Physical oceanography from mooring KPO_1235
GEOMAR moorings are typically equipped with instruments recording pressure, temperature, conductivity, dissolved oxygen and current velocity. Instruments with pressure, temperature, conductivity and oxygen sensors were calibrated in situ immediately prior to and after a mooring deployment period by...
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PANGAEA
2023
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.962193 https://doi.org/10.1594/PANGAEA.962193 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.962193 2024-09-09T20:08:44+00:00 Physical oceanography from mooring KPO_1235 Brandt, Peter Imbol Koungue, Rodrigue Anicet Krahmann, Gerd Dengler, Marcus LATITUDE: -10.826720 * LONGITUDE: 13.002000 * DATE/TIME START: 2021-04-14T14:09:35 * DATE/TIME END: 2022-05-02T16:06:00 * MINIMUM DEPTH, water: -114.86 m * MAXIMUM DEPTH, water: 1183.59 m 2023 text/tab-separated-values, 1768582 data points https://doi.pangaea.de/10.1594/PANGAEA.962193 https://doi.org/10.1594/PANGAEA.962193 en eng PANGAEA Imbol Koungue, Rodrigue Anicet (in prep.): Drivers and impact of the 2021 extreme warm event in the tropical Angolan upwelling system. Physical oceanography from mooring KPO_1235 in nc format [dataset]. https://download.pangaea.de/reference/121957/attachments/kpo_1235.zip https://doi.pangaea.de/10.1594/PANGAEA.962193 https://doi.org/10.1594/PANGAEA.962193 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Current velocity east-west north-south DATE/TIME DEPTH water Flag KPO_1235 M181 M181_12-1 Meteor (1986) MOOR Mooring Oxygen Pressure Salinity Sample code/label South Atlantic Ocean Temperature TRATLEQ 2 dataset 2023 ftpangaea https://doi.org/10.1594/PANGAEA.962193 2024-07-24T02:31:35Z GEOMAR moorings are typically equipped with instruments recording pressure, temperature, conductivity, dissolved oxygen and current velocity. Instruments with pressure, temperature, conductivity and oxygen sensors were calibrated in situ immediately prior to and after a mooring deployment period by attaching them to the CTD frame during CTDO casts. Correction terms were then developed from the difference between the sensor readings and the calibrated CTDO data during several minute long calibration stops. These correction terms were then applied to the full deployment periods. This ensured best data quality with recognition of potential sensor drifts and also allowed for the estimation of calibration and measurement errors (Hahn et al. 2014, Bittig et al. 2018, Berx et al. 2019). Dataset South Atlantic Ocean PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(13.002000,13.002000,-10.826720,-10.826720) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Current velocity east-west north-south DATE/TIME DEPTH water Flag KPO_1235 M181 M181_12-1 Meteor (1986) MOOR Mooring Oxygen Pressure Salinity Sample code/label South Atlantic Ocean Temperature TRATLEQ 2 |
spellingShingle |
Current velocity east-west north-south DATE/TIME DEPTH water Flag KPO_1235 M181 M181_12-1 Meteor (1986) MOOR Mooring Oxygen Pressure Salinity Sample code/label South Atlantic Ocean Temperature TRATLEQ 2 Brandt, Peter Imbol Koungue, Rodrigue Anicet Krahmann, Gerd Dengler, Marcus Physical oceanography from mooring KPO_1235 |
topic_facet |
Current velocity east-west north-south DATE/TIME DEPTH water Flag KPO_1235 M181 M181_12-1 Meteor (1986) MOOR Mooring Oxygen Pressure Salinity Sample code/label South Atlantic Ocean Temperature TRATLEQ 2 |
description |
GEOMAR moorings are typically equipped with instruments recording pressure, temperature, conductivity, dissolved oxygen and current velocity. Instruments with pressure, temperature, conductivity and oxygen sensors were calibrated in situ immediately prior to and after a mooring deployment period by attaching them to the CTD frame during CTDO casts. Correction terms were then developed from the difference between the sensor readings and the calibrated CTDO data during several minute long calibration stops. These correction terms were then applied to the full deployment periods. This ensured best data quality with recognition of potential sensor drifts and also allowed for the estimation of calibration and measurement errors (Hahn et al. 2014, Bittig et al. 2018, Berx et al. 2019). |
format |
Dataset |
author |
Brandt, Peter Imbol Koungue, Rodrigue Anicet Krahmann, Gerd Dengler, Marcus |
author_facet |
Brandt, Peter Imbol Koungue, Rodrigue Anicet Krahmann, Gerd Dengler, Marcus |
author_sort |
Brandt, Peter |
title |
Physical oceanography from mooring KPO_1235 |
title_short |
Physical oceanography from mooring KPO_1235 |
title_full |
Physical oceanography from mooring KPO_1235 |
title_fullStr |
Physical oceanography from mooring KPO_1235 |
title_full_unstemmed |
Physical oceanography from mooring KPO_1235 |
title_sort |
physical oceanography from mooring kpo_1235 |
publisher |
PANGAEA |
publishDate |
2023 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.962193 https://doi.org/10.1594/PANGAEA.962193 |
op_coverage |
LATITUDE: -10.826720 * LONGITUDE: 13.002000 * DATE/TIME START: 2021-04-14T14:09:35 * DATE/TIME END: 2022-05-02T16:06:00 * MINIMUM DEPTH, water: -114.86 m * MAXIMUM DEPTH, water: 1183.59 m |
long_lat |
ENVELOPE(13.002000,13.002000,-10.826720,-10.826720) |
genre |
South Atlantic Ocean |
genre_facet |
South Atlantic Ocean |
op_relation |
Imbol Koungue, Rodrigue Anicet (in prep.): Drivers and impact of the 2021 extreme warm event in the tropical Angolan upwelling system. Physical oceanography from mooring KPO_1235 in nc format [dataset]. https://download.pangaea.de/reference/121957/attachments/kpo_1235.zip https://doi.pangaea.de/10.1594/PANGAEA.962193 https://doi.org/10.1594/PANGAEA.962193 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.962193 |
_version_ |
1809942799871639552 |