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| 02277nam 2200421zi 4500 |
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001 | 9.916796 |
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003 | CaOODSP |
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005 | 20230131161140 |
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006 | m o d f |
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007 | cr cn||||||||| |
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008 | 221031t20222022onca ob f000 0 eng d |
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020 | |a9780660460697 |
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040 | |aCaOODSP|beng|erda|cCaOODSP |
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043 | |an-cn-bc|an-cn-ab|an-cn-nu |
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086 | 1 |aM183-2/8928E-PDF |
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100 | 1 |aChʻoe, Pyŏng-hŭi, |eauthor. |
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245 | 10|aRADARSAT Constellation Mission (RCM) InSAR preliminary observations of slope movements in British Columbia, Alberta, and Nunavut / |cB-H. Choe, A. Blais-Stevens, S. Samsonov, and J. Dudley. |
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264 | 1|a[Ottawa] : |bGeological Survey of Canada, |c2022. |
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264 | 4|c©2022 |
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300 | |a1 online resource (15 pages) : |billustrations. |
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336 | |atext|btxt|2rdacontent |
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337 | |acomputer|bc|2rdamedia |
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338 | |aonline resource|bcr|2rdacarrier |
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490 | 1 |aOpen file, |x2816-7155 ; |v8928 |
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504 | |aIncludes bibliographical references (page 14). |
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520 | |a"This report provides preliminary results observed from new RCM InSAR data acquired over 21 sites in British Columbia (BC), Alberta (AB), and Nunavut (NU) from April 2020, by comparing them with RADARSAT-2 and Sentinel-1 observations in some cases. Based on the preliminary observations, the advantages and limitations of RCM InSAR for landslide monitoring and some guidelines for future operational plans are suggested"--Introduction, page 1. |
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650 | 0|aLandslide hazard analysis|zBritish Columbia. |
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650 | 0|aLandslide hazard analysis|zAlberta. |
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650 | 0|aLandslide hazard analysis|zNunavut. |
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650 | 0|aSynthetic aperture radar|xImage quality. |
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650 | 6|aRisques de glissement de terrain|zColombie-Britannique. |
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650 | 6|aRisques de glissement de terrain|zAlberta. |
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650 | 6|aRisques de glissement de terrain|zNunavut. |
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650 | 6|aRadar à synthèse d'ouverture|xQualité de l'image. |
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710 | 2 |aGeological Survey of Canada, |eissuing body. |
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830 | #0|aOpen file (Geological Survey of Canada)|x2816-7155 ; |v8928.|w(CaOODSP)9.506878 |
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856 | 40|qPDF|s14.21 MB|uhttps://publications.gc.ca/collections/collection_2023/rncan-nrcan/m183-2/M183-2-8928-eng.pdf |
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856 | 40|qHTML|sN/A|uhttps://doi.org/10.4095/331099 |
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