Application of Persistent Scatterer Interferometry (PSI) in monitoring slope movements in Nainital, Uttarakhand Lesser Himalaya, India

Author:

Yhokha Akano,Goswami Pradeep K,Chang Chung-Pai,Yen Jiun-Yee,Ching Kuo-En,Aruche K Manini

Funder

Ministry of Science and Technology, Taiwan

Department of Science & Technology, Government of India

European Space Agency

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference41 articles.

1. Adam N, Kampes B and Eineder M 2005 Development of a scientific permanent scatterer system: Modifications for mixed ERS/ENVISAT time series; ESA Spec. Publ.  SP-572 457–465.

2. Amelung F, Jónsson S, Zebker H and Segall P 2000 Widespread uplift and ‘trapdoor’ faulting on Galapagos volcanoes observed with radar interferometry; Nature  407 (6807) 993–996.

3. Anbalagan R, Kumar R, Lakshmanan K, Parida S and Neethu S 2015 Landslide hazard zonation mapping using frequency ratio and fuzzy logic approach, a case study of Lachung Valley, Sikkim; Geoenviron. Disasters  2(6), https://doi.org/10.1186/s40677-014-0009-y .

4. Auden J B 1934 The geology of the Krol belt; Geol. Surv. India Rec.  71 357–454.

5. Auden J B 1942 Geological report on the hill side of Nainital; Unpubl. Rep., Geol. Surv. India, Kolkata.

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