Water temperature and salinity taken by CTD and XBT from vessel Arctic Sunrise in Kangerlussuaq Fjord and Nioghalvfjerdsfjorden, Greenland, from 2009-08-28 to 2009-09-08 (NCEI Accession 0210954)
공공데이터포털
These temperature and salinity profiles were collected in Kangerlussuaq Fjord and Nioghalvfjerdsfjorden, Greenland, during August and September 2009. The XBT profiles were collected with Lockheed Martin XBTs, types 5, 6, and 7. The profiles are 1 m bin averages. The CTD profiles were collected with two RBR CTDs, serial numbers 18559 and 12845; these profiles are also 1 m bin averages. Data are in NetCDF.
Water temperature, conductivity, and current data collected by CTDs and current meters on moored buoys in the Sermilik Fjord and Kangerlussuaq Glacier, in East Greenland from 2009-08-17 to 2012-09-11 (NCEI Accession 0127320)
공공데이터포털
The data included in this dataset were collected in East Greenland in the Sermilik Fjord, located in the Ammassalik district close to the town of Tasiilaq, and at the Kangerlussuaq Glacier. Data collection was conducted by deploying eleven moorings from August 2009 to August 2010. One mooring was not recovered until September 2012 and three moorings were never recovered. The recovered moorings located in the Sermilik Fjord were named CM1, CM3, CM5, CM6, and SM3. The recovered moorings located at Kangerlussuaq Glacier were GP1, GP2, and GP3. The moorings were equipped with SBE MicroCATs, Onset UTBI-001 TidbiTs, Nortek Aquadopps, RBR DR-1050s, and RBR XR-420s.
Water Temperature, conductivity, and currents data collected by CTDs and current meters on moored buoys in the Sermilik Fjord, Greenland from 2012-09-18 to 2013-08-20 (NCEI Accession 0127325)
공공데이터포털
The data included in this dataset were collected in the Sermilik Fjord, located in East Greenland in the Ammassalik district close to the town of Tasiilaq. Data collection was conducted by deploying five moorings from September 2012 to August 2013. One mooring was not recovered. The four recovered moorings were named CM0, CM1, CM5, and SF4. Mooring CM0 was located mid-fjord at a depth of 125 meters and was equipped with an SBE MicroCAT, an RBR DR-1050, and an Onset U-22 ProV2. Mooring CM1 was located next to CM0 at a depth of 125 meters. It was equipped with an SBE MicroCAT, an RBR DR-1050, and an Onset UTBI-001 TidbiT. Mooring CM5 was located outside of the fjord entrance at a depth of 290 meters. It was equipped with an SBE MicroCAT and a Nortek Aquadopp. Mooring SF4 was positioned in the middle of the fjord at a depth of 880 meters. Data collected from this mooring included two RBR XR-420s, ten Onset UTBI-001 Temperature Loggers, two SBE MicroCAT, an RBR DR-1050, a Nortek Aquadopp, and an RDI LR-ADCP.
Temperature and conductivity data collected by CTDs on moored buoys in the Sermilik Fjord, Greenland from 2008-07 to 2009-08 (NCEI Accession 0123217)
공공데이터포털
The data included in this dataset were collected in the Sermilik Fjord, located in East Greenland in the Ammassalik district close to the town of Tasiilaq. Data collection was conducted during the summer of 2008 in separate legs. During the first leg, which took place during July 2008, two moorings were deployed; one at a depth of 185 meters and one at a depth of 25 meters. The deeper mooring was equipped with one RBR DR-1050 depth recorder, 10 Onset UBTI-001 Temperature Loggers, and one SBE-37(P) Microcat. The shallow mooring was equipped with one RBR DR-1050 depth recorder and one SBE-37(P) Microcat. These moorings were deployed on July 6, 2008 and were recovered on September 1, 2008. The second leg of the data collection, which took place in September 2008, also deployed two moorings at the same locations as the July moorings. Each of these moorings was equipped with one SBE-37 (P) Microcat. These two moorings were deployed on Sept 3, 2008. The shallow mooring was recovered on August 20, 2009 and the deep mooring was recovered on November 16, 2011. The purpose of this data collection was part of an exploratory project whose long term goals were to: 1) quantify the (liquid) fresh water flux out of Sermilik Fjord, and 2) determine what water masses flow into the fjord. In particular, if the warm, Atlantic water (Irminger Water) which is found off the slope, is able to penetrate into the fjord.