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Abstract:
The CTD measurements were collected in Isfjorden (78°70’ N-78°27’ N, 13°-17° E), Spitsbergen during the cruises on the R/V Oceania conducted by the Institute of Oceanology of the Polish Academy of Sciences (IO PAN) in the late July – early August surveys (covering the main melting season) in 2013–2019 (24-25 July 2013, 24 July 2014, 10 August 2015, 9-10 August 2016, 12-13 August 2017, 2-3 August 2018, 26-27 July 2019). The continuous, high resolution laser-based measurements were performed within the upper 70-m water column along a 60-km transect crossing Isfjorden, starting from sampling station located at the mouth of the southern branch of Isfjorden – Adventfjorden (ISA), through station in the central part of Isfjorden (ISF3 sampling station) up to the innermost part of Billefjorden (BAB sampling station). A conductivity-temperature-depth sensors (CTD, SBE 911plus, Seabird Electronics Inc., USA) and a fluorometer (Seapoint Sensors Inc., USA) were used to collect presented data.Access: copyrightShow more...
Abstract:
The CTD measurements were collected in Isfjorden (78°70’ N-78°27’ N, 13°-17° E), Spitsbergen during the cruises on the R/V Oceania conducted by the Institute of Oceanology of the Polish Academy of Sciences (IO PAN) in the late July – early August surveys (covering the main melting season) in 2013–2019 (24-25 July 2013, 24 July 2014, 10 August 2015, 9-10 August 2016, 12-13 August 2017, 2-3 August 2018, 26-27 July 2019). The continuous, high resolution laser-based measurements were performed within the upper 70-m water column along a 60-km transect crossing Isfjorden, starting from sampling station located at the mouth of the southern branch of Isfjorden – Adventfjorden (ISA), through station in the central part of Isfjorden (ISF3 sampling station) up to the innermost part of Billefjorden (BAB sampling station). A conductivity-temperature-depth sensors (CTD, SBE 911plus, Seabird Electronics Inc., USA) and a fluorometer (Seapoint Sensors Inc., USA) were used to collect presented data.Access: copyrightShow more...
Abstract:
The CTD measurements were collected in Isfjorden (78°70’ N-78°27’ N, 13°-17° E), Spitsbergen during the cruises on the R/V Oceania conducted by the Institute of Oceanology of the Polish Academy of Sciences (IO PAN) in the late July – early August surveys (covering the main melting season) in 2013–2019 (24-25 July 2013, 24 July 2014, 10 August 2015, 9-10 August 2016, 12-13 August 2017, 2-3 August 2018, 26-27 July 2019). The continuous, high resolution laser-based measurements were performed within the upper 70-m water column along a 60-km transect crossing Isfjorden, starting from sampling station located at the mouth of the southern branch of Isfjorden – Adventfjorden (ISA), through station in the central part of Isfjorden (ISF3 sampling station) up to the innermost part of Billefjorden (BAB sampling station). A conductivity-temperature-depth sensors (CTD, SBE 911plus, Seabird Electronics Inc., USA) and a fluorometer (Seapoint Sensors Inc., USA) were used to collect presented data.Access: copyrightShow more...
Abstract:
The CTD measurements were collected in Isfjorden (78°70’ N-78°27’ N, 13°-17° E), Spitsbergen during the cruises on the R/V Oceania conducted by the Institute of Oceanology of the Polish Academy of Sciences (IO PAN) in the late July – early August surveys (covering the main melting season) in 2013–2019 (24-25 July 2013, 24 July 2014, 10 August 2015, 9-10 August 2016, 12-13 August 2017, 2-3 August 2018, 26-27 July 2019). The continuous, high resolution laser-based measurements were performed within the upper 70-m water column along a 60-km transect crossing Isfjorden, starting from sampling station located at the mouth of the southern branch of Isfjorden – Adventfjorden (ISA), through station in the central part of Isfjorden (ISF3 sampling station) up to the innermost part of Billefjorden (BAB sampling station). A conductivity-temperature-depth sensors (CTD, SBE 911plus, Seabird Electronics Inc., USA) and a fluorometer (Seapoint Sensors Inc., USA) were used to collect presented data.Access: copyrightShow more...
Abstract:
The CTD measurements were collected in Isfjorden (78°70’ N-78°27’ N, 13°-17° E), Spitsbergen during the cruises on the R/V Oceania conducted by the Institute of Oceanology of the Polish Academy of Sciences (IO PAN) in the late July – early August surveys (covering the main melting season) in 2013–2019 (24-25 July 2013, 24 July 2014, 10 August 2015, 9-10 August 2016, 12-13 August 2017, 2-3 August 2018, 26-27 July 2019). The continuous, high resolution laser-based measurements were performed within the upper 70-m water column along a 60-km transect crossing Isfjorden, starting from sampling station located at the mouth of the southern branch of Isfjorden – Adventfjorden (ISA), through station in the central part of Isfjorden (ISF3 sampling station) up to the innermost part of Billefjorden (BAB sampling station). A conductivity-temperature-depth sensors (CTD, SBE 911plus, Seabird Electronics Inc., USA) and a fluorometer (Seapoint Sensors Inc., USA) were used to collect presented data.Access: copyrightShow more...
