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  • 1
    Publication Date: 2024-07-04
    Description: The multibeam echo sounder (MBES) data was collected from the 03.02.2019 (09:44 UTC) to the 13.02.2019 (16:19 UTC) with the Kongsberg EM122 on RV SONNE during the transit from Suva (Fiji) to Manzanillo (Mexico) in the Pacific Ocean. The deep-water MBES EM122 operates with an acoustic frequency of 12 kHz and a beam opening angle of 0.5° x 1°. The raw and unprocessed bathymetric and backscatter data is stored in Kongsberg format (*.all), each containing up to 60 min of data. The therein included time, motion and position data (WGS84, geographic) was measured by the Kongsberg Seapath system on board. During the acquisition the echo sounder was monitored as well as settings and filter adjusted according to the environment. The transit speed was up to 13 knots. The swath opening angle was set to 70° resulting in a swath width of about 15 km in 3,000 m water depth. Further, high density and dual swath mode were used resulting in 2 x 432 beams per ping. As the data was collected during transit, no specific surveys were performed. No sound velocity profiles (SVPs) were measured during the cruise. In the beginning of data acquisition, an SVP from a previous cruise was used. On the 04.02.2019, a synthetic SVP extracted from he World Ocean Atlas 2009 from NOAA (Levitus, 2013) using the software "Sound Speed Manager" (developed by the UNH Center for Coastal and Ocean Mapping and NOAA Coast Survey Development Laboratory (CSDL)) was applied in the MBES acquisition software SIS. The SVP data is not part of this submission but can be extracted from the *.all files. The data was post-processed using the software QPS Qimera. No further SVP re-computation, navigation correction or tide correction was applied. Erroneous depth measurements were deleted manually by using the swath and slice editor. The vertical datum is mean sea level (MSL). The cleaned data was exported as bathymetric grids in a resolution of 100 m (geotiff format, projected coordinates WGS84/UTM zone 5S (EPSG: 32705)).
    Keywords: Bathymetry; Binary Object; Binary Object (File Size); Binary Object (Media Type); Elevation, maximum; Elevation, minimum; File content; Horizontal datum; Horizontal datum, projection stored in file; KEM122; KONGSBERG EM122; Latitude, northbound; Latitude, southbound; Longitude, eastbound; Longitude, westbound; OceanLight; Pacific Ocean; Raster cell size; SO267/2; SO267/2_0_Underway-1; Sonne_2; UTM Easting, Universal Transverse Mercator; UTM Northing, Universal Transverse Mercator; UTM Zone, Universal Transverse Mercator; Vertical datum
    Type: Dataset
    Format: text/tab-separated-values, 187 data points
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2024-07-04
    Description: The multibeam echo sounder (MBES) data was collected from the 03.02.2019 (09:44 UTC) to the 13.02.2019 (16:19 UTC) with the Kongsberg EM122 on RV SONNE during the transit from Suva (Fiji) to Manzanillo (Mexico) in the Pacific Ocean. The deep-water MBES EM122 operates with an acoustic frequency of 12 kHz and a beam opening angle of 0.5° x 1°. The raw and unprocessed bathymetric and backscatter data is stored in Kongsberg format (*.all), each containing up to 60 min of data. The therein included time, motion and position data (WGS84, geographic) was measured by the Kongsberg Seapath system on board. During the acquisition the echo sounder was monitored as well as settings and filter adjusted according to the environment. The transit speed was up to 13 knots. The swath opening angle was set to 70° resulting in a swath width of about 15 km in 3,000 m water depth. Further, high density and dual swath mode were used resulting in 2 x 432 beams per ping. As the data was collected during transit, no specific surveys were performed. No sound velocity profiles (SVPs) were measured during the cruise. In the beginning of data acquisition, an SVP from a previous cruise was used. On the 04.02.2019, a synthetic SVP extracted from he World Ocean Atlas 2009 from NOAA (Levitus, 2013) using the software "Sound Speed Manager" (developed by the UNH Center for Coastal and Ocean Mapping and NOAA Coast Survey Development Laboratory (CSDL)) was applied in the MBES acquisition software SIS. The SVP data is not part of this submission but can be extracted from the *.all files. The data was post-processed using the software QPS Qimera. No further SVP re-computation, navigation correction or tide correction was applied. Erroneous depth measurements were deleted manually by using the swath and slice editor. The vertical datum is mean sea level (MSL). The cleaned data was exported in gsf format.
