Hydrological and current velocity data from moorings P1, P2, P4, P5 and P6 in the Filchner Trough region in the southern Weddell Sea, February 2017 to March 2021
Deep water formed around the Antarctic continent drives the world ocean circulation. More than 50% of this deep water is formed within only about 10% of the Antarctic circumpolar band: the Weddell Sea. Subtle changes in the circulation of the Weddell Sea can lead to major changes in floating ice shelves, with critical implications for global sea-level, the production of deep water, and the global ocean overturning circulation. The Filchner Trough on the continental shelf in the southern Weddell Sea plays an important role for the water mass exchange between the cold water on the continental shelf and the warm water off the continental shelf: It serves as a conduit for relatively warm water to flow southward across the continental shelf toward the Filchner Ronne Ice shelf and for the dense, cold water produced underneath the ice shelf to flow northward off the continental shelf to feed Antarctic Bottom Water. Four moorings (P1, P2, P4, P5) were places within the inflow pathway of the warm water at the northern entrance to the Filchner Trough on the continental shelf, and one mooring (P6) was placed off the continental shelf over the deep ocean. The mooring time series cover the period from February 2017 to March 2021 and are used to investigate the processes controlling the on-shore transport of relatively warm water onto the shelf toward the ice shelf and the interaction of the warm water with the cold dense water. The moorings provide observations of the circulation on the continental shelf and the temperature variability on small (tidal) to large (seasonal, interannual) time scales.
Important Note: This submission has been initially submitted to SEA
scieNtific Open data Edition (SEANOE) publication service and received the recorded DOI.
The metadata elements have been further processed (refined) in EMODnet
Ingestion Service in order to conform with the Data Submission Service
specifications.
owner : {{md.getOwnername()}}
{{'mdStatusRecord' | translate}}: {{('mdStatus-' + md.mdStatus) | translate}}
- Identification
- Content
- ReferenceSystem
- Quality
- DomainConsistancy
- Constraints
- Distribution
- Meta-metadata
- ObjectCatalogue
Date | 2023-06-21 |
---|---|
Date type | Creation: Date identifies when the resource was brought into existence |
Date | 2024-12-06 |
Date type | Revision: Date identifies when the resource was examined or re-examined and improved or amended |
Date | 2025-01-23 |
Date type | Publication: Date identifies when the resource was issued |
Date type | Publication: Date identifies when the resource was issued |
Unique resource identifier | a53ad03f-3130-1303-3030-000000100680 |
Unique resource identifier |
Point of contact
Organisation name | SEA scieNtific Open data Edition |
---|---|
Delivery point | By address: IFREMER / IDM / SISMER - Scientific Information Systems for the SEA, IFREMER Centre de Bretagne, ZI Pointe du diable CS 10070 |
City | PLOUZANE |
Postal code | 29280 |
Country | France |
Electronic mail address | data@seanoe.org |
Linkage | https://www.seanoe.org/ |
Role | Publisher: Publisher |
Point of contact
Organisation name | Ifremer, Scientific Information Systems for the sea |
---|---|
Delivery point | IFREMER Centre de Bretagne ZI Pointe du diable CS 10070 |
City | PLOUZANE |
Postal code | 29280 |
Country | France |
Electronic mail address | sismer@ifremer.fr |
Linkage | http://data.ifremer.fr/SISMER |
Role | Dataset Holding Organisation: Dataset Holding Organisation |
Point of contact
Organisation name | Ifremer, Scientific Information Systems for the sea |
---|---|
Delivery point | IFREMER Centre de Bretagne ZI Pointe du diable CS 10070 |
City | PLOUZANE |
Postal code | 29280 |
Country | France |
Electronic mail address | sismer@ifremer.fr |
Linkage | http://data.ifremer.fr/SISMER |
Role | Author: Party who authored the resource |
Descriptive keywords
GEMET - INSPIRE themes, version 1.0 | |
---|---|
SeaDataNet Agreed Parameter Groups |
Water column temperature and salinity
|
Currents
|
SeaDataNet device categories |
current meters
|
current profilers
|
salinity sensor
|
SeaVoX Device Catalogue |
Nortek Aquadopp 3D Doppler current meter
|
Teledyne RDI 300 kHz narrowband vessel-mounted ADCP
|
Teledyne RDI Ocean Observer 75 kHz narrowband ADCP
|
Sea-Bird SBE 37 MicroCat CTP (submersible) CTD sensor series
|
SeaDataNet Parameter Discovery Vocabulary |
Salinity of the water column
|
Horizontal velocity of the water column (currents)
|
Temperature of the water column
|
SeaVoX Platform Categories | mooring |
MEDIN data format categories | Network Common Data Form |
Character set | UTF8: 8-bit variable size UCS Transfer Format, based on ISO/IEC 10646 |
---|---|
Topic category code |
|
Reference System Information
Anchor | WGS 1984 |
---|
Hierarchy level | Dataset: Information applies to the dataset |
---|
Lineage
Statement | Processed data|Deep water formed around the Antarctic continent drives the world ocean circulation. More than 50% of this deep water is formed within only about 10% of the Antarctic circumpolar band: the Weddell Sea. Subtle changes in the circulation of the Weddell Sea can lead to major changes in floating ice shelves, with critical implications for global sea-level, the production of deep water, and the global ocean overturning circulation. The Filchner Trough on the continental shelf in the southern Weddell Sea plays an important role for the water mass exchange between the cold water on the continental shelf and the warm water off the continental shelf: It serves as a conduit for relatively warm water to flow southward across the continental shelf toward the Filchner Ronne Ice shelf and for the dense, cold water produced underneath the ice shelf to flow northward off the continental shelf to feed Antarctic Bottom Water. Four moorings (P1, P2, P4, P5) were places within the inflow pathway of the warm water at the northern entrance to the Filchner Trough on the continental shelf, and one mooring (P6) was placed off the continental shelf over the deep ocean. The mooring time series cover the period from February 2017 to March 2021 and are used to investigate the processes controlling the on-shore transport of relatively warm water onto the shelf toward the ice shelf and the interaction of the warm water with the cold dense water. The moorings provide observations of the circulation on the continental shelf and the temperature variability on small (tidal) to large (seasonal, interannual) time scales. |
---|
Domain consistency
Conformance result
|
Domain consistency
Conformance result
|
Domain consistency
Conformance result
|
mdLegalAndSecurityConstraintsSection
Resource constraints
|
|||||||||||
Resource constraints
|
Transfer options
|
File identifier | a53ad03f-3130-1303-3030-000000100680 | ||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Metadata language | English | ||||||||||||||||
Character set | UTF8: 8-bit variable size UCS Transfer Format, based on ISO/IEC 10646 | ||||||||||||||||
Hierarchy level | Dataset: Information applies to the dataset | ||||||||||||||||
Date stamp | 2025-03-13T00:00:00 | ||||||||||||||||
Metadata standard name | ISO 19115:2003/19139 | ||||||||||||||||
Metadata standard version | 1.0 | ||||||||||||||||
Contact
|
Overviews
extent
- geoDesc
- {{d}}
- geoBox
-
- geoDescCode
- {{mdView.current.record.geoDescCode}}
tempExtent
- creationDate
- publicationDate
- revisionDate
- tempExtentBegin
Associated resources
Not available