Abstract | ||
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An inversion algorithm is presented to reconstruct ice growth under thermal cycling conditions by using time-series active microwave measurements. The method uses a direct scattering model consisting of a one-dimensional thermodynamic model of saline ice growth that includes thermal interactions with the atmosphere, and a physical-based electromagnetic model that accounts for thermal and electromagnetic properties of ice and combined volume and surface scattering effects. The crucial part of the inversion algorithm is to use sequentially measured radar data together with the direct scattering model to retrieve sea ice parameters. The algorithm is applied to CRRELEX 94 data and successfully reconstruct the evolution of ice growth under a thermal cycling environment |
Year | DOI | Venue |
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1998 | 10.1109/IGARSS.1998.703796 | Geoscience and Remote Sensing Symposium Proceedings, 1998. IGARSS '98. 1998 IEEE International |
Keywords | Field | DocType |
backscatter,oceanographic techniques,radar cross-sections,radar theory,remote sensing by radar,sea ice,active microwave measurements,direct scattering model,diurnal thermal cycling conditions,ice growth,inversion algorithm,measurement technique,model,ocean,one-dimensional thermodynamic model,physical-based electromagnetic model,radar remote sensing,radar scattering,retrieval,saline ice growth,saline ice thickness,theory,inverse problem,inverse scattering,indexing terms,thermodynamics,time series data,inverse problems,atmospheric modeling,time series,electromagnetic modeling,thermal cycling,diurnal cycle,polarization | Radar,Atmosphere,Sea ice,Thermal,Backscatter,Remote sensing,Temperature cycling,Scattering,Mathematics,Inverse scattering problem | Journal |
Volume | Issue | ISBN |
4 | 5 | 0-7803-4403-0 |
Citations | PageRank | References |
1 | 0.36 | 2 |
Authors | ||
5 |
Name | Order | Citations | PageRank |
---|---|---|---|
Shih-En Shih | 1 | 1 | 0.36 |
Kung-Hau Ding | 2 | 199 | 36.10 |
Jin Au Kong | 3 | 255 | 42.06 |
Nghiem, S.V. | 4 | 9 | 3.64 |
A. K. Jordan | 5 | 20 | 5.79 |