    Keywords: Bathymetry; Binary Object; Binary Object (File Size); Binary Object (Media Type); Comment; Data file recording distance; Data file recording duration; DATE/TIME; ELEVATION; Event label; File content; KEM122; KONGSBERG EM122; LATITUDE; LONGITUDE; Number of pings; OceanLight; Pacific Ocean; Ship speed; SO267/2; SO267/2_0_Underway-1; Sonne_2; Start of data file, depth; Start of data file, heading; Start of data file recording, date/time; Start of data file recording, latitude; Start of data file recording, longitude; Stop of data file, depth; Stop of data file, heading; Stop of data file recording, date/time; Stop of data file recording, latitude; Stop of data file recording, longitude
    Type: Dataset
    Format: text/tab-separated-values, 4352 data points
    Location Call Number Expected Availability
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  • 3
    Publication Date: 2024-07-04
    Description: The multibeam echo sounder (MBES) data was collected from the 03.02.2019 (09:44 UTC) to the 13.02.2019 (16:19 UTC) with the Kongsberg EM122 on RV SONNE during the transit from Suva (Fiji) to Manzanillo (Mexico) in the Pacific Ocean. The deep-water MBES EM122 operates with an acoustic frequency of 12 kHz and a beam opening angle of 0.5° x 1°. The raw and unprocessed bathymetric and backscatter data is stored in Kongsberg format (*.all), each containing up to 60 min of data. The therein included time, motion and position data (WGS84, geographic) was measured by the Kongsberg Seapath system on board. During the acquisition the echo sounder was monitored as well as settings and filter adjusted according to the environment. The transit speed was up to 13 knots. The swath opening angle was set to 70° resulting in a swath width of about 15 km in 3,000 m water depth. Further, high density and dual swath mode were used resulting in 2 x 432 beams per ping. As the data was collected during transit, no specific surveys were performed. No sound velocity profiles (SVPs) were measured during the cruise. In the beginning of data acquisition, an SVP from a previous cruise was used. On the 04.02.2019, a synthetic SVP extracted from he World Ocean Atlas 2009 from NOAA (Levitus, 2013) using the software "Sound Speed Manager" (developed by the UNH Center for Coastal and Ocean Mapping and NOAA Coast Survey Development Laboratory (CSDL)) was applied in the MBES acquisition software SIS. The SVP data is not part of this submission but can be extracted from the *.all files.
    Keywords: Bathymetry; Binary Object; Binary Object (File Size); Binary Object (Media Type); Comment; Data file recording distance; Data file recording duration; DATE/TIME; ELEVATION; Event label; Extracted from file; Extracted with MB-System; File content; KEM122; Kongsberg datagram raw file name; KONGSBERG EM122; LATITUDE; LONGITUDE; Multibeam Echosounder; Number of pings; OceanLight; Ship speed; SO267/2; SO267/2_0_Underway-1; Sonne_2; Start of data file, depth; Start of data file, heading; Start of data file recording, date/time; Start of data file recording, latitude; Start of data file recording, longitude; Stop of data file, depth; Stop of data file, heading; Stop of data file recording, date/time; Stop of data file recording, latitude; Stop of data file recording, longitude
    Type: Dataset
    Format: text/tab-separated-values, 4608 data points
    Location Call Number Expected Availability
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  • 4
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    HafenCity University Hamburg
    In:  EPIC3HafenCity University Hamburg, 107 p.
