SwePub
Sök i LIBRIS databas

  Utökad sökning

WFRF:(Vasilenko Evgeny)
 

Sökning: WFRF:(Vasilenko Evgeny) > The Ice-Free Topogr...

LIBRIS Formathandbok  (Information om MARC21)
FältnamnIndikatorerMetadata
00006421naa a2200577 4500
001oai:DiVA.org:uu-372714
003SwePub
008190108s2018 | |||||||||||000 ||eng|
024a https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-3727142 URI
024a https://doi.org/10.1029/2018GL0797342 DOI
040 a (SwePub)uu
041 a engb eng
042 9 SwePub
072 7a ref2 swepub-contenttype
072 7a art2 swepub-publicationtype
100a Fuerst, Johannes J.u Univ Erlangen Nurnberg, Inst Geog, Erlangen, Germany4 aut
2451 0a The Ice-Free Topography of Svalbard
264 1c 2018
338 a print2 rdacarrier
520 a We present a first version of the Svalbard ice-free topography (SVIFT1.0) using a mass conserving approach for mapping glacier ice thickness. SVIFT1.0 is informed by more than 1 million point measurements, totalling more than 8,700 km of thickness profiles. SVIFT1.0 is publicly available and represents the geometric state around the year 2010. Our estimate for the total ice volume is 6,199 km(3), equivalent to 1.5-cm sea level rise. The thickness map suggests that 13% of the glacierized area is grounded below sea level. A complementary map of error estimates comprises uncertainties in the thickness surveys as well as in other input variables. Aggregated error estimates are used to define a likely ice-volume range of 5,200-7,300 km(3). The ice front thickness of marine-terminating glaciers is a key quantity for ice loss attribution because it controls the potential ice discharge by iceberg calving into the ocean. We find a mean ice front thickness of 135 m for the archipelago (likely range 123-158 m). Plain Language Summary Svalbard is an archipelago in the Arctic, north of Norway, which is comparable in size to the New York metropolitan area. Roughly half of it is covered by glacier ice. Yet to this day, the ice volume stored in the many glaciers on Svalbard is not well known. Many attempts have been made to infer a total volume estimate, but results differ substantially. This surprises because of the long research activity in this area. A large record of more than 1 million thickness measurements exists, making Svalbard an ideal study area for the application of a state-of-the-art mapping approach for glacier ice thickness. The mapping approach computes an ice volume that will raise global sea level by more than half an inch if instantaneously melted. If spread over the metropolitan area, New York would be buried beneath a 100-m ice cover. The asset of this approach is that it provides not only a thickness map for each glacier on the archipelago but also an error map that defines the likely local thickness range. Finally, we provide the first well-informed estimate of the ice front thickness of all marine-terminating glaciers that loose icebergs to the ocean. The archipelago-wide mean ice front cliff is 135 m.
650 7a NATURVETENSKAPx Geovetenskap och miljövetenskapx Naturgeografi0 (SwePub)105072 hsv//swe
650 7a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Physical Geography0 (SwePub)105072 hsv//eng
700a Navarro, Franciscou Univ Politecn Madrid, Dept Matemat Aplicada Tecnol Informac & Comunicac, ETSI Telecomunicac, Madrid, Spain4 aut
700a Gillet-Chaulet, Fabienu Inst Geosci Environm, Grenoble, France;Univ Grenoble Alpes, CNRS, IRD, Grenoble INP,IGE, Grenoble, France4 aut
700a Huss, Matthiasu Univ Fribourg, Dept Geosci, Fribourg, Switzerland;Swiss Fed Inst Technol, Lab Hydraul Hydrol & Glaciol, Zurich, Switzerland4 aut
700a Moholdt, Geiru Norwegian Polar Res Inst, Fram Ctr, Tromso, Norway4 aut
700a Fettweis, Xavieru Univ Liege, Dept Geog, Liege, Belgium4 aut
700a Lang, Charlotteu Univ Liege, Dept Geog, Liege, Belgium4 aut
700a Seehaus, Thorstenu Univ Erlangen Nurnberg, Inst Geog, Erlangen, Germany4 aut
700a Ai, Songtaou Wuhan Univ, Chinese Antarctic Ctr Surveying & Mapping, Wuhan, Hubei, Peoples R China4 aut
700a Benham, Toby J.u Univ Cambridge, Scott Polar Res Inst, Cambridge, England4 aut
700a Benn, Douglas I.u Univ St Andrews, St Andrews Glaciol, Sch Geog & Sustainable Dev, St Andrews, Fife, Scotland4 aut
700a Bjornsson, Helgiu Univ Iceland, Inst Earth Sci, Reykjavik, Iceland4 aut
700a Dowdeswell, Julian A.u Univ Cambridge, Scott Polar Res Inst, Cambridge, England4 aut
700a Grabiec, Mariuszu Univ Silesia Katowice, Fac Earth Sci, Katowice, Poland4 aut
700a Kohler, Jacku Norwegian Polar Res Inst, Fram Ctr, Tromso, Norway4 aut
700a Lavrentiev, Ivanu Russian Acad Sci, Inst Geog, Moscow, Russia4 aut
700a Lindback, Katrinu Norwegian Polar Res Inst, Fram Ctr, Tromso, Norway4 aut
700a Melvold, Kjetilu Univ Erlangen Nurnberg, Inst Geog, Erlangen, Germany;Univ Fribourg, Dept Geosci, Fribourg, Switzerland;Norwegian Water Resources & Energy Directorate NV, Oslo, Norway4 aut
700a Pettersson, Rickardu Uppsala universitet,Luft-, vatten- och landskapslära4 aut0 (Swepub:uu)ricpe317
700a Rippin, Davidu Univ York, Dept Environm, York, N Yorkshire, England4 aut
700a Saintenoy, Albaneu Univ Paris Saclay, Univ Paris Sud, GEOPS, CNRS, Orsay, France4 aut
700a Sanchez-Gamez, Pablou Departamento de Matemática Aplicada a las Tecnologías de la Información y las Comunicaciones, ETSI de Telecomunicación, Universidad Politécnica de Madrid, , Madrid, Spain4 aut
700a Schuler, Thomas V.u Univ Oslo, Dept Geosci, Oslo, Norway;UNIS Univ Ctr Svalbard, Dept Arctic Geophys, Longyearbyen, Norway4 aut
700a Sevestre, Heidiu Univ St Andrews, St Andrews Glaciol, Sch Geog & Sustainable Dev, St Andrews, Fife, Scotland4 aut
700a Vasilenko, Evgenyu Acad Sci Uzbek, Inst Ind Res Akadempribor, Tashkent, Uzbekistan4 aut
700a Braun, Matthias H.u Univ Erlangen Nurnberg, Inst Geog, Erlangen, Germany4 aut
710a Univ Erlangen Nurnberg, Inst Geog, Erlangen, Germanyb Univ Politecn Madrid, Dept Matemat Aplicada Tecnol Informac & Comunicac, ETSI Telecomunicac, Madrid, Spain4 org
773t Geophysical Research Lettersg 45:21, s. 11760-11769q 45:21<11760-11769x 0094-8276x 1944-8007
8564 8u https://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-372714
8564 8u https://doi.org/10.1029/2018GL079734

Hitta via bibliotek

Till lärosätets databas

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Stäng

Kopiera och spara länken för att återkomma till aktuell vy