Physical and chemical oceanography in the Arctic Ocean
Data from sections across the Eurasian Basin of the Arctic Ocean occupied by the German Research Vessel Polarstern in 1987 and by the Swedish icebreaker Oden in 1991 are used to derive information on the freshwater balance of the Arctic Ocean halocline and on the sources of the deep waters of the Na...
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Format: | Other/Unknown Material |
Language: | English |
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PANGAEA
1995
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.761145 https://doi.org/10.1594/PANGAEA.761145 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.761145 |
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openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
91004 91008 Arctic Ocean ARK-IV/2 ARK-IV/3 AWI_Paleo Chejsa Island CTD/Rosette CTD-RO Dalniye Zelentsy DZ-68 DZ-68_1 DZ-68_10 DZ-68_11 DZ-68_12 DZ-68_13 DZ-68_14 DZ-68_15 DZ-68_16 DZ-68_2 DZ-68_3 DZ-68_5 DZ-68_8 DZ-68_9 E.S.A.R.E.92 ESARE92/14 ESARE92/17 ESARE92/2 ESARE92/3 ESARE92/4 ESARE92/5 ESARE92/6 ESARE92/7 ESARE92/8 Green Bell Island Greenland Sea M71 M71_79 M8/1 M8/1_617 Meteor (1964) Meteor (1986) MULT Multiple investigations Nordenskiöld Bay North Greenland Sea OD91 OD91_004 OD91_008 OD91_009-1 |
spellingShingle |
91004 91008 Arctic Ocean ARK-IV/2 ARK-IV/3 AWI_Paleo Chejsa Island CTD/Rosette CTD-RO Dalniye Zelentsy DZ-68 DZ-68_1 DZ-68_10 DZ-68_11 DZ-68_12 DZ-68_13 DZ-68_14 DZ-68_15 DZ-68_16 DZ-68_2 DZ-68_3 DZ-68_5 DZ-68_8 DZ-68_9 E.S.A.R.E.92 ESARE92/14 ESARE92/17 ESARE92/2 ESARE92/3 ESARE92/4 ESARE92/5 ESARE92/6 ESARE92/7 ESARE92/8 Green Bell Island Greenland Sea M71 M71_79 M8/1 M8/1_617 Meteor (1964) Meteor (1986) MULT Multiple investigations Nordenskiöld Bay North Greenland Sea OD91 OD91_004 OD91_008 OD91_009-1 Bauch, Dorothea Physical and chemical oceanography in the Arctic Ocean |
topic_facet |
91004 91008 Arctic Ocean ARK-IV/2 ARK-IV/3 AWI_Paleo Chejsa Island CTD/Rosette CTD-RO Dalniye Zelentsy DZ-68 DZ-68_1 DZ-68_10 DZ-68_11 DZ-68_12 DZ-68_13 DZ-68_14 DZ-68_15 DZ-68_16 DZ-68_2 DZ-68_3 DZ-68_5 DZ-68_8 DZ-68_9 E.S.A.R.E.92 ESARE92/14 ESARE92/17 ESARE92/2 ESARE92/3 ESARE92/4 ESARE92/5 ESARE92/6 ESARE92/7 ESARE92/8 Green Bell Island Greenland Sea M71 M71_79 M8/1 M8/1_617 Meteor (1964) Meteor (1986) MULT Multiple investigations Nordenskiöld Bay North Greenland Sea OD91 OD91_004 OD91_008 OD91_009-1 |
description |
Data from sections across the Eurasian Basin of the Arctic Ocean occupied by the German Research Vessel Polarstern in 1987 and by the Swedish icebreaker Oden in 1991 are used to derive information on the freshwater balance of the Arctic Ocean halocline and on the sources of the deep waters of the Nansen, Amundsen and Makarov basins. Salinity, d18O and mass balances allow separation of the river-runoff and the sea-ice meltwater fractions contained in the Arctic halocline. This provides the basis for tracking the river-runoff signal from the shelf seas across the central Arctic Ocean to Fram Strait. The halocline has to be divided into at least three lateral regimes: the southern Nansen Basin with net sea-ice melting, the northern Nansen Basin and Amundsen Basin with net sea-ice formation and increasing river-runoff fractions, and the Canadian Basin with minimum sea-ice meltwater and maximum river-runoff fractions and water of Pacific origin. In the Canadian Basin, silicate is used as a tracer to identify Pacific water entering through Bering Strait and an attempt is made to quantify its influence on the halocline waters of the Canadian