Underway physical oceanography and carbonate chemistry measured during the EURO-BASIN cruise M87/1 (Deep Convection Cruise)
The track of the cruise, and the location of the different stations cover a large range of water masses, many of which take part in the exchange across the Greenland-Scotland Ridge, and of importance for the biogeochemical fluxes in the region. These water masses are of very different origins, which...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.830273 2024-09-15T18:05:42+00:00 Underway physical oceanography and carbonate chemistry measured during the EURO-BASIN cruise M87/1 (Deep Convection Cruise) Bellerby, Richard G J MEDIAN LATITUDE: 60.844034 * MEDIAN LONGITUDE: -7.192515 * SOUTH-BOUND LATITUDE: 42.750000 * WEST-BOUND LONGITUDE: -13.840000 * NORTH-BOUND LATITUDE: 63.670000 * EAST-BOUND LONGITUDE: 1.010000 * DATE/TIME START: 2012-03-19T00:00:00 * DATE/TIME END: 2012-05-02T00:00:00 * MINIMUM DEPTH, water: 0 m * MAXIMUM DEPTH, water: 0 m 2014 text/tab-separated-values, 335700 data points https://doi.pangaea.de/10.1594/PANGAEA.830273 https://doi.org/10.1594/PANGAEA.830273 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.830273 https://doi.org/10.1594/PANGAEA.830273 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Bjerknes Centre for Climate Research Basin Scale Analysis Synthesis and Integration CT Deep Convection Cruise DEPTH water EURO-BASIN Event label Faroe Islands Fugacity of carbon dioxide (water) at sea surface temperature (wet air) LATITUDE LONGITUDE M87/1a M87/1a-track M87/1b M87/1b-track Meteor (1986) Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pressure atmospheric Pressure at equilibration Salinity Temperature Temperature at equilibration Time Stamp Underway cruise track measurements xCO2 (water) at equilibrator temperature (dry air) dataset 2014 ftpangaea https://doi.org/10.1594/PANGAEA.830273 2024-07-24T02:31:32Z The track of the cruise, and the location of the different stations cover a large range of water masses, many of which take part in the exchange across the Greenland-Scotland Ridge, and of importance for the biogeochemical fluxes in the region. These water masses are of very different origins, which can be observed in the concentration of the different biogeochemical parameters. The concentrations are a result of the combination of the physical and biogeochemical environment in each formation region, and the processes acting on the water masses as they are transported away from the formation areas. The aim of the biogeochemistry measurements was to achieve a better understanding of the strength and variability of the biological carbon pump in the North Atlantic and Nordic Seas. Dataset Faroe Islands Greenland Greenland-Scotland Ridge Nordic Seas North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-13.840000,1.010000,63.670000,42.750000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Basin Scale Analysis Synthesis and Integration CT Deep Convection Cruise DEPTH water EURO-BASIN Event label Faroe Islands Fugacity of carbon dioxide (water) at sea surface temperature (wet air) LATITUDE LONGITUDE M87/1a M87/1a-track M87/1b M87/1b-track Meteor (1986) Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pressure atmospheric Pressure at equilibration Salinity Temperature Temperature at equilibration Time Stamp Underway cruise track measurements xCO2 (water) at equilibrator temperature (dry air) |
spellingShingle |
Basin Scale Analysis Synthesis and Integration CT Deep Convection Cruise DEPTH water EURO-BASIN Event label Faroe Islands Fugacity of carbon dioxide (water) at sea surface temperature (wet air) LATITUDE LONGITUDE M87/1a M87/1a-track M87/1b M87/1b-track Meteor (1986) Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pressure atmospheric Pressure at equilibration Salinity Temperature Temperature at equilibration Time Stamp Underway cruise track measurements xCO2 (water) at equilibrator temperature (dry air) Bellerby, Richard G J Underway physical oceanography and carbonate chemistry measured during the EURO-BASIN cruise M87/1 (Deep Convection Cruise) |
topic_facet |
Basin Scale Analysis Synthesis and Integration CT Deep Convection Cruise DEPTH water EURO-BASIN Event label Faroe Islands Fugacity of carbon dioxide (water) at sea surface temperature (wet air) LATITUDE LONGITUDE M87/1a M87/1a-track M87/1b M87/1b-track Meteor (1986) Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pressure atmospheric Pressure at equilibration Salinity Temperature Temperature at equilibration Time Stamp Underway cruise track measurements xCO2 (water) at equilibrator temperature (dry air) |
description |
The track of the cruise, and the location of the different stations cover a large range of water masses, many of which take part in the exchange across the Greenland-Scotland Ridge, and of importance for the biogeochemical fluxes in the region. These water masses are of very different origins, which can be observed in the concentration of the different biogeochemical parameters. The concentrations are a result of the combination of the physical and biogeochemical environment in each formation region, and the processes acting on the water masses as they are transported away from the formation areas. The aim of the biogeochemistry measurements was to achieve a better understanding of the strength and variability of the biological carbon pump in the North Atlantic and Nordic Seas. |
format |
Dataset |
author |
Bellerby, Richard G J |
author_facet |
Bellerby, Richard G J |
author_sort |
Bellerby, Richard G J |
title |
Underway physical oceanography and carbonate chemistry measured during the EURO-BASIN cruise M87/1 (Deep Convection Cruise) |
title_short |
Underway physical oceanography and carbonate chemistry measured during the EURO-BASIN cruise M87/1 (Deep Convection Cruise) |
title_full |
Underway physical oceanography and carbonate chemistry measured during the EURO-BASIN cruise M87/1 (Deep Convection Cruise) |
title_fullStr |
Underway physical oceanography and carbonate chemistry measured during the EURO-BASIN cruise M87/1 (Deep Convection Cruise) |
title_full_unstemmed |
Underway physical oceanography and carbonate chemistry measured during the EURO-BASIN cruise M87/1 (Deep Convection Cruise) |
title_sort |
underway physical oceanography and carbonate chemistry measured during the euro-basin cruise m87/1 (deep convection cruise) |
publisher |
PANGAEA |
publishDate |
2014 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.830273 https://doi.org/10.1594/PANGAEA.830273 |
op_coverage |
MEDIAN LATITUDE: 60.844034 * MEDIAN LONGITUDE: -7.192515 * SOUTH-BOUND LATITUDE: 42.750000 * WEST-BOUND LONGITUDE: -13.840000 * NORTH-BOUND LATITUDE: 63.670000 * EAST-BOUND LONGITUDE: 1.010000 * DATE/TIME START: 2012-03-19T00:00:00 * DATE/TIME END: 2012-05-02T00:00:00 * MINIMUM DEPTH, water: 0 m * MAXIMUM DEPTH, water: 0 m |
long_lat |
ENVELOPE(-13.840000,1.010000,63.670000,42.750000) |
genre |
Faroe Islands Greenland Greenland-Scotland Ridge Nordic Seas North Atlantic |
genre_facet |
Faroe Islands Greenland Greenland-Scotland Ridge Nordic Seas North Atlantic |
op_source |
Bjerknes Centre for Climate Research |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.830273 https://doi.org/10.1594/PANGAEA.830273 |
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.830273 |
_version_ |
1810443221405270016 |