Amphibian Seismological Studies in the Ross Sea, Antarctica

The Antarctic Ross Sea is one of the key regions for polar research activities. Research stations from several countries located at the coast are the base for inland expeditions. Even in the southern austral summer, the Ross Sea is party covered with drifting ice fields; this requires an icebreaker...

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Main Authors: Schmidt-Aursch, Mechita, Hong, Jong Kuk, Lee, Won Sang, Geissler, Wolfram, Sukyoung, Yun, Gohl, Karsten, Park, Yongcheol, Yoo, Hyun Jae
Format: Conference Object
Language:unknown
Published: 2016
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Online Access:https://epic.awi.de/id/eprint/39446/
https://hdl.handle.net/10013/epic.47502
id ftawi:oai:epic.awi.de:39446
record_format openpolar
spelling ftawi:oai:epic.awi.de:39446 2024-09-15T17:47:04+00:00 Amphibian Seismological Studies in the Ross Sea, Antarctica Schmidt-Aursch, Mechita Hong, Jong Kuk Lee, Won Sang Geissler, Wolfram Sukyoung, Yun Gohl, Karsten Park, Yongcheol Yoo, Hyun Jae 2016-04 https://epic.awi.de/id/eprint/39446/ https://hdl.handle.net/10013/epic.47502 unknown Schmidt-Aursch, M. orcid:0000-0002-2393-4514 , Hong, J. K. , Lee, W. S. , Geissler, W. orcid:0000-0001-6807-555X , Sukyoung, Y. , Gohl, K. orcid:0000-0002-9558-2116 , Park, Y. and Yoo, H. J. (2016) Amphibian Seismological Studies in the Ross Sea, Antarctica , European Geosciences Union General Assembly 2016, Vienna, Austria, 17 April 2016 - 22 April 2016 . hdl:10013/epic.47502 EPIC3European Geosciences Union General Assembly 2016, Vienna, Austria, 2016-04-17-2016-04-22 Conference notRev 2016 ftawi 2024-06-24T04:13:16Z The Antarctic Ross Sea is one of the key regions for polar research activities. Research stations from several countries located at the coast are the base for inland expeditions. Even in the southern austral summer, the Ross Sea is party covered with drifting ice fields; this requires an icebreaker for all marine explorations. Therefore, large geophysical surveys in the Ross Sea are difficult. But the area is of special interest for seismologists: The Terror Rift in the western Ross Sea is a prominent neotectonic structure of the West Antarctic Rift System (WARS). It is located near the coast in the Victoria Land Basin and extends parallel to the Transantarctic Mountains. The rifting processes and the accompanying active onshore volcanism lead to increased seismicity in the region. The annual waxing and waning of the sea-ice and the dynamics of the large Ross Ice Shelf and nearby glaciers generate additional seismic signals. Investigation on seismological activities associated with the WARS and the cryogenic signals simultaneously would give us an unprecedented opportunity to have a better understanding of the Evolution of the WARS (EWARS) and the rapid change in the cryospheric environment nearby. The Korean Polar Research Institute (KOPRI) and the Alfred-Wegener-Institut (AWI) have conducted a pilot study off the Korean Jang Bogo research station in the Terra Nova Bay by developing a collaborative research program (EWARS) since 2011 to explore seismicity and seismic noise in this region. Four broadband ocean-bottom seismometers (OBS) from the German DEPAS pool were deployed in January 2012 with the Korean research icebreaker RV Araon. Three instruments could successfully be recovered after 13 months, the fourth OBS was not accessible due to local sea-ice coverage. We have successfully completed a second recovery operation It was retrieved one year late in January 2014. All stations recorded data of good quality, one station stopped after 8 months due to a recorder error. The OBS recovered in 2014 recorded more ... Conference Object Antarc* Antarctic Antarctica Ice Shelf Ross Ice Shelf Ross Sea Sea ice Victoria Land Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