Abstract:
The CTD measurements were collected in Isfjorden (78°70’ N-78°27’ N, 13°-17° E), Spitsbergen during the cruises on the R/V Oceania conducted by the Institute of Oceanology of the Polish Academy of Sciences (IO PAN) in the late July – early August surveys (covering the main melting season) in 2013–2019 (24-25 July 2013, 24 July 2014, 10 August 2015, 9-10 August 2016, 12-13 August 2017, 2-3 August 2018, 26-27 July 2019). The continuous, high resolution laser-based measurements were performed within the upper 70-m water column along a 60-km transect crossing Isfjorden, starting from sampling station located at the mouth of the southern branch of Isfjorden – Adventfjorden (ISA), through station in the central part of Isfjorden (ISF3 sampling station) up to the innermost part of Billefjorden (BAB sampling station). A conductivity-temperature-depth sensors (CTD, SBE 911plus, Seabird Electronics Inc., USA) and a fluorometer (Seapoint Sensors Inc., USA) were used to collect presented data.Access: copyrightShow more...
Abstract:
The CTD measurements were collected in Isfjorden (78°70’ N-78°27’ N, 13°-17° E), Spitsbergen during the cruises on the R/V Oceania conducted by the Institute of Oceanology of the Polish Academy of Sciences (IO PAN) in the late July – early August surveys (covering the main melting season) in 2013–2019 (24-25 July 2013, 24 July 2014, 10 August 2015, 9-10 August 2016, 12-13 August 2017, 2-3 August 2018, 26-27 July 2019). The continuous, high resolution laser-based measurements were performed within the upper 70-m water column along a 60-km transect crossing Isfjorden, starting from sampling station located at the mouth of the southern branch of Isfjorden – Adventfjorden (ISA), through station in the central part of Isfjorden (ISF3 sampling station) up to the innermost part of Billefjorden (BAB sampling station). A conductivity-temperature-depth sensors (CTD, SBE 911plus, Seabird Electronics Inc., USA) and a fluorometer (Seapoint Sensors Inc., USA) were used to collect presented data.Access: copyrightShow more...
Abstract:
Hydrographic and current time series data from outside the northern side of the Isfjorden Mouth during 5 October 2017 to 24 August 2018 at 78°10.911’ N; 013°23.350’ E, and 242 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 outflow from Isfjorden and the hydrographic differences between the northern and southern part of the mouth. It was equipped with two Aanderaa Instruments recoding current meters (RCMs) with auxiliary CTD sensors covering the upper and the bottom layer. Additionally, three SBE 37 MicroCAT CTDs and three VEMCO mini temperature loggers were evenly distributed over the water column. For further details of the mooring and data, see Skogseth et al. (2019).Show more...
Abstract:
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).Show more...
Abstract:
Hydrographic and current time series data from Isfjorden online mooring (IFO) during 30 September 2016 to 11 March 2017 at 78°14.845’ N; 015°19.870’ E, and 60 m depth. The mooring was deployed by the University Centre in Svalbard (UNIS) in collaboration with Aanderaa Data Instruments (AADI) as part of the Svalbard Environmental Protection Fund project “Blir det is på Isfjorden i år?” to monitor inflow of Atlantic Water to Isfjorden and possible presence of sea ice on the surface. IFO constituted of an Aanderaa Instruments recording Doppler current profiler (SeaGuard II) configured with 2-m bins and with auxiliary CTD sensors, and was deployed on 30 September 2016 in a bottom frame at 60 m depth. On 3 November 2016, a 40 m SeaGuard string with temperature and conductivity sensors at 46 m and 33 m depths was connected to the SeaGuard II and ended in an in-line SeaGuard with auxiliary CTD sensors at 20 m depth. The sea cable providing power to the instruments and transferring data to land, was cut off on 11 March 2017. For further details of the mooring and data, see Skogseth et al. (2019).Show more...
Abstract:
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).Show more...
Abstract:
Hydrographic and current time series data from outside the northern side of the Isfjorden Mouth during 15 October 2016 to 2 October 2017 at 78°10.927’ N; 013°23.000’ E, and 224 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 outflow from Isfjorden and the hydrographic differences between the northern and southern part of the mouth. It 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 were evenly distributed over the water column. For further details of the mooring and data, see Skogseth et al. (2019).Show more...
Abstract:
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).Show more...
Abstract:
Hydrographic and current time series data from outside the southern side of the Isfjorden Mouth during 31 August 2015 to 12 August 2016 at 78.0611 deg. N and 13.5249 deg. 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).Show more...
Abstract:
Hydrographic and current time series data from outside the northern side of the Isfjorden Mouth during 31 August 2015 to 12 August 2016 at 78°10.829’ N; 013°22.737’ E, and 228 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 outflow from Isfjorden and the hydrographic differences between the northern and southern part of the mouth. It was equipped with three Aanderaa Instruments recoding current meters (RCMs) with auxiliary CTD sensors covering the upper, the intermediate, and the bottom layer. For further details of the mooring and data, see Skogseth et al. (2019).
