Satellite-derived high-resolution sea-ice motion, 2007-2011 - Envisat Satellite Data

• Other Authors: AADC (owner), AADC, DATA OFFICER (distributor), AADC, DATA OFFICER (custodian), AU/AADC > Australian Antarctic Data Centre, Australia (hasAssociationWith), Australian Antarctic Data Centre (publisher), Australian Antarctic Division (sponsor), HEIL, PETRA (collaborator), HEIL, PETRA (hasPrincipalInvestigator), HEIL, PETRA (author), HYLAND, GLENN (collaborator), HYLAND, GLENN (hasPrincipalInvestigator), HYLAND, GLENN (author), Heil, P. and Hyland, G. (originator)
• Format: Dataset
• Language: unknown
• Published: Australian Ocean Data Network
• Subjects: oceans; EARTH SCIENCE > OCEANS > SEA ICE > SEA ICE MOTION; CRYOSPHERE > IMAGE CROSSCORRELATION; SAR > Synthetic Aperture Radar; ENVISAT > Environmental Satellite; ACE/CRC; AMD/AU; AMD; CEOS; GEOGRAPHIC REGION > POLAR; OCEAN > SOUTHERN OCEAN; CONTINENT > ANTARCTICA; Antarc*; Antarctic; Antarctica; Sea ice; Southern Ocean
• Online Access: https://researchdata.edu.au/satellite-derived-high-satellite-data/2816427

Progress Code: onGoing Statement: The geolocation accuracy of the relevant Envisat ASAR products have an absolute error of up to 750 m (10 pixels) due to inaccuracies in the positional specifications in the SAR image headers. However, as the sea-ice motion applies a differencing technique, the absolute errors offset each other and derived ice displacement are in the order of 1.5pixels width or 115m. Purpose The purpose of this dataset was to create a NetCDF-format database of high-resolution(:SAR) Antarctic sea-ice motion vectors. Envisat was was launched on 01/03/2002, by ESA and operated until 08/04/2012. It provided suitable imagery for the austral winters (May - November) of 2007 to 2011. Envisat caried a C-band (5.33 GHz; wavelength ∼ 5.6 cm) Advanced Synthetic Aperture Radar [ASAR], capable to acquire data in multiple modes (image, alternating polarization, wave, ScanSAR (wide swath), and ScanSAR (global monitoring)) at various incidence angles and in several polarisations. Of ASAR's five distinct measurement modes, the following two modes may be used to derive sea-ice motion from overlapping images in our project: 1. ASAR Wide Swath Mode -- 400 km by 400 km wide swath image. Spatial resolution of approximately 150 m by 150 m for nominal product. VV or HH polarization. 2. ASAR Global Monitoring Mode -- Spatial resolution of approximately 1000 m in azimuth by 1000 m in range for nominal product. Up to a full orbit of coverage. HH or VV polarization. For further detail, see ESA's Copernicus web portal. Sea-ice motion is derived from suitable SAR image pairs with sufficient spatial overlap but relatively short time separation, i.e. ideally 6days or less. Image-crosscorrelation analysis is employed to identify displacement vectors within the image pair. The underlying processing and analysis is part of the (mostly) automated IMCORR [IMageCORRelation] Processing, Analysis and Display System [IPADS]. This study uses C-band (HH polarisation) ASAR scenes, with an image pixel size of 75 m across a 405 km ...