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flight inclusive* Book by 31 March 2021 expedition cruises 2022 | 23 Flight-inclusive o er valid on selected cruises in 2022/23 to Antarctica, Alaska, Northwest Passage, Greenland, Iceland and Svalbard. DESTINATION VOYAGE Days DATE/S SHIP LEAD IN price Antarctica Antarctica and Falklands 16 Nov 2022 – Mar 2023 MS Roald Amundsen £6,095pp Highlights of Antarctica 12 Nov 2022 – Mar 2023 MS Fridtjof Nansen £5,994pp In-depth Antarctica, Falklands and South Georgia 23 Nov 2022 – Feb 2023 MS Fram £8,982pp Alaska Wilderness, Glaciers & Culture 14 May & June 2022 MS Roald Amundsen £3,621pp Inside Passage, Bears & Aleutian Islands 18 July & Aug 2022 MS Roald Amundsen £5,600pp Northwest In the Wake of Great Explorers 26 Aug 2022 MS Roald Amundsen £15,032pp Passage In the Wake of Great Explorers 19/20 Aug & Sep 2022 MS Fram £9,477pp Greenland Disko Bay – The Heart of Greenland 16 Jun–Sep 2022 MS Fridtjof Nansen £5,352pp The Ultimate Fjord and National Park Expedition 13 Aug 2022 MS Fridtjof Nansen £4,941pp Iceland The Land of Elves, Sagas and Volcanoes 9/11 June-Aug 2022 MS Fram/MS Fridtjof Nansen £3,044pp Spitsbergen, Jan Mayen, Iceland – Arctic Islands Discovery 14 July 2022 MS Fram £5,022pp Svalbard In the Realm of the Polar Bear 10 June-Sep 2022 MS Spitsbergen/MS Fram £4,446pp The Ultimate Expedition 12 July-Sep 2022 MS Spitsbergen/MS Fram £5,104pp Island Hopping In and Around the Arctic 15 Sep 2022 MS Spitsbergen £4,198pp *Terms and conditions: Flight inclusive from London valid on selected expedition cruises departing in 2022/23. Any fl ights booked with Hurtigruten are ATOL protected (ATOL 3584). Alternative UK airports also available for a small supplement – contact us for details. O er is subject to availability. O er not combinable with any other o ers, expect ‘Book with Confi dence’ and ‘Ambassador Programme’ © DAN AVILA, GUNTER KRAUSE, ANDREA KLAUSSNER, JULIE SKOTTE, DOMINIC BARRINGTON HURTIGRUTEN; CHASE DEKKER WILDLIFE IMAGES, IACOMINO FRIMAGES SAIL SAIL MS MAUD from SMALL SHIP EXPEDITIONS FROM home APPROX. 500 GUESTS DOVER SAVE UP TO 20%* Valid on selected cruises in 2021/22/23 to Norway’s Northern Lights, Norway’s Fjords and Arctic Sunshine, the British Isles and Southern Scandinavia. Book by 31 March 2021 DESTINATION VOYAGE Days DATE/S SHIP price Norway Northern Lights and Fjords Expedition 15 Mar 2021 – Mar 2022 MS Maud FROM £2,879pp Northern Lights and Fjords Expedition 11/15/22 Mar 2022 – Mar 2023 MS Maud FROM £2,373pp Norwegian Fjords, North Cape and the Arctic Sunshine 15 May – Sep 2021 MS Maud FROM £3,144pp Norwegian Fjords, North Cape and the Arctic Sunshine 11/15/22 Apr 2022 – Sep 2022 MS Maud FROM £2,498pp British Isles Remote Islands, Natural Wonders, and a Diverse Coastline 13 May – Sep 2021 MS Maud FROM £3,229pp Remote Islands, Natural Wonders, and a Diverse Coastline 13 Apr – Sep 2022 MS Maud FROM £2,849pp Picturesque Ports, Isolated Islands and Wonderful Wildlife 15 Apr – Aug 2021 MS Maud FROM £3,039pp Picturesque Ports, Isolated Islands and Wonderful Wildlife 15 Apr – July 2022 MS Maud FROM £3,149pp Southern Archipelagos, Fjords and Quaint Fishing Towns 15 Jun – Aug 2021 MS Maud FROM £3,199pp Scandinavia Archipelagos, Fjords and Quaint Fishing Towns 15 Jun – Aug 2022 MS Maud FROM £3,419pp *Terms and conditions: Save up to 20% o er varies by cabin grade and departure date. New bookings online. Bookings must be confi rmed by 31 March 2021. Hurtigruten operates and fl exible pricing system and prices are capacity controlled, confi rmed at time of booking. Booking terms and conditions apply. © PIOTR KRZESLAK, NEIL WALKER, SOLFRID BØE, STIAN KLO, BENNO HOFF.

