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In this study, Synthetic Aperture Radar (SAR) images from Envisat ASAR C-band descending Track 176 and ALOS PALSAR L-band ascending Track 500 are processed to generate the coseismic deformation caused by the earthquake.
Range offset and azimuth offset derived from descending track 23 (a, b), ascending track 130 (c, d), descending track 29 (e, f).
Blue and red rectangles show the observation footprint of PALSAR-2 data for ascending and descending track, respectively.
The maximal deformation region of the coseismic field obtained from the descending track data is fundamentally consistent with that of the subsidence region obtained from the ascending track data.
Currently, there are 32 GPS satellites in operation and the period of a GPS satellite is approximately 24 h, which results in 64 available tracks (ascending and descending track) per day.
Data from descending track 28 and ascending track 142 (Table 2) were processed using the GMTSAR software (Sandwell et al. 2011) with the application of a 100-m Gaussian filter.
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a Post-seismic image correlation map of the descending tracks.
The co-seismic deformation field of the Hatanbulag earthquake was observed using ASAR C-band data acquired from the descending tracks.
Points were acquired approximately 172 meters apart along the satellite's flight path, which included both ascending and descending tracks on an orbit with a 94° declination [12].
Points were acquired approximately 172 meters apart along the satellite's flight path, which included both ascending and descending tracks on an orbit with a 94° declination [ 12].
A dynamic boundary layer based neural network quasi-sliding mode control law is proposed to track a desired descending path.
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