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HPCN Europe 2000 Proceedings of the 8th International Conference on High-Performance Computing and Networking
A dynamic earth observation system
Parallel Computing - Special issue: High performance computing with geographical data
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ITCC '04 Proceedings of the International Conference on Information Technology: Coding and Computing (ITCC'04) Volume 2 - Volume 2
eMicrob: a grid-based spatial epidemiology application
ICCS'05 Proceedings of the 5th international conference on Computational Science - Volume Part III
Data-Parallel method for georeferencing of MODIS level 1b data using grid computing
ICCS'05 Proceedings of the 5th international conference on Computational Science - Volume Part III
A remote sensing application workflow and its implementation in remote sensing service grid node
ICCS'06 Proceedings of the 6th international conference on Computational Science - Volume Part I
Remote sensing information processing grid node with loose-coupling parallel structure
ICCS'06 Proceedings of the 6th international conference on Computational Science - Volume Part I
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The signal at the top of the atmosphere will certainly contain information about both the surface and the atmosphere. To derive the geophysical parameters from satellites remote sensing images, the atmospheric effects must be decoupled. Aerosol Optical Thickness (AOT), an important aerosol optical property, should be correctly determined to remove the atmospheric effect. The retrieval process is great time-consuming and the EMS memory required is too large for a personal computing to run efficiently. Therefore, to facilitate the process smoothly, SYNTAM model is used to retrieve AOT over a wide range of land including China and one European area from MODIS data on the Remote Sensing Information Service Grid Node (RSIN, http://www.tgp.ac.cn) deployed at Institute of Remote Sensing Applications, Chinese Academy of Sciences. AOT retrieval results show that the RSIN Grid service is high efficient and has the potential to be applied to the remote sensing parameter inversion.