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Ice Shelf Advance and Retreat Rates Along the Coast of Queen Maud Land, Antarctica K
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 106, NO. C4, PAGES 7097–7106, APRIL 15, 2001 Ice shelf advance and retreat rates along the coast of Queen Maud Land, Antarctica K. T. Kim,1 K. C. Jezek,2 and H. G. Sohn3 Byrd Polar Research Center, The Ohio State University, Columbus, Ohio Abstract. We mapped ice shelf margins along the Queen Maud Land coast, Antarctica, in a study of ice shelf margin variability over time. Our objective was to determine the behavior of ice shelves at similar latitudes but different longitudes relative to ice shelves that are dramatically retreating along the Antarctic Peninsula, possibly in response to changing global climate. We measured coastline positions from 1963 satellite reconnaissance photography and 1997 RADARSAT synthetic aperture radar image data for comparison with coastlines inferred by other researchers who used Landsat data from the mid-1970s. We show that these ice shelves lost ϳ6.8% of their total area between 1963 and 1997. Most of the areal reduction occurred between 1963 and the mid-1970s. Since then, ice margin positions have stabilized or even readvanced. We conclude that these ice shelves are in a near-equilibrium state with the coastal environment. 1. Introduction summer 0Њ isotherm [Tolstikov, 1966, p. 76; King and Turner, 1997, p. 141]. Following Mercer’s hypothesis, we might expect Ice shelves are vast slabs of glacier ice ﬂoating on the coastal these ice shelves to be relatively stable at the present time. ocean surrounding Antarctica. They are a continuation of the Following the approach of other investigators [Rott et al., ice sheet and form, in part, as glacier ice ﬂowing from the 1996; Ferrigno et al., 1998; Skvarca et al., 1999], we compare the interior ice sheet spreads across the ocean surface and away position of ice shelf margins and grounding lines derived from from the coast.
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Supplementary File For: Blix A.S. 2016. on Roald Amundsen's Scientific Achievements. Polar Research 35. Correspondence: AAB Bu
Supplementary file for: Blix A.S. 2016. On Roald Amundsen’s scientific achievements. Polar Research 35. Correspondence: AAB Building, Institute of Arctic and Marine Biology, University of Tromsø, NO-9037 Tromsø, Norway. E-mail: [email protected] Selected publications from the Gjøa expedition not cited in the text Geelmuyden H. 1932. Astronomy. The scientific results of the Norwegian Arctic expedition in the Gjøa 1903-1906. Geofysiske Publikasjoner 6(2), 23-27. Graarud A. 1932. Meteorology. The scientific results of the Norwegian Arctic expedition in the Gjøa 1903-1906. Geofysiske Publikasjoner 6(3), 31-131. Graarud A. & Russeltvedt N. 1926. Die Erdmagnetischen Beobachtungen der Gjöa-Expedition 1903- 1906. (Geomagnetic observations of the Gjøa expedition, 1903-06.) The scientific results of the Norwegian Arctic expedition in the Gjøa 1903-1906. Geofysiske Publikasjoner 3(8), 3-14. Holtedahl O. 1912. On some Ordovician fossils from Boothia Felix and King William Land, collected during the Norwegian expedition of the Gjøa, Captain Amundsen, through the North- west Passage. Videnskapsselskapets Skrifter 1, Matematisk–Naturvidenskabelig Klasse 9. Kristiania (Oslo): Jacob Dybwad. Lind J. 1910. Fungi (Micromycetes) collected in Arctic North America (King William Land, King Point and Herschell Isl.) by the Gjöa expedition under Captain Roald Amundsen 1904-1906. Videnskabs-Selskabets Skrifter 1. Mathematisk–Naturvidenskabelig Klasse 9. Christiania (Oslo): Jacob Dybwad. Lynge B. 1921. Lichens from the Gjøa expedition. Videnskabs-Selskabets Skrifter 1. Mathematisk– Naturvidenskabelig Klasse 15. Christiania (Oslo): Jacob Dybwad. Ostenfeld C.H. 1910. Vascular plants collected in Arctic North America (King William Land, King Point and Herschell Isl.) by the Gjöa expedition under Captain Roald Amundsen 1904-1906.
