ein solcher Vorgang ist bei einem solchen Gletscher allerdings nicht ungewöhnlich und nicht notwendigerweise auf die Erderwärmung zurückzuführen. According to the U.S. National Ice Center, this iceberg, named B-46, has an area of 87 square miles. The West Antarctic ice sheet: behavior and environment. 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. Together with its neighbouring glaciers, every year the up to 50-kilometre-wide ice stream transports more than 300 gigatonnes of ice from the hinterland to the Amundsen Sea, and is responsible for between five and ten percent of the global sea-level rise. [9] Während der Großteil des beobachteten Abschmelzens nicht durch diesen Vulkanismus verursacht wird, sondern ein Effekt der globalen Erwärmung ist, so sei der Vulkanismus dennoch als zusätzlicher Faktor in künftigen Szenarien zu berücksichtigen: Magmaflüsse könnten sich innerhalb der vulkanisch aktiven Region ändern; oder die geringer werdende Last des abschmelzenden Eisschildes könnte die vulkanische Aktivität verstärken. 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“. It is a great way to boost corporate knowledge and to stay current on the latest news and developments in the hydrographic industry. Der starke Rückgang im Jahr 2012 war vermutlich auf die deutliche Abkühlung der Amundsen-See zurückzuführen. Pine Island Glacier drains much of the marine-based West Antarctic Ice Sheet, and it has a configuration susceptible to rapid disintegration and recession. That must be what happened during a calving event in 2007. Image. Pine Island Glacier in Antarctica spawns new iceberg on February 11, 2020. 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. View the forecasted snow maps for the region around Pine Island Glacier. NASA Earth Observatory animation by Lauren Dauphin, using MODIS data from NASA EOSDIS/LANCE and GIBS/Worldview. Pine Island Glacier is also buttressed by a large, floating ice shelf, which is itself thinning and which calved a huge iceberg in late 2018.That iceberg was labeled B46 by scientists. Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung Stabsstelle Kommunikation und Medien Am Handelshafen 12 27570 Bremerhaven 18]). Pine Island and Thwaites glaciers. Weather maps produced by aq.freemeteo.com. Maps for all. In 2009, researchers sent a robot submarine beneath Pine Island Glacier’s floating ice tongue and discovered a ridge about half the size of the one off Thwaites Glacier. Scale: lines x samples = 86km x 90km. 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. 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. Get permission to reuse our content quickly and easily with PLS Permissions Request. Washington, DC, American Geophysical Union, 237 – 256. 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. But for most of the ice shelves in the Antarctic, we know very little about the features of the underlying seafloor. Banking over the edge of Pine Island Glacier ice shelf (6305643431).jpg 5,184 × 3,456; 2.59 MB The glacier is one of the main pathways for ice entering the Amundsen Sea from the West Antarctic Ice Sheet, and is one of the fastest-retreating glaciers in Antarctica. Image Information. Der Pine-Island-Gletscher (englisch Pine Island Glacier, abgekürzt PIG) ist ein bedeutender Eisstrom im Ellsworthland in Westantarktika. The catchments of Pine Island Glacier and Thwaites Glacier in the Amundsen Sea Embayment are two of the largest, most rapidly changing, and potentially unstable sectors of the West Antarctic Ice Sheet. 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. Diese wurde durch die vorherrschenden östliche Winde verursacht, die durch einen starken La-Niña-Effekt bedingt waren. Normalerweise sind in diesem Gebiet westliche Winde vorherrschend. (Photo: Jan Erik Arndt). Satellite altimetry and interferometry show that the grounded PIG thinned by up to 1.6 meters per year between 1992 and 1999, affecting 150 kilometers of the inland glacier. Die Abbruchskante verschiebt sich seit langem immer mehr in Richtung Land. 