    Publication Date: 2016-12-12
    Description: Vast areas of the Yermak Plateau have been affected by major glaciations during the Quaternary. Our understanding of the timing and dimensions of the marine-based ice sheets in the Svalbard-Barents Sea region during the Quaternary today is still limited. The main objective of this thesis is to improve the knowledge in the glacial history on the aspect of when and how the Arctic Ocean with the Svalbard-Barents Sea Ice Sheets has been reconnected. Multibeam swath bathymetry, high-resolution subbottom acoustic profiling and sediment coring can be combined to identify ice-grounding events in the past. A case study is presented here for the Yermak Plateau and northern Svalbard margin located between 79° and 83°N and 2° and 16°E. The geophysical datasets were acquired from research vessels, Polarstern (PS) and Maria S. Merian (MSM), during the expeditions PS92 and MSM31. Three types of subglacial features were detected from bathymetric mapping, in the form of ice- produced mega-scale glacial lineations, iceberg plowmarks of various dimensions and a grounding-zone wedge. The acoustic stratigraphy showed four acoustic facies: the first with undulating laminated upper surface and very little acoustic penetration below, indicative of highly disturbed sediments by ice action; a second with a thick laminated strata over acoustically transparent lenses, resulting from debris flow; a third with well-developed stratification produced by sedimentation under calm condition, often laminated with parallel to sub-parallel internal reflectors; and the last with well-stratified strata also produced by sedimentation under calm environment but present over a strong and undulating reflector at the base. Mega-scale lineations are attributed to be formed during the Saalian with the grounding of large ice shelf fragments exiting towards the Fram Strait. Quasi-linear huge plowmarks are likely to be formed either by multiple keels of a single megaberg or by keels of several icebergs that are trapped together within multi-year sea ice whereas, fresh-looking and irregular smaller plowmarks might have been formed by single keels of icebergs. The grounding-zone wedge, at its maximum position at the shelf edge, represents the maximum extent of the Late Weichselian ice sheet extended from Svalbard-Barents Sea. The geotechnical properties of the sediments from gravity cores recovered, did not possess any qualities of overconsolidation but showed a hint of slightly higher consolidation at certain core depths, implying the sediment erosion by grounded ice shelves or icebergs. Undisturbed lineations but rather faint ones due to younger sediments on top at the southernmost Yermak Plateau and an acoustic reflector at the sediment depth of 15-20 m below sea floor at the plateau crest suggest that there might not be any connection between the Arctic Ocean and Svalbard-Barents Sea Ice Sheet through Yermak Plateau after MIS19/20 boundary.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Thesis , notRev
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  • 5
    ISSN: 1476-5535
    Keywords: Yeast ; Oleaginous ; Rhodotorula glutinis ; Lipid ; Fat ; Molasses ; Fed batch
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: Summary Rhodotorula glutinis is known to produce fat when cultivated under nitrogen-limiting conditions. Economically, molasses is an ideal substrate, however, due to the presence of nitrogen in molasses, the lipid yield obtained is much lower than that obtained from glucose or sucrose. Higher yields were obtained using molasses in a fed batch fermentation supplemented with glucose or sucrose during the lipid accumulation phase. The fatty acids profile of the lipids thus produced, using a very simple and economical medium, was similar to that obtained from glucose and sucrose.
    Type of Medium: Electronic Resource
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  • 6
    Publication Date: 2013-03-08
    Print ISSN: 1438-4957
    Electronic ISSN: 1611-8227
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Published by Springer
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  • 7
    Publication Date: 2012-11-17
    Print ISSN: 1438-4957
    Electronic ISSN: 1611-8227
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Published by Springer
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  • 8
    Publication Date: 2010-01-22
    Print ISSN: 0175-7598
    Electronic ISSN: 1432-0614
    Topics: Biology , Process Engineering, Biotechnology, Nutrition Technology
    Published by Springer
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  • 9
    Publication Date: 2015-11-01
    Print ISSN: 0960-1481
    Electronic ISSN: 1879-0682
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Published by Elsevier
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  • 10
    Publication Date: 2014-08-21
    Print ISSN: 2190-6815
    Electronic ISSN: 2190-6823
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Published by Springer
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