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Transits of the Northwest Passage to End of the 2020 Navigation Season Atlantic Ocean ↔ Arctic Ocean ↔ Pacific Ocean
TRANSITS OF THE NORTHWEST PASSAGE TO END OF THE 2020 NAVIGATION SEASON ATLANTIC OCEAN ↔ ARCTIC OCEAN ↔ PACIFIC OCEAN R. K. Headland and colleagues 7 April 2021 Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge, United Kingdom, CB2 1ER. <[email protected]> The earliest traverse of the Northwest Passage was completed in 1853 starting in the Pacific Ocean to reach the Atlantic Oceam, but used sledges over the sea ice of the central part of Parry Channel. Subsequently the following 319 complete maritime transits of the Northwest Passage have been made to the end of the 2020 navigation season, before winter began and the passage froze. These transits proceed to or from the Atlantic Ocean (Labrador Sea) in or out of the eastern approaches to the Canadian Arctic archipelago (Lancaster Sound or Foxe Basin) then the western approaches (McClure Strait or Amundsen Gulf), across the Beaufort Sea and Chukchi Sea of the Arctic Ocean, through the Bering Strait, from or to the Bering Sea of the Pacific Ocean. The Arctic Circle is crossed near the beginning and the end of all transits except those to or from the central or northern coast of west Greenland. The routes and directions are indicated. Details of submarine transits are not included because only two have been reported (1960 USS Sea Dragon, Capt. George Peabody Steele, westbound on route 1 and 1962 USS Skate, Capt. Joseph Lawrence Skoog, eastbound on route 1). Seven routes have been used for transits of the Northwest Passage with some minor variations (for example through Pond Inlet and Navy Board Inlet) and two composite courses in summers when ice was minimal (marked ‘cp’).
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Searching for HMS Terror
ARTICLE KNOWLEDGE GAINED IN THE SEARCH FOR FRANKLIN Searching for HMS Terror “We know where the target is not located” is the only guaranteed result of any search expedition. This statement does not make for exciting headlines, however, the value of knowledge gained during the search itself and its many benefits to a variety of end-users, cannot be easily dismissed. The 2015 Franklin Expedition search coordinated by Parks Canada was the continuing multi-year, multi-partner effort that saw the discovery of HMS Erebus in September of 2014. In this article we will discuss the knowledge gained and multiple uses of the data collected toward our conclusion of verifying where HMS Terror is not located. In 1845, Captain Sir John Franklin led an ill-fated expedition to find the final elusive link in the Northwest Passage through what is now the Canadian Arctic Archipelago. Supplied for three years, HMS Erebus (Figure 1) and HMS Terror sailed from England outfitted with innovative auxiliary steam engines, coal-fired heating systems, and all manner of internal and external hull reinforcement to better withstand the ice -- including bows sheathed in iron hull plating. Given the experience of Franklin, his hand-picked crew, and the well- equipped ships he commanded, few anticipated the tragedy and ensuing searches that continue to this day. Many motivating factors have contributed to the launch of the searches for the ‘Lost Expedition’. Initially it was a rescue mission, and then a recovery mission, when all hope for any survivors was lost. Modern day searches coordinated and funded by the Government of Canada are motivated not only by the important history the lost expedition represents, but the added substantiation to Canada’s sovereignty claim to the Arctic.