Basin. For this purpose literature data from the CESAR and LOREX ice camps are used. Based on mass balances and depending on the value of precipitation over the area of the Arctic Ocean the average mean residence time of the river-runoff fraction contained in the Arctic Ocean halocline is determined to be about 14 or 11 years. Water column inventories of river-runoff and sea-ice meltwater are calculated for a section just north of Fram Strait and implications for the ice export rate through Fram Strait are discussed. Salinity, tritium, 3He and the d18O ratio of halocline waters sampled during the 1987 Polarstern cruise to the Nansen Basin are used to estimate the mean residence time of the river-runoff component in the halocline and on the shelves of the Arctic Ocean. These estimates are done by comparing ages of the halocline waters based on a combination of tracers yielding ... |
format |
Other/Unknown Material |
author |
Bauch, Dorothea |
author_facet |
Bauch, Dorothea |
author_sort |
Bauch, Dorothea |
title |
Physical and chemical oceanography in the Arctic Ocean |
title_short |
Physical and chemical oceanography in the Arctic Ocean |
title_full |
Physical and chemical oceanography in the Arctic Ocean |
title_fullStr |
Physical and chemical oceanography in the Arctic Ocean |
title_full_unstemmed |
Physical and chemical oceanography in the Arctic Ocean |
title_sort |
physical and chemical oceanography in the arctic ocean |
publisher |
PANGAEA |
publishDate |
1995 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.761145 https://doi.org/10.1594/PANGAEA.761145 |
op_coverage |
MEDIAN LATITUDE: 76.797570 * MEDIAN LONGITUDE: 38.498935 * SOUTH-BOUND LATITUDE: 70.000000 * WEST-BOUND LONGITUDE: -17.520000 * NORTH-BOUND LATITUDE: 88.276700 * EAST-BOUND LONGITUDE: 163.603300 * DATE/TIME START: 1987-06-10T18:41:00 * DATE/TIME END: 1992-01-01T00:00:00 |
long_lat |
ENVELOPE(-17.520000,163.603300,88.276700,70.000000) |
genre |
amundsen basin Arctic Arctic Ocean Bell Island Berichte zur Polarforschung Bering Strait Fram Strait Greenland Greenland Sea Nansen Basin North Greenland oden Polar Research Polarforschung Reports on polar research Sea ice |
genre_facet |
amundsen basin Arctic Arctic Ocean Bell Island Berichte zur Polarforschung Bering Strait Fram Strait Greenland Greenland Sea Nansen Basin North Greenland oden Polar Research Polarforschung Reports on polar research Sea ice |
op_source |
Supplement to: Bauch, Dorothea (1995): The distribution of d18O in the Arctic Ocean: implications for the freshwater balance of the halocline and the sources of deep and bottom waters (Die Verteilung von d18O im Arktischen Ozean: Implikationen für die Süßwasserbilanz der Halokline und die Quellen des Tiefen- und Bodenwassers). Berichte zur Polarforschung = Reports on Polar Research, 159, 144 pp, https://doi.org/10.2312/BzP_0159_1995 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.761145 https://doi.org/10.1594/PANGAEA.761145 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.76114510.2312/BzP_0159_1995 |
_version_ |
1810475825510744064 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.761145 2024-09-15T17:38:52+00:00 Physical and chemical oceanography in the Arctic Ocean Bauch, Dorothea MEDIAN LATITUDE: 76.797570 * MEDIAN LONGITUDE: 38.498935 * SOUTH-BOUND LATITUDE: 70.000000 * WEST-BOUND LONGITUDE: -17.520000 * NORTH-BOUND LATITUDE: 88.276700 * EAST-BOUND LONGITUDE: 163.603300 * DATE/TIME START: 1987-06-10T18:41:00 * DATE/TIME END: 1992-01-01T00:00:00 1995 application/zip, 6 datasets https://doi.pangaea.de/10.1594/PANGAEA.761145 https://doi.org/10.1594/PANGAEA.761145 