RAFOS Float Trajectories from the MOVE Project in the Tropical Atlantic in 2000 and 2001 ...
In early 2000 and again in 2001, RAFOS floats were deployed in the western tropical Atlantic near latitude 16N. These floats drift at pre-determined depths for durations of typically one year or more, and they are geo-located by triangulation using sound signals from moored underwater sound sources....
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ftdatacite:10.1594/pangaea.897147 2024-09-30T14:25:32+00:00 RAFOS Float Trajectories from the MOVE Project in the Tropical Atlantic in 2000 and 2001 ... Lankhorst, Matthias Zenk, Walter 2019 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.897147 https://doi.pangaea.de/10.1594/PANGAEA.897147 en eng PANGAEA https://store.pangaea.de/Publications/Lankhorst-Zenk_2019/move_rafos_trajectories_filtered_and_gaps_removed.asc https://dx.doi.org/10.1016/j.dsr.2009.06.002 https://dx.doi.org/10.1029/2005gl025368 https://store.pangaea.de/Publications/Lankhorst-Zenk_2019/move_rafos_trajectories_filtered_and_gaps_removed.asc Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Event label Sample code/label DATE/TIME Time point, descriptive LATITUDE LONGITUDE DEPTH, water Pressure, water Temperature, water Current velocity, east-west Current velocity, north-south RAFOS float KN161-02 SO153 Knorr Sonne Dataset dataset 2019 ftdatacite https://doi.org/10.1594/pangaea.89714710.1016/j.dsr.2009.06.00210.1029/2005gl025368 2024-09-02T08:37:33Z In early 2000 and again in 2001, RAFOS floats were deployed in the western tropical Atlantic near latitude 16N. These floats drift at pre-determined depths for durations of typically one year or more, and they are geo-located by triangulation using sound signals from moored underwater sound sources. The float trajectories then show the currents of the water they drift in. The first batch of floats drifted in the layer of the Antarctic Intermediate Water near 800m depth, the second in the upper North Atlantic Deep Water near 1400m depth. Here, the trajectory data from the floats (position and lateral velocity) are presented, together with temperature and pressure records. Two versions of the data are included: one that leaves gaps in the trajectories untreated (see "Download data"), and another one that is smoothed with a low-pass filter and has gaps filled or removed (see "Other version"). The floats were part of the Meridional Overturning Variability Experiment (MOVE), a project to investigate the ... Dataset Antarc* Antarctic North Atlantic Deep Water North Atlantic DataCite Antarctic The Antarctic |
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ftdatacite |
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English |
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Event label Sample code/label DATE/TIME Time point, descriptive LATITUDE LONGITUDE DEPTH, water Pressure, water Temperature, water Current velocity, east-west Current velocity, north-south RAFOS float KN161-02 SO153 Knorr Sonne |
spellingShingle |
Event label Sample code/label DATE/TIME Time point, descriptive LATITUDE LONGITUDE DEPTH, water Pressure, water Temperature, water Current velocity, east-west Current velocity, north-south RAFOS float KN161-02 SO153 Knorr Sonne Lankhorst, Matthias Zenk, Walter RAFOS Float Trajectories from the MOVE Project in the Tropical Atlantic in 2000 and 2001 ... |
topic_facet |
Event label Sample code/label DATE/TIME Time point, descriptive LATITUDE LONGITUDE DEPTH, water Pressure, water Temperature, water Current velocity, east-west Current velocity, north-south RAFOS float KN161-02 SO153 Knorr Sonne |
description |
In early 2000 and again in 2001, RAFOS floats were deployed in the western tropical Atlantic near latitude 16N. These floats drift at pre-determined depths for durations of typically one year or more, and they are geo-located by triangulation using sound signals from moored underwater sound sources. The float trajectories then show the currents of the water they drift in. The first batch of floats drifted in the layer of the Antarctic Intermediate Water near 800m depth, the second in the upper North Atlantic Deep Water near 1400m depth. Here, the trajectory data from the floats (position and lateral velocity) are presented, together with temperature and pressure records. Two versions of the data are included: one that leaves gaps in the trajectories untreated (see "Download data"), and another one that is smoothed with a low-pass filter and has gaps filled or removed (see "Other version"). The floats were part of the Meridional Overturning Variability Experiment (MOVE), a project to investigate the ... |
format |
Dataset |
author |
Lankhorst, Matthias Zenk, Walter |
author_facet |
Lankhorst, Matthias Zenk, Walter |
author_sort |
Lankhorst, Matthias |
title |
RAFOS Float Trajectories from the MOVE Project in the Tropical Atlantic in 2000 and 2001 ... |
title_short |
RAFOS Float Trajectories from the MOVE Project in the Tropical Atlantic in 2000 and 2001 ... |
title_full |
RAFOS Float Trajectories from the MOVE Project in the Tropical Atlantic in 2000 and 2001 ... |
title_fullStr |
RAFOS Float Trajectories from the MOVE Project in the Tropical Atlantic in 2000 and 2001 ... |
title_full_unstemmed |
RAFOS Float Trajectories from the MOVE Project in the Tropical Atlantic in 2000 and 2001 ... |
title_sort |
rafos float trajectories from the move project in the tropical atlantic in 2000 and 2001 ... |
publisher |
PANGAEA |
publishDate |
2019 |
url |
https://dx.doi.org/10.1594/pangaea.897147 https://doi.pangaea.de/10.1594/PANGAEA.897147 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic North Atlantic Deep Water North Atlantic |
genre_facet |
Antarc* Antarctic North Atlantic Deep Water North Atlantic |
op_relation |
https://store.pangaea.de/Publications/Lankhorst-Zenk_2019/move_rafos_trajectories_filtered_and_gaps_removed.asc https://dx.doi.org/10.1016/j.dsr.2009.06.002 https://dx.doi.org/10.1029/2005gl025368 https://store.pangaea.de/Publications/Lankhorst-Zenk_2019/move_rafos_trajectories_filtered_and_gaps_removed.asc |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.89714710.1016/j.dsr.2009.06.00210.1029/2005gl025368 |
_version_ |
1811645378309652480 |