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Sail from Dover DAY 9 | Romsdalsmuseet, One of Finnsnes / Senja Norway’S Largest Folk Museums
Return address Hurtigruten Ltd, Unit 1a, Commonwealth Buildings, Woolwich Church Street, SE18 5NS <T><F><S> <COMPANY> <ADDR1> <ADDR2> <ADDR3> <ADDR4> <ADDR5> <ADDR6> <ADDR7> Cust. ref.:<ACCOUNT_ID> <TOWN> <COUNTY> <Job ref>/<Cell>/<Seq. No> <ZIP> <SSC>/<Bag ID>/<Bag no.>/<MS brake> Notifi cation: We use your information in accordance with our Privacy Policy, updated June 2019. Please see www.hurtigruten.co.uk/practical-information/statement-of-privacy/ New expedition cruises 2021 | 2022 SAIL from save up to 20%* DOVER British Isles | Norway’s Northern Lights | Norway’s Arctic sunshine & Fjords | southern Scandinavia MS MAUD welcome For 127 years, Hurtigruten have been With our unique Science Center pioneers in expedition cruising, from as the beating heart of the ship, the rugged coastline of Norway and our expedition team serve as hosts, the Arctic islands, to the remote lecturers, instructors, companions continent of Antarctica. Our mission and guides as they bring to life is to deliver authentic adventures for breath-taking destinations. the naturally curious. Your health and safety is our I am thrilled to present our series top priority, and we constantly of NEW expedition cruises update our protocols and safety from Dover for 2021/22. Start guidelines, in consultation with your holiday without the stress of the Norwegian Government and a crowded airport, as we embark with local health authorities. from the beautiful cruise terminal Please book with confidence, in Dover, to discover hand-picked and for the latest information, gems on expertly-planned itineraries visit our website. visiting the British Isles, southern We can’t wait to welcome you Scandinavia and the stunning onboard MS Maud.
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(TSFN): 0402917N-M AMENDED Research Report 2017 Gjoa Haven
Toward a Sustainable Fishery for Nunavummiut (TSFN): 0402917N-M AMENDED Research Report 2017 Gjoa Haven HTA and Queen’s University (Supervisor: Virginia K. Walker; M. Sc. Students: Erin Hamilton and Geraint Element; Queen’s University, Department of Biology, Kingston, ON, K7L 3N6) Assessment of Water Microbial Communities and Microplastics in the Canadian Arctic’s Lower Northwest Passage (Kitikmeot Region) Section 1: Collection of Surface Water for Fish Microbiome Study Background Information Both fish slime on the scales as well as the intestines is made up of cells associated with the fish immune system as well as the microbiota or beneficial microorganisms. The microorganisms including symbiotic bacteria contribute to the health of the fish and by extension, the health of fish stocks. It is thought that the microbiomes contribute to fish well-being either through competing with harmful bacteria and therefore excluding them, or through a more complex interaction with the host immune defense response. From an academic view, it is important to characterize the microbiomes of fish to infer the functions these microbes serve to increase understanding of fish immunity, but from a practical view, knowledge of the fish microbiomes and of the waters they live in, will provide insight into the impact of climate change on fish populations that are an important food source to communities in the Northwest Passage. Accompanied by community members from Gjoa Haven, a research team sampled fish and water from fresh and saltwater sites around King William Island, Nunavut (with separate fish sampling permits and animal care permits for this aspect of the work; see application material).
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Canada's Arctic Marine Atlas
Lincoln Sea Hall Basin MARINE ATLAS ARCTIC CANADA’S GREENLAND Ellesmere Island Kane Basin Nares Strait N nd ansen Sou s d Axel n Sve Heiberg rdr a up Island l Ch ann North CANADA’S s el I Pea Water ry Ch a h nnel Massey t Sou Baﬃn e Amund nd ISR Boundary b Ringnes Bay Ellef Norwegian Coburg Island Grise Fiord a Ringnes Bay Island ARCTIC MARINE z Island EEZ Boundary Prince i Borden ARCTIC l Island Gustaf E Adolf Sea Maclea Jones n Str OCEAN n ait Sound ATLANTIC e Mackenzie Pe Ball nn antyn King Island y S e trait e S u trait it Devon Wel ATLAS Stra OCEAN Q Prince l Island Clyde River Queens in Bylot Patrick Hazen Byam gt Channel o Island Martin n Island Ch tr. Channel an Pond Inlet S Bathurst nel Qikiqtarjuaq liam A Island Eclipse ust Lancaster Sound in Cornwallis Sound Hecla Ch Fitzwil Island and an Griper nel ait Bay r Resolute t Melville Barrow Strait Arctic Bay S et P l Island r i Kel l n e c n e n Somerset Pangnirtung EEZ Boundary a R M'Clure Strait h Island e C g Baﬃn Island Brodeur y e r r n Peninsula t a P I Cumberland n Peel Sound l e Sound Viscount Stefansson t Melville Island Sound Prince Labrador of Wales Igloolik Prince Sea it Island Charles ra Hadley Bay Banks St s Island le a Island W Hall Beach f Beaufort o M'Clintock Gulf of Iqaluit e c n Frobisher Bay i Channel Resolution r Boothia Boothia Sea P Island Sachs Franklin Peninsula Committee Foxe Harbour Strait Bay Melville Peninsula Basin Kimmirut Taloyoak N UNAT Minto Inlet Victoria SIA VUT Makkovik Ulukhaktok Kugaaruk Foxe Island Hopedale Liverpool Amundsen Victoria King
