Swath sonar bathymetry during POLARSTERN cruise ARK-XXII/1b (PS70) with links to multibeam raw data files

Multibeam data were measured as part of the project HERMES during R/V Polarstern cruise ARK-XXII/1 (2007-05-29 to 2007-07-25) along transits and survey profiles and partly during stationary work. Data were achieved mainly in the coastal areas of northern Norway, at the Hakon Mosby Mud Volcano at the...

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Bibliographic Details
Main Authors: Klages, Michael, Albrecht, Sebastian, Eisenschmidt, Julia, Schenke, Hans Werner, Gauger, Steffen
Format: Dataset
Language:English
Published: PANGAEA 2011
Subjects:
ARK-XXII/1b
AWI_BPP
Bentho-Pelagic Processes @ AWI
CT
DATE/TIME
HERMES
Hotspot Ecosystem Research on the Margins of European Seas
LATITUDE
LONGITUDE
Norwegian Sea
Polarstern
PS70
PS70/1b-track
Standard for Geospatial Metadata V.2
Swath-mapping system Atlas Hydrosweep DS-2
Underway cruise track measurements
Uniform resource locator/link to image
Uniform resource locator/link to metadata file
Uniform resource locator/link to raw data file
Svalbard
Norway
Floholmen
Arctic
Berichte zur Polar- und Meeresforschung
Northern Norway
Reports on Polar and Marine Research
Sea ice
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.773184
https://doi.org/10.1594/PANGAEA.773184
Description
Summary:Multibeam data were measured as part of the project HERMES during R/V Polarstern cruise ARK-XXII/1 (2007-05-29 to 2007-07-25) along transits and survey profiles and partly during stationary work. Data were achieved mainly in the coastal areas of northern Norway, at the Hakon Mosby Mud Volcano at the continental margin approx. 200 nm off the norwegian coast and the AWI-Hausgarten area approx. 150 nm west of Svalbard. A number of surveys were carried out in the coastal areas of northern Norway (Sula Reef, Roest Reef, Traena area, Floholmen area, Sotbakken area) and around the area of the Hakon Mosby Mud Volcano. The multibeam sonar system Atlas Hydrosweep DS-2 (Atlas Hydrographic, http://www.atlashydro.com) was operated using 59 beams and 90° aperture angle. The refraction correction was achieved using CTD profiles measured during this cruise or, during transits, utilizing the system's own cross fan calibration. The quality of data might be reduced during bad weather periods or adverse sea ice conditions (only in the AWI-Hausgarten area). This dataset contains raw data that are not processed and thus may contain errors and blunders in depth and position.

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