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Accurate knowledge of the Antarctic ice sheet mass balance plays an important role on the global sea level change. Here two-pass differential InSAR (DInSAR) technique is applied for tidal signal modeling underneath the Sulzberger ice shelf, West Antarctica. The fine resolution DEM over grounded ice and ice shelf, obtained by combining ERS-1/2 tandem InSAR and ICESat laser altimetry, has been used to correct the topography phase from interferograms, resulting in a more accurate time series of vertical deformation measurements. In this study, it is demonstrated for the first time, that observable tidal constituents can be estimated underneath an ice shelf (ice tongue) using an InSAR time series. In particular, it is shown that the time series of observed tidal differences from InSAR agrees well with a number of global/regional ocean tide models such as NAO.99b, TPXO.6.2, GOT00.2, CATS02.01, and FES2004 with the regional model, CATS02.01, having the best agreement. The technique developed here can be applied to other regions where tide modeling is poor in accuracy and resolution.
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Department of Civil Engineering and Environmental SciencesKorea Military AcademyP.O. Box 77-2 Gongneung Dong, Nowon Gu, Seoul, Koreashark@kma.ac.kr2001-2006 Ph. D., Ohio State University, Columbus, Ohio, U.S.A.1994-1995 M.S., Yonsei University, Seoul, Korea1988-1992 B.S., Korea Military Academy, Seoul, Korea
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- PublisherVDM Verlag Dr. Müller
- Publication date2009
- ISBN 10 3639156102
- ISBN 13 9783639156102
- BindingPaperback
- Number of pages116
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DEM GENERATION and OCEAN TIDE MODELING using InSAR: Theory and Application
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DEM GENERATION and OCEAN TIDE MODELING using InSAR
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Book Description Taschenbuch. Condition: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -Accurate knowledge of the Antarctic ice sheet mass balance plays an important role on the global sea level change. Here two-pass differential InSAR (DInSAR) technique is applied for tidal signal modeling underneath the Sulzberger ice shelf, West Antarctica. The fine resolution DEM over grounded ice and ice shelf, obtained by combining ERS-1/2 tandem InSAR and ICESat laser altimetry, has been used to correct the topography phase from interferograms, resulting in a more accurate time series of vertical deformation measurements. In this study, it is demonstrated for the first time, that observable tidal constituents can be estimated underneath an ice shelf (ice tongue) using an InSAR time series. In particular, it is shown that the time series of observed tidal differences from InSAR agrees well with a number of global/regional ocean tide models such as NAO.99b, TPXO.6.2, GOT00.2, CATS02.01, and FES2004 with the regional model, CATS02.01, having the best agreement. The technique developed here can be applied to other regions where tide modeling is poor in accuracy and resolution. 116 pp. Englisch. Seller Inventory # 9783639156102
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DEM GENERATION and OCEAN TIDE MODELING using InSAR Theory and Application
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DEM GENERATION and OCEAN TIDE MODELING using InSAR Theory and Application
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DEM GENERATION and OCEAN TIDE MODELING using InSAR : Theory and Application
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Book Description Taschenbuch. Condition: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - Accurate knowledge of the Antarctic ice sheet mass balance plays an important role on the global sea level change. Here two-pass differential InSAR (DInSAR) technique is applied for tidal signal modeling underneath the Sulzberger ice shelf, West Antarctica. The fine resolution DEM over grounded ice and ice shelf, obtained by combining ERS-1/2 tandem InSAR and ICESat laser altimetry, has been used to correct the topography phase from interferograms, resulting in a more accurate time series of vertical deformation measurements. In this study, it is demonstrated for the first time, that observable tidal constituents can be estimated underneath an ice shelf (ice tongue) using an InSAR time series. In particular, it is shown that the time series of observed tidal differences from InSAR agrees well with a number of global/regional ocean tide models such as NAO.99b, TPXO.6.2, GOT00.2, CATS02.01, and FES2004 with the regional model, CATS02.01, having the best agreement. The technique developed here can be applied to other regions where tide modeling is poor in accuracy and resolution. Seller Inventory # 9783639156102
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