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Expedition to the South Pole
Framheim, National Library of Norway. Roald Amundsen Expedition to the South Pole E&T P 29 Roald Amundsen -2- Expedition to the South Pole by Roald Amundsen -1- Lecture delivered in German by Roald Amundsen before the Berlin Geographical Society on October 9, 1912. Translated and reprinted from the Zeitschr. der Gesell. für Erdkunde zu Berlin, 1912, No.7, pp. 481-498. Reprinted in the Annual Report of the Board of Regents of The Smithsonian Institution, Washington D.C., 1912, by permission from the Bulletin of the American Geographical Society, vol. 44, No. 11, November, 1912, New York, pp. 822-838. This edition of 100 copies was issued by The Erebus & Terror Press, Jaffrey, New Hampshire, for those attending the SouthPole-sium v.3 Oslo, Norway 12-14 May 2017. Certain images and footnotes were not included. Printed at Savron Graphics Jaffrey, New Hampshire May 2017 ❦ -2- Expedition to the South Pole HE PLAN of the third Fram expedition was twofold: First, the attainment Tof the South Pole, and, second, the exploration of the north polar regions. This evening I have the honor to report to you on the accomplishment of the first part of this plan. I can only briefly mention here the expeditions which have worked in the region which we had selected for our starting point. As we wished to reach the South Pole, our first problem was to go south as far as possible with our ship and there establish our station. Even so, the sled journeys would be long enough. I knew that the English expedition would again choose their old winter quarters in McMurdo Sound, South Victoria Land, as their starting point.
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Synchronization of Ice Core Records Via Atmospheric Gases
Clim. Past, 3, 325–330, 2007 www.clim-past.net/3/325/2007/ Climate © Author(s) 2007. This work is licensed of the Past under a Creative Commons License. Synchronization of ice core records via atmospheric gases T. Blunier1, R. Spahni1, J.-M. Barnola2, J. Chappellaz2, L. Loulergue2, and J. Schwander1 1Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland 2Laboratoire de Glaciologie et Geophysique´ de l’Environnement (LGGE), CNRS-UJF, 54 rue Moliere,` BP96 38402 Saint Martin d’Heres Cedex, France Received: 12 January 2007 – Published in Clim. Past Discuss.: 15 February 2007 Revised: 14 May 2007 – Accepted: 1 June 2007 – Published: 18 June 2007 Abstract. To interpret new high resolution climate records it this synchronization point the time scales between Greenland becomes more and more important to know about the succes- and Antarctic ice cores diverge (Parrenin et al., 2007; Ruth sion of climate events. Such knowledge is hard to get espe- et al., 2007). The time scales can be linked via global gas cially when dealing with different types of climate archives. parameters. Here the complication is that the age of the gas Even for ice cores a direct synchronization between ice cores occluded in the ice is not identical to the age of the surround- from Greenland and Antarctica has not been possible so far ing ice. This age difference (1age) is a result of the gas due to the lack of time markers occurring in both hemi- being occluded not on top of the ice sheet but in a depth of spheres.
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Franklin's Lost Ship: the Historic Discover of H.M.S. Erebus, by John Geiger and Alanna Mitchell
108 • REVIEWS FRANKLIN’S LOST SHIP: THE HISTORIC Otter, Harris and his dive team were able to make further DISCOVERY OF H.M.S. EREBUS. By JOHN GEIGER and dives on the wreck via a hole cut in the ice. They were able ALANNA MITCHELL. Toronto: HarperCollins Publishers to take a further series of spectacular photos of the wreck Ltd. ISBN 978-1-44344-417-0. 201 p., maps, b&w and to raise one of the ship’s brass six-pounder cannons. and colour illus., endnotes, bibliography. Hardbound. Geiger and Mitchell describe the exciting events of the Cdn$39.99. 2014 expedition in considerable detail, and their text is accompanied by spectacular photos of the wreck and of On 19 May 1845, HMS Erebus and Terror sailed from the Arctic landscape. Having no expertise in the techni- London under the command of Sir John Franklin, with the cal aspects of the underwater search, this reviewer has to aim of completing the first transit of the Northwest Passage assume that the descriptions of the search are accurate. The from the Atlantic Ocean to the Pacific. On 17 September various stages of the search and the dives are covered in 2014, underwater archeologists Ryan Harris and Jonathan chapters that alternate with chapters on the history of Sir Moore of Parks Canada dived on the wreck of HMS Ere- John Franklin, his final voyage, and the extensive searches bus, to find it sitting almost upright and surprisingly intact that were subsequently mounted for the missing ships. in only 11 m of water in Queen Maud Gulf, in the general Unfortunately these chapters are strewn with errors, which area where Inuit traditional accounts maintain that the ship greatly lower the value of the book as a historical source.
