Abstract
Persistent scatterer interferometry (PSI) makes use of points with temporally coherent phase to achieve high accuracy measurements. However, in non-urban environments, the PS density is generally very low and distributed scatterers (DS) are dominant. Thus, it is difficult to monitor crustal deformation in a mountainous area where many active faults/volcanoes are located. To improve the spatial density of the measurement points, the use of DS, in which the phase quality should be comparable to PS, is indispensable.
| Original language | English |
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| Number of pages | 1 |
| Publication status | Published - 2015 |
| Event | Japan Geoscience Union Meeting 2015 - Makuhari, Japan Duration: 24 May 2015 → 28 May 2018 https://confit.atlas.jp/guide/event/jpgu2015/top |
Conference
| Conference | Japan Geoscience Union Meeting 2015 |
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| Abbreviated title | JPGU 2015 |
| Country/Territory | Japan |
| City | Makuhari |
| Period | 24/05/15 → 28/05/18 |
| Internet address |
Keywords
- Phase linking
- Distributed scatterers
- InSAR time series analysis
- Persistent scatterer interferometry (PSI)