Data from Cryosat-2 satellite showing elevation change over Pine Island Glacier and Thwaites Glacier

Datacite citation style:
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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Dataset
Delft University of Technology logo
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geolocation
Amundsen Sea Embayment
time coverage
2010-2017
licence
cc-by-sa.png logo CC BY-SA 4.0
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

DATA

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