Title | ||
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Tibetan Plateau permafrost evolution monitoring using C- and L-band spaceborne SAR Interferometry |
Abstract | ||
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In this study, the permafrost evolution in Tibetan Plateau (TP) was monitored through the detection of the overlaying active layer motion using space-observed Persistent Scatterers SAR Interferometry (PSI). Two bands SAR data, 38 scenes of C-band Envisat ASAR and 19 scenes of L-band ALOS PALSAR data were employed. The small baseline strategy was introduced to minimize the seasonal decorrelation effect. The derived surface motions (primarily in the range of -20 mm/yr to 20 mm/yr) over Beiluhe section, Qinghai, China indicated that human activities aggravate the surface motions, e.g. the construction and operation of Qinghai-Tibet Railway (QTR). SAR interferometry-derived results were firstly cross-compared, and then further validated by the precise leveling data. |
Year | DOI | Venue |
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2012 | 10.1109/IGARSS.2012.6351139 | IGARSS |
Keywords | Field | DocType |
geophysical techniques,synthetic aperture radar,beiluhe section,surface motions,c-band envisat asar data,l-band spaceborne sar interferometry,china,l-band alos palsar data,active layer motion,permafrost,small baseline strategy,tibetan plateau permafrost evolution monitoring,persistent scatterers sar interferometry,precise leveling data,geophysical image processing,qinghai-tibet railway,ice,c-band spaceborne sar interferometry,small baseline,space-observed persistent scatterer sar interferometry,radar interferometry,human activities,seasonal decorrelation effect,spaceborne radar,tibetan plateau,l band,surface topography,coherence,interferometry | Plateau,Spaceborne radar,Active layer,Decorrelation,L band,Computer science,Synthetic aperture radar,Remote sensing,Interferometry,Geodesy,Permafrost | Conference |
ISSN | ISBN | Citations |
2153-6996 E-ISBN : 978-1-4673-1158-8 | 978-1-4673-1158-8 | 0 |
PageRank | References | Authors |
0.34 | 2 | 2 |
Name | Order | Citations | PageRank |
---|---|---|---|
Fulong Chen | 1 | 12 | 6.51 |
Hui Lin | 2 | 459 | 64.06 |