From Australian Oceans Data Network

Satellite-derived high-resolution sea-ice motion in the Southern Ocean, 2015-2019 - ESA Sentinel1 Satellite Data

Created 13/03/2025

Updated 13/03/2025

Sea-ice motion derived from two (partially) overlapping ESA Sentinel1 [S1]A or B scenes. Satellites S1A/B carry C-band (5.405 GHz) Synthetic Aperture Radar [SAR] sensors. For this data set images from the Extra Wide swath (EW) mode of operation (swath width 410 km) have been used. EW mode data are available as a medium-resolution ground range detected (GRD) product, i.e., resolution of 93 × 87 m and pixel size 40 × 40 m. Approximately two-thirds of the EW mode data recorded over the Antarctic area are dual-polarisation (HH + HV) products. The remainder are mainly single-polarisation (HH) products. For further detail, see ESA's Copernicus web portal. Ice motion is derived from suitable SAR image pairs with sufficient spatial overlap but relatively short time separation, i.e. ideally 6 days or less. Image-crosscorrelation analysis is employed to identify displacement vectors within the image pair.

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Field Value
Title Satellite-derived high-resolution sea-ice motion in the Southern Ocean, 2015-2019 - ESA Sentinel1 Satellite Data
Language eng
Licence notspecified
Landing Page https://devweb.dga.links.com.au/data/dataset/3c8cb956-38ca-42d5-87d0-4fad03c500fa
Contact Point
CSIRO Oceans & Atmosphere
metadata@aad.gov.au
Reference Period 01/01/2015 - 31/12/2019
Geospatial Coverage {"type": "Polygon", "coordinates": [[[-180.0, -80.0], [180.0, -80.0], [180.0, -55.0], [-180.0, -55.0], [-180.0, -80.0]]]}
Data Portal data.gov.au

Data Source

This dataset was originally found on data.gov.au "Satellite-derived high-resolution sea-ice motion in the Southern Ocean, 2015-2019 - ESA Sentinel1 Satellite Data". Please visit the source to access the original metadata of the dataset:
https://devweb.dga.links.com.au/data/dataset/satellite-derived-high-resolution-sea-ice-motion-in-the-southern-ocean-2015-2019-esa-sentinel1-

No duplicate datasets found.