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. The Pine Island Glacier. "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.. A second, applied objective is to map elevation changes in Pine Island Glacier, a glacier that plays a key role in the question of stability of the West Antarctic Ice Sheet and has been changing rapidly in recent years. The glacier is one of the main pathways for ice entering the Amundsen Sea from the West Antarctic Ice Sheet, and is one of the fastest-retreating glaciers in Antarctica. As such, our Polarstern expedition in February 2017 was an unprecedented opportunity to map 370 square kilometres of an area that had previously largely been covered by the Pine Island Glacier’s ice shelf,” explains first author Dr Jan Erik Arndt from the Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research (AWI) in Bremerhaven. [3] Eine weitere im Jahr 2014 veröffentlichte Studie machte deutlich, dass der Pine-Island-Gletscher sehr sensitiv auf Klimaveränderungen reagiert. Located near the base of the Antarctic Peninsula—the “thumb” of the continent—the glacier lies more than 2,600 kilometers (1,600 miles) from the tip of South America. 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. Simply search for Hydro International and fill in the article you are looking for. Der Gletscher gilt als destabilisiert; im Jahr 2017 ist seine Fließgeschwindigkeit auf 2,5 Meilen pro Jahr gestiegen. [6] Dies führte am 8. (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. Pine Island Glacier drains much of the marine-based West Antarctic Ice Sheet, and it has a configuration susceptible to rapid disintegration and recession. 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. Model Pine Island Glacier Follow an example of how to create a mesh and set up the floating ice shelf of a real-world glacier Use observational data to parameterize the model Learn how to use inversions to infer basal friction and plot the results Introduction. When one of the rifts finally became too large, the entire face of the ice shelf broke off. Find more information on www.geo-matching.com! Drei verschiedene Simulationen für den Pine-Island-Gletscher kamen zum Ergebnis, dass sich der Pine-Island-Gletscher recht rasch weitere 40 Kilometer zurückziehen wird. Raw Images. The new maps of the ocean floor in Pine Island Bay, which is predominantly 800 to 1,000 metres deep, reveal a previously unmapped submarine ridge and two mountains, the peaks of which reach up to a water depth of 370 metres. Pine Island Glacier — Last month it was discovered that a large iceberg had recently separated from the calving front of Antarctica’s Pine Island Glacier. NASA-Forschungsflug über den Pine-Island-Gletscher im November 2011. The Landsat satellite acquired the image on January 13, 2001. 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. Pine Island Glacier’s Newest Iceberg. It is possible that a retreat of the PIG may accelerate ice discharge from the WAIS interior. Images and Data for Pine Island Glacier measured between 02.04.2016 and 28.06.2020. Retreat at Pine Island Glacier. The bathymetric maps of the seafloor in Pine Island Bay and the results of the image analyses can now be fed into computer models of the West Antarctic Ice Sheet, helping produce more accurate simulations. [7], 2014 befand sich die Grounding Line an einer Stelle, an der der Meeresboden zur Küste hin nicht ansteigt, sondern zunächst wieder abfällt. Inset shows map extent in Antarctica. Between April and May 2007, the detached iceberg in front of Pine Island moves significantly. 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. The January 2011 Landsat satellite imagery (not shown) showed a series of splits along the western edge of the glacier. Share on Facebook; Share on Twitter; Share on Reddit; Share on Google+; Share on Pinterest; Embed; earthobservatory.nasa.gov. Media in category "Pine Island Glacier" The following 44 files are in this category, out of 44 total. CrossRef; Google Scholar; Wang, Xianwei Cheng, Xiao Gong, Peng Shum, C.K. Click on the grey box links to switch between ice velocity products from the 270 different Sentinel-1 image pairs for Pine Island Glacier from the first image pair starting on 15.11.2014 to the final pair on 22.06.2020. Weeks camped on Antarctica 's Pine Island Glacier is the largest discharger of ice in spawns! Happen as warming water melt the ice shelf basal channels in deep-water upwelling, polynyas and ocean in... On Google+ ; Share on Facebook, LinkedIn, Twitter or sign up for the latest news developments... 27570 Bremerhaven Pine Island Glacier 3,5 bis 10 mm innerhalb der nächsten 20 Jahre, was den betrifft! Wird, nimmt jährlich um ungefähr einen Meter ab Masseverlusts des Westantarktischen Eisschilds verantwortlich nimmt um! 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