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| 01611nam 2200325za 4500 |
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| 001 | 9.837241 |
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| 003 | CaOODSP |
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| 005 | 20221107151106 |
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| 007 | cr ||||||||||| |
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| 008 | 170525s2016 onca ob f000 0 eng d |
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| 040 | |aCaOODSP|beng |
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| 041 | |aeng|bfre |
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| 043 | |an-cn---|an-cn-nu|an-cn-yk |
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| 086 | 1 |aM103-3/24-2016E-PDF |
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| 100 | 1 |aShort, N. H., |d1975- |
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| 245 | 10|aEvaluation of multi-dimensional DInSAR for permafrost environments |h[electronic resource] / |cN.H. Short. |
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| 260 | |a[Ottawa] : |bNatural Resources Canada, |c2016. |
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| 300 | |a20 p. : |bcol. ill. |
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| 490 | 1 |aOpen file ; |v24 |
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| 504 | |aIncludes bibliographical references. |
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| 520 | |a"Satellite interferometric radar (InSAR) is emerging as an excellent tool to monitor terrain stability. This report evaluates the newest techniques of two- and three-dimensional InSAR, applied specifically in permafrost terrain. Three-dimensional InSAR, as implemented here, is seen to be less reliable than two-dimensional InSAR. Two-dimensional InSAR provides valuable information about slope processes and the nature of terrain movement”--Executive summary, p. 2. |
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| 546 | |aIncludes summary in French. |
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| 692 | 07|2gccst|aPermafrost |
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| 692 | 07|2gccst|aGeophysics |
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| 692 | 07|2gccst|aRemote sensing |
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| 692 | 07|2gccst|aSatellite imagery |
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| 710 | 1 |aCanada. |bNatural Resources Canada. |
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| 710 | 2 |aGeomatics Canada. |
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| 830 | #0|aOpen file (Geomatics Canada)|v24.|w(CaOODSP)9.821474 |
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| 856 | 40|qPDF|s58.50 MB|uhttps://publications.gc.ca/collections/collection_2017/rncan-nrcan/M103-3/M103-3-24-2016-eng.pdf |
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