Annual Rep ort of RADARC, 2002

The spatial and temporal distributions of the anthropogenic radionuclides 137Cs and 90Sr, originating from nuclear bomb testing, the Sellafield reprocessing plants in the Irish Sea, the Ob and Yenisey river discharges, are simulated using a global version of the Miami Isopycnic Co-ordinate Ocean Mod...

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Main Authors: Gao, Yongqi, Drange, Helge, Johannessen, Ola M., Petersson, Lasse H.
Format: Report
Language:English
Published: 2003
Subjects:
Online Access:https://zenodo.org/record/7609792
https://doi.org/10.5281/zenodo.7609792
id ftzenodo:oai:zenodo.org:7609792
record_format openpolar
spelling ftzenodo:oai:zenodo.org:7609792 2023-05-15T14:54:52+02:00 Annual Rep ort of RADARC, 2002 Gao, Yongqi Drange, Helge Johannessen, Ola M. Petersson, Lasse H. 2003-03-03 https://zenodo.org/record/7609792 https://doi.org/10.5281/zenodo.7609792 eng eng doi:10.5281/zenodo.7609791 https://zenodo.org/communities/nersc-research https://zenodo.org/record/7609792 https://doi.org/10.5281/zenodo.7609792 oai:zenodo.org:7609792 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode Radionuclides Contamination Ocean Norwegian Sea Kara Sea Dispersion Model MICOM info:eu-repo/semantics/report publication-report 2003 ftzenodo https://doi.org/10.5281/zenodo.760979210.5281/zenodo.7609791 2023-03-11T01:04:01Z The spatial and temporal distributions of the anthropogenic radionuclides 137Cs and 90Sr, originating from nuclear bomb testing, the Sellafield reprocessing plants in the Irish Sea, the Ob and Yenisey river discharges, are simulated using a global version of the Miami Isopycnic Co-ordinate Ocean Model (MICOM). The physical model is forced with daily atmospheric re-analyses fields for the period 1950 to present. It is shown that the radionuclides from the Sellafield discharge reach the Barents Sea region after 4-5 years, in accordance with observations. The simulation provides a detailed distribution and evolution of the radionuclides over the integration time. For the Atlantic waters o the coast of Norway and in the southern Barents Sea, the atmospheric fallout dominates over of Sellafield release up to the mid 1960s and from the early 1990s, whereas Sellafield is the main source for the two radionuclides in the 1970s and 1980s. The Ob river discharge dominate the surface 90Sr over most of the Arctic Ocean and along the eastern and western coasts of the Greenland before 1960. During the period of 1980 to 1990, the atmospheric fallout and the Ob river discharge are equally important in the 90Sr distribution over the Arctic Ocean. It is furthermore argued that model systems like the one presented here can be used for future prediction of radioactive contamination in the Nordic Seas and the Arctic Ocean, for instance under various global warming scenarios NERSC Technical report no. 235. Funded by the European Union under Contract no. ICA2-CT-2000-10037 Report Arctic Arctic Ocean Barents Sea Global warming Greenland Kara Sea Nordic Seas Norwegian Sea ob river yenisey river Zenodo Arctic Arctic Ocean Barents Sea Norwegian Sea Kara Sea Greenland Norway Yenisey ENVELOPE(82.680,82.680,71.828,71.828)
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic Radionuclides
Contamination
Ocean
Norwegian Sea
Kara Sea
Dispersion
Model
MICOM
spellingShingle Radionuclides
Contamination
Ocean
Norwegian Sea
Kara Sea
Dispersion
Model
MICOM
Gao, Yongqi
Drange, Helge
Johannessen, Ola M.
Petersson, Lasse H.
Annual Rep ort of RADARC, 2002
topic_facet Radionuclides
Contamination
Ocean
Norwegian Sea
Kara Sea
Dispersion
Model
MICOM
description The spatial and temporal distributions of the anthropogenic radionuclides 137Cs and 90Sr, originating from nuclear bomb testing, the Sellafield reprocessing plants in the Irish Sea, the Ob and Yenisey river discharges, are simulated using a global version of the Miami Isopycnic Co-ordinate Ocean Model (MICOM). The physical model is forced with daily atmospheric re-analyses fields for the period 1950 to present. It is shown that the radionuclides from the Sellafield discharge reach the Barents Sea region after 4-5 years, in accordance with observations. The simulation provides a detailed distribution and evolution of the radionuclides over the integration time. For the Atlantic waters o the coast of Norway and in the southern Barents Sea, the atmospheric fallout dominates over of Sellafield release up to the mid 1960s and from the early 1990s, whereas Sellafield is the main source for the two radionuclides in the 1970s and 1980s. The Ob river discharge dominate the surface 90Sr over most of the Arctic Ocean and along the eastern and western coasts of the Greenland before 1960. During the period of 1980 to 1990, the atmospheric fallout and the Ob river discharge are equally important in the 90Sr distribution over the Arctic Ocean. It is furthermore argued that model systems like the one presented here can be used for future prediction of radioactive contamination in the Nordic Seas and the Arctic Ocean, for instance under various global warming scenarios NERSC Technical report no. 235. Funded by the European Union under Contract no. ICA2-CT-2000-10037
format Report
author Gao, Yongqi
Drange, Helge
Johannessen, Ola M.
Petersson, Lasse H.
author_facet Gao, Yongqi
Drange, Helge
Johannessen, Ola M.
Petersson, Lasse H.
author_sort Gao, Yongqi
title Annual Rep ort of RADARC, 2002
title_short Annual Rep ort of RADARC, 2002
title_full Annual Rep ort of RADARC, 2002
title_fullStr Annual Rep ort of RADARC, 2002
title_full_unstemmed Annual Rep ort of RADARC, 2002
title_sort annual rep ort of radarc, 2002
publishDate 2003
url https://zenodo.org/record/7609792
https://doi.org/10.5281/zenodo.7609792
long_lat ENVELOPE(82.680,82.680,71.828,71.828)
geographic Arctic
Arctic Ocean
Barents Sea
Norwegian Sea
Kara Sea
Greenland
Norway
Yenisey
geographic_facet Arctic
Arctic Ocean
Barents Sea
Norwegian Sea
Kara Sea
Greenland
Norway
Yenisey
genre Arctic
Arctic Ocean
Barents Sea
Global warming
Greenland
Kara Sea
Nordic Seas
Norwegian Sea
ob river
yenisey river
genre_facet Arctic
Arctic Ocean
Barents Sea
Global warming
Greenland
Kara Sea
Nordic Seas
Norwegian Sea
ob river
yenisey river
op_relation doi:10.5281/zenodo.7609791
https://zenodo.org/communities/nersc-research
https://zenodo.org/record/7609792
https://doi.org/10.5281/zenodo.7609792
oai:zenodo.org:7609792
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.760979210.5281/zenodo.7609791
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