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.761145 https://doi.org/10.1594/PANGAEA.761145 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Bauch, Dorothea (1995): The distribution of d18O in the Arctic Ocean: implications for the freshwater balance of the halocline and the sources of deep and bottom waters (Die Verteilung von d18O im Arktischen Ozean: Implikationen für die Süßwasserbilanz der Halokline und die Quellen des Tiefen- und Bodenwassers). Berichte zur Polarforschung = Reports on Polar Research, 159, 144 pp, https://doi.org/10.2312/BzP_0159_1995 91004 91008 Arctic Ocean ARK-IV/2 ARK-IV/3 AWI_Paleo Chejsa Island CTD/Rosette CTD-RO Dalniye Zelentsy DZ-68 DZ-68_1 DZ-68_10 DZ-68_11 DZ-68_12 DZ-68_13 DZ-68_14 DZ-68_15 DZ-68_16 DZ-68_2 DZ-68_3 DZ-68_5 DZ-68_8 DZ-68_9 E.S.A.R.E.92 ESARE92/14 ESARE92/17 ESARE92/2 ESARE92/3 ESARE92/4 ESARE92/5 ESARE92/6 ESARE92/7 ESARE92/8 Green Bell Island Greenland Sea M71 M71_79 M8/1 M8/1_617 Meteor (1964) Meteor (1986) MULT Multiple investigations Nordenskiöld Bay North Greenland Sea OD91 OD91_004 OD91_008 OD91_009-1 dataset publication series 1995 ftpangaea https://doi.org/10.1594/PANGAEA.76114510.2312/BzP_0159_1995 2024-07-24T02:31:20Z Data from sections across the Eurasian Basin of the Arctic Ocean occupied by the German Research Vessel Polarstern in 1987 and by the Swedish icebreaker Oden in 1991 are used to derive information on the freshwater balance of the Arctic Ocean halocline and on the sources of the deep waters of the Nansen, Amundsen and Makarov basins. Salinity, d18O and mass balances allow separation of the river-runoff and the sea-ice meltwater fractions contained in the Arctic halocline. This provides the basis for tracking the river-runoff signal from the shelf seas across the central Arctic Ocean to Fram Strait. The halocline has to be divided into at least three lateral regimes: the southern Nansen Basin with net sea-ice melting, the northern Nansen Basin and Amundsen Basin with net sea-ice formation and increasing river-runoff fractions, and the Canadian Basin with minimum sea-ice meltwater and maximum river-runoff fractions and water of Pacific origin. In the Canadian Basin, silicate is used as a tracer to identify Pacific water entering through Bering Strait and an attempt is made to quantify its influence on the halocline waters of the Canadian Basin. For this purpose literature data from the CESAR and LOREX ice camps are used. Based on mass balances and depending on the value of precipitation over the area of the Arctic Ocean the average mean residence time of the river-runoff fraction contained in the Arctic Ocean halocline is determined to be about 14 or 11 years. Water column inventories of river-runoff and sea-ice meltwater are calculated for a section just north of Fram Strait and implications for the ice export rate through Fram Strait are discussed. Salinity, tritium, 3He and the d18O ratio of halocline waters sampled during the 1987 Polarstern cruise to the Nansen Basin are used to estimate the mean residence time of the river-runoff component in the halocline and on the shelves of the Arctic Ocean. These estimates are done by comparing ages of the halocline waters based on a combination of tracers yielding ... Other/Unknown Material amundsen basin Arctic Arctic Ocean Bell Island Berichte zur Polarforschung Bering Strait Fram Strait Greenland Greenland Sea Nansen Basin North Greenland oden Polar Research Polarforschung Reports on polar research Sea ice PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-17.520000,163.603300,88.276700,70.000000) |