Stef Lhermitte; Bert Wouters (2020): Data from Cryosat-2 satellite showing elevation change over Pine Island Glacier and Thwaites Glacier. Version 1. 4TU.ResearchData. dataset. https://doi.org/10.4121/uuid:da761d33-2e37-41e9-af6b-cd4b8d588e55

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Categories

• Physical Geography and Environmental Geoscience
• Other Earth Sciences

Keywords

Antarctica Cryosat-2 Geomatic Engineering

Geolocation

Time coverage

2010-2017

Licence

CC BY-SA 4.0

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by Stef Lhermitte , Bert Wouters

Rates of elevation change for 2010-2017 derived from interferometric measurements from Cryosat-2. Elevation change was derived from interferometric measurements from Cryosat-2. ESA L1b waveforms retrieved by the satellite in its SARIn (synthetic aperture radar interferometry) mode were processed following the swath processing approach of Gray et al(2013). The resulting dense set of time-dependent elevation measurements was used to derive elevation changes in a Eulerian framework at a 500 m resolution following the method presented in Wouters et al. (2015).

History

• 2020-08-21 first online, published, posted

Publisher

4TU.ResearchData

Format

media types: application/zip, image/tiff

Funding

• Nederlandse Organisatie voor Wetenschappelijk Onderzoek, 016.Vidi.171.065
• Nederlandse Organisatie voor Wetenschappelijk Onderzoek, ALWGO.2018.043

Organizations

TU Delft, Faculty of Civil Engineering and Geosciences, Department of Geoscience & Remote Sensing