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Norway Wants Explorer Ship Back 80 Years After Sinking 22 August 2011, by Michel Viatteau and Michel Comte
Norway wants explorer ship back 80 years after sinking 22 August 2011, by Michel Viatteau and Michel Comte Eighty years after it sank in the Canadian Arctic, International Polar Heritage Committee president explorer Roald Amundsen's three-mast ship Maud Susan Barr. may once again sail across the Atlantic to become the centerpiece of a new museum in Norway. "So I would not like to see the wreck removed." Canada, however, must still agree to the She also noted that the Maud expedition was not repatriation plan hatched by Norwegian investors, among Amundsen's most glorious and that two amid strong opposition from locals in the Canadian vessels from his more prestigious voyages -- the territory of Nunavut who want the ship to stay for Gjoa and Fram --- are preserved at a museum in tourists to admire from shore. Oslo. The wreck now sits at the bottom of Cambridge Amundsen was the first European explorer to sail Bay in Nunavut, but its hulk is partly visible above through the Northwest Passage in search of a new the frigid waters that preserved it for decades. shorter shipping route from Europe to Asia in 1906, and to the South Pole in 1911. "The incredibly strong-built oak ship has been helped by the Arctic cold and clean water to be -- Bring Maud home -- kept in a reasonably good shape," said Jan Wanggaard, a Norwegian who recently visited the He again sailed through the Northeast Passage wreck to sort out technical problems with raising with the Maud in 1918-20 without getting far the ship as well as to survey the views from locals enough north to start the drift from east to west and and officials.
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IGS Nordic Branch Meeting 2020
IGS Nordic Branch Meeting 2020 All times are in CET. Wednesday 11th November 11:00 – 11:15 Welcome and introduction 11:15 – 11:30 Meet and Greet 11:30 – 12:15 Open Topics in Glaciology, conveners: TBA 11:30 – 11:45 Thorstein Thorsteinsson: A sudden jökulhlaup from the newly formed marginal lake at Langjökull, W-Iceland 11:45 – 12:00 MC Sanjana: Ocean Sound Field Components in Kongsfjorden, Svalbard and its distribution 12:00 – 12:15 Suchithra Sundaram: Spring Arctic sea ice variability and its impact on Indian summer monsoon 12:30 – 13:15 Lunch 13:15 – 14:15 Subglacial 1, conveners: TBA 13:15 - 13:30 Rebecca Schlegel: Rapid erosion of a subglacial landform under the Rutford Ice Stream, West Antarctica 13:30 – 13:45 Eyjolfur Magnússon: The bedrock and tephra layer topography within the glacier filled Katla caldera, Iceland, deduced from dense RES-survey 13:45 – 14:00 Andreas Alexander: Subglacial permafrost dynamics and erosion inside subglacial channels driven by surface events in Svalbard 14:00 – 14:15 Nathan Maier: Constraining the relationship between velocity and basal traction over the grounded regions of Greenland 14:15 – 14:45 Coffee break 14:45 – 16:00 Poster session, conveners: TBA 14:45 – 15:15 3 minute poster presentations in the following order: Shridhar Jawak, Ward van Pelt, Kamilla H. Sjursen, Anne M. Solgaard, Brian Whalley, Mai Winstrup , Øyvind Winton, Levan Tielidze. 15:15 – 16:00 Poster room 1: Levan Tielidze: Reconstruction of Late Quaternary glaciation in the Ahuriri River valley, New Zealand, based on geomorphological mapping and cosmogenic 10Be data Brian Whalley: Glaciers in the Critical zone: A proposal for an earth science observatory, Lyngen North Norway 15:15 – 16:00 Poster room 2: Anne M.
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