Temporal change in the extinction coefficient of snow on the Greenland ice sheet from an analysis of Seasat and Geosat altimeter data
- 1 January 1996
- journal article
- Published by Institute of Electrical and Electronics Engineers (IEEE) in IEEE Transactions on Geoscience and Remote Sensing
- Vol. 34 (5) , 1066-1073
- https://doi.org/10.1109/36.536522
Abstract
No abstract availableKeywords
This publication has 22 references indexed in Scilit:
- Detection of volume scattering effects in beamwidth limited altimetry dataPublished by Institute of Electrical and Electronics Engineers (IEEE) ,2002
- A waveform model for surface and volume scattering from ice and snowIEEE Transactions on Geoscience and Remote Sensing, 1996
- Greenland ice-sheet surface properties observed by the Seasat-A scatterometer at enhanced resolutionJournal of Glaciology, 1994
- The depth of penetration in Antarctic firn at 10 GHzIEEE Transactions on Geoscience and Remote Sensing, 1993
- A surface and volume scattering retracking algorithm for ice sheet satellite altimetryIEEE Transactions on Geoscience and Remote Sensing, 1993
- Active and passive microwave signatures of Antarctic firn by means of field measurements and satellite dataAnnals of Glaciology, 1993
- Geographic and seasonal variations in the surface properties of the ice sheets by satellite-radar altimetryJournal of Glaciology, 1993
- A combined surface-and volume-scattering model for ice-sheet radar altimetryJournal of Glaciology, 1993
- A model of satellite radar altimeter return from ice sheetsInternational Journal of Remote Sensing, 1988
- Radiative Transfer Modeling of Microwave Emission and Dependence on Firn PropertiesAnnals of Glaciology, 1982