Hydrographic and current time series data from outside the southern side of the Isfjorden Mouth during 5 October 2017 to 25 August 2018 at 78°03.653’ N; 013°31.346’ E, and 202 m depth. The mooring was deployed by the University Centre in Svalbard (UNIS) as a part of the AGF course “Polar Ocean Climate” to monitor inflow of Atlantic Water to Isfjorden, and was equipped with three Aanderaa Instruments recoding current meters (RCMs) with auxiliary CTD sensors covering the upper, the intermediate, and the bottom layer. Additionally, three SBE 37 MicroCAT CTDs and five VEMCO mini temperature loggers were evenly distributed over the water column. For further details of the mooring and data, see Skogseth et al. (2019).

Hydrographic and current time series data from outside the southern side of the Isfjorden Mouth during 6 September 2012 to 28 August 2013 at 78°03.643’ N; 013°31.327’ E, and 202 m depth. The mooring was deployed by the University Centre in Svalbard (UNIS) as a part of the AGF course “Polar Ocean Climate” to monitor inflow of Atlantic Water to Isfjorden, and was equipped with three Aanderaa Instruments recoding current meters (RCMs) with auxiliary CTD sensors covering the upper, the intermediate, and the bottom layer. Additionally, three SBE 37 MicroCAT CTDs and five VEMCO mini temperature loggers were evenly distributed over the water column. For further details of the mooring and data, see Skogseth et al. (2019).

Hydrographic and current time series data from inner Tempelfjorden during 29 January 2016 to 23 June 2017 at 78°26.606’ N; 017°21.269’ E, and 52 m depth. The mooring was deployed by the University Centre in Svalbard (UNIS) in collaboration with the Scottish Association for Marine Science (SAMS) as part of the project CRIOS to monitor any influence of water temperature on the tidewater glacier Tunabreen. It was equipped with one Aanderaa Instruments SeaGuard recoding current meter (RCM) with auxiliary CTD sensors close to the bottom. Additionally, three SBE 37 MicroCAT CTDs were distributed within 10 m above the RCM. For further details of the mooring and data, see Skogseth et al. (2019).

Hydrographic and current time series data from outside the southern side of the Isfjorden Mouth during 2 September 2013 to 26 August 2014 at 78°03.625’ N; 013°31.267’ E, and 199 m depth. The mooring was deployed by the University Centre in Svalbard (UNIS) as a part of the AGF course “Polar Ocean Climate” to monitor inflow of Atlantic Water to Isfjorden, and was equipped with three Aanderaa Instruments recoding current meters (RCMs) with auxiliary CTD sensors covering the upper, the intermediate, and the bottom layer. Additionally, two SBE 37 MicroCAT CTDs and four VEMCO mini temperature loggers were evenly distributed over the water column. For further details of the mooring and data, see Skogseth et al. (2019).

Hydrographic and current time series data from outside the southern side of the Isfjorden Mouth during 8 September 2011 to 3 September 2012 at 78°03.637’ N; 013°31.271’ E, and 205 m depth. The mooring was deployed by the University Centre in Svalbard (UNIS) as a part of the AGF course “Polar Ocean Climate” to monitor inflow of Atlantic Water to Isfjorden, and was equipped with three Aanderaa Instruments recoding current meters (RCMs) with auxiliary CTD sensors covering the upper, the intermediate, and the bottom layer. Additionally, three SBE 37 MicroCAT CTDs and five VEMCO mini temperature loggers were evenly distributed over the water column. For further details of the mooring and data, see Skogseth et al. (2019).

Hydrographic and current time series data from outside the southern side of the Isfjorden Mouth during 19 August 2016 to 2 October 2017 at 78°03.667’ N; 013°31.492’ E, and 205 m depth. The mooring was deployed by the University Centre in Svalbard (UNIS) as a part of the AGF course “Polar Ocean Climate” to monitor inflow of Atlantic Water to Isfjorden, and was equipped with one Aanderaa Instruments recording Doppler current profiler (RDCP) and two Aanderaa Instruments recoding current meters (RCMs) with auxiliary CTD sensors covering the upper, the intermediate, and the bottom layer. Additionally, three SBE 37 MicroCAT CTDs and five VEMCO mini temperature loggers were evenly distributed over the water column. For further details of the mooring and data, see Skogseth et al. (2019).