34 year satellite time series to monitor characteristics, extent and dynamics of Larsen B, Antarctic Peninsula

A variety of data are used to investigate Larsen B, which is at present the northernmost section of the Larsen Ice Shelf. Recently declassified USArgon satellite photographs of 1963, Kosmos photographs of 1975, Landsat images of 1986, 1988 and 1990, ERS-1/2 SAR images from 1992 to1997, Radarsat of 1...

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Main Authors: Skvarca, P., Rack, W., Rott, H.
Format: Article in Journal/Newspaper
Language:unknown
Published: 1999
Subjects:
Online Access:https://epic.awi.de/id/eprint/6000/
https://hdl.handle.net/10013/epic.16554
id ftawi:oai:epic.awi.de:6000
record_format openpolar
spelling ftawi:oai:epic.awi.de:6000 2023-09-05T13:15:19+02:00 34 year satellite time series to monitor characteristics, extent and dynamics of Larsen B, Antarctic Peninsula Skvarca, P. Rack, W. Rott, H. 1999 https://epic.awi.de/id/eprint/6000/ https://hdl.handle.net/10013/epic.16554 unknown Skvarca, P. , Rack, W. and Rott, H. (1999) 34 year satellite time series to monitor characteristics, extent and dynamics of Larsen B, Antarctic Peninsula , 29 , pp. 255-260 . hdl:10013/epic.16554 EPIC329, pp. 255-260 Article peerRev 1999 ftawi 2023-08-22T19:45:49Z A variety of data are used to investigate Larsen B, which is at present the northernmost section of the Larsen Ice Shelf. Recently declassified USArgon satellite photographs of 1963, Kosmos photographs of 1975, Landsat images of 1986, 1988 and 1990, ERS-1/2 SAR images from 1992 to1997, Radarsat of 1998 and field surveys are used to analyze the areal extent, surface characteristics and dynamic behaviour of this ice shelf sectionover more than three decades. Visible and radar imagery together with field observations are used synergistically to describe the ice shelf morphology,including meltwater features and rifts. In contrast to the retreat of the ice shelf sections in the north, Larsen B advanced steadily from 1963 to early1995 when the area decreased significantly due to a major calving event. Analysis of different satellite images indicates that melting is proceedingfurther south in coincidence with the regional warming trend. In addition, fracturing processes and rapid development of new rifts are observed,associated with recent acceleration of ice motion close to the front. All observations indicate that major calving events should be expected for this iceshelf section in the near future. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Ice Shelf Larsen Ice Shelf Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Antarctic Antarctic Peninsula Larsen Ice Shelf ENVELOPE(-62.500,-62.500,-67.500,-67.500)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description A variety of data are used to investigate Larsen B, which is at present the northernmost section of the Larsen Ice Shelf. Recently declassified USArgon satellite photographs of 1963, Kosmos photographs of 1975, Landsat images of 1986, 1988 and 1990, ERS-1/2 SAR images from 1992 to1997, Radarsat of 1998 and field surveys are used to analyze the areal extent, surface characteristics and dynamic behaviour of this ice shelf sectionover more than three decades. Visible and radar imagery together with field observations are used synergistically to describe the ice shelf morphology,including meltwater features and rifts. In contrast to the retreat of the ice shelf sections in the north, Larsen B advanced steadily from 1963 to early1995 when the area decreased significantly due to a major calving event. Analysis of different satellite images indicates that melting is proceedingfurther south in coincidence with the regional warming trend. In addition, fracturing processes and rapid development of new rifts are observed,associated with recent acceleration of ice motion close to the front. All observations indicate that major calving events should be expected for this iceshelf section in the near future.
format Article in Journal/Newspaper
author Skvarca, P.
Rack, W.
Rott, H.
spellingShingle Skvarca, P.
Rack, W.
Rott, H.
34 year satellite time series to monitor characteristics, extent and dynamics of Larsen B, Antarctic Peninsula
author_facet Skvarca, P.
Rack, W.
Rott, H.
author_sort Skvarca, P.
title 34 year satellite time series to monitor characteristics, extent and dynamics of Larsen B, Antarctic Peninsula
title_short 34 year satellite time series to monitor characteristics, extent and dynamics of Larsen B, Antarctic Peninsula
title_full 34 year satellite time series to monitor characteristics, extent and dynamics of Larsen B, Antarctic Peninsula
title_fullStr 34 year satellite time series to monitor characteristics, extent and dynamics of Larsen B, Antarctic Peninsula
title_full_unstemmed 34 year satellite time series to monitor characteristics, extent and dynamics of Larsen B, Antarctic Peninsula
title_sort 34 year satellite time series to monitor characteristics, extent and dynamics of larsen b, antarctic peninsula
publishDate 1999
url https://epic.awi.de/id/eprint/6000/
https://hdl.handle.net/10013/epic.16554
long_lat ENVELOPE(-62.500,-62.500,-67.500,-67.500)
geographic Antarctic
Antarctic Peninsula
Larsen Ice Shelf
geographic_facet Antarctic
Antarctic Peninsula
Larsen Ice Shelf
genre Antarc*
Antarctic
Antarctic Peninsula
Ice Shelf
Larsen Ice Shelf
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Ice Shelf
Larsen Ice Shelf
op_source EPIC329, pp. 255-260
op_relation Skvarca, P. , Rack, W. and Rott, H. (1999) 34 year satellite time series to monitor characteristics, extent and dynamics of Larsen B, Antarctic Peninsula , 29 , pp. 255-260 . hdl:10013/epic.16554
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