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 The Antarctic Ross Sea is one of the key regions for polar research activities. Research stations from several countries located at the coast are the base for inland expeditions. Even in the southern austral summer, the Ross Sea is party covered with drifting ice fields; this requires an icebreaker for all marine explorations. Therefore, large geophysical surveys in the Ross Sea are difficult. But the area is of special interest for seismologists: The Terror Rift in the western Ross Sea is a prominent neotectonic structure of the West Antarctic Rift System (WARS). It is located near the coast in the Victoria Land Basin and extends parallel to the Transantarctic Mountains. The rifting processes and the accompanying active onshore volcanism lead to increased seismicity in the region. The annual waxing and waning of the sea-ice and the dynamics of the large Ross Ice Shelf and nearby glaciers generate additional seismic signals. Investigation on seismological activities associated with the WARS and the cryogenic signals simultaneously would give us an unprecedented opportunity to have a better understanding of the Evolution of the WARS (EWARS) and the rapid change in the cryospheric environment nearby. The Korean Polar Research Institute (KOPRI) and the Alfred-Wegener-Institut (AWI) have conducted a pilot study off the Korean Jang Bogo research station in the Terra Nova Bay by developing a collaborative research program (EWARS) since 2011 to explore seismicity and seismic noise in this region. Four broadband ocean-bottom seismometers (OBS) from the German DEPAS pool were deployed in January 2012 with the Korean research icebreaker RV Araon. Three instruments could successfully be recovered after 13 months, the fourth OBS was not accessible due to local sea-ice coverage. We have successfully completed a second recovery operation It was retrieved one year late in January 2014. All stations recorded data of good quality, one station stopped after 8 months due to a recorder error. The OBS recovered in 2014 recorded more ...
format Conference Object
author Schmidt-Aursch, Mechita
Hong, Jong Kuk
Lee, Won Sang
Geissler, Wolfram
Sukyoung, Yun
Gohl, Karsten
Park, Yongcheol
Yoo, Hyun Jae
spellingShingle Schmidt-Aursch, Mechita
Hong, Jong Kuk
Lee, Won Sang
Geissler, Wolfram
Sukyoung, Yun
Gohl, Karsten
Park, Yongcheol
Yoo, Hyun Jae
Amphibian Seismological Studies in the Ross Sea, Antarctica
author_facet Schmidt-Aursch, Mechita
Hong, Jong Kuk
Lee, Won Sang
Geissler, Wolfram
Sukyoung, Yun
Gohl, Karsten
Park, Yongcheol
Yoo, Hyun Jae
author_sort Schmidt-Aursch, Mechita
title Amphibian Seismological Studies in the Ross Sea, Antarctica
title_short Amphibian Seismological Studies in the Ross Sea, Antarctica
title_full Amphibian Seismological Studies in the Ross Sea, Antarctica
title_fullStr Amphibian Seismological Studies in the Ross Sea, Antarctica
title_full_unstemmed Amphibian Seismological Studies in the Ross Sea, Antarctica
title_sort amphibian seismological studies in the ross sea, antarctica
publishDate 2016
url https://epic.awi.de/id/eprint/39446/
https://hdl.handle.net/10013/epic.47502
genre Antarc*
Antarctic
Antarctica
Ice Shelf
Ross Ice Shelf
Ross Sea
Sea ice
Victoria Land
genre_facet Antarc*
Antarctic
Antarctica
Ice Shelf
Ross Ice Shelf
Ross Sea
Sea ice
Victoria Land
op_source EPIC3European Geosciences Union General Assembly 2016, Vienna, Austria, 2016-04-17-2016-04-22
op_relation Schmidt-Aursch, M. orcid:0000-0002-2393-4514 , Hong, J. K. , Lee, W. S. , Geissler, W. orcid:0000-0001-6807-555X , Sukyoung, Y. , Gohl, K. orcid:0000-0002-9558-2116 , Park, Y. and Yoo, H. J. (2016) Amphibian Seismological Studies in the Ross Sea, Antarctica , European Geosciences Union General Assembly 2016, Vienna, Austria, 17 April 2016 - 22 April 2016 . hdl:10013/epic.47502
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