2007
DOI: 10.1029/2007gl029745
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Interferogram formation in the presence of complex and large deformation

Abstract: Sierra Negra volcano in Isabela island, Galápagos, erupted from October 22 to October 30 in 2005. During the 8 days of eruption, the center of Sierra Negra's caldera subsided about 5.4 meters. Three hours prior to the onset of the eruption, an earthquake (Mw 5.4) occurred, near the caldera. Because of the large and complex phase gradient due to the huge subsidence and the earthquake, it is difficult to form an interferogram inside the caldera that spans the eruption. The deformation is so large and spatially v… Show more

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Cited by 70 publications
(63 citation statements)
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(15 reference statements)
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“…Theoretically, the range displacement map from the pixel offset technique is expected to contain the same information as the differential interferogram [24]. In order to quantitatively evaluate the combination of the two techniques, the differences between LOS displacements of ten points in Area 4 derived from DInSAR processing in a time span of 22 days and offset tracking processing in a time span of 110 days are calculated in Table 4.…”
Section: Offset Tracking Results Between Sar Acquisitionsmentioning
confidence: 99%
See 1 more Smart Citation
“…Theoretically, the range displacement map from the pixel offset technique is expected to contain the same information as the differential interferogram [24]. In order to quantitatively evaluate the combination of the two techniques, the differences between LOS displacements of ten points in Area 4 derived from DInSAR processing in a time span of 22 days and offset tracking processing in a time span of 110 days are calculated in Table 4.…”
Section: Offset Tracking Results Between Sar Acquisitionsmentioning
confidence: 99%
“…At the end, the final range and azimuth offsets can be estimated by measuring the row and column offsets between two acquisitions. During the processing, various parameters, such as the cross-correlation window size and oversampling factor, should be carefully evaluated to adjust to the size of deformation features and SAR image pixel size [24].…”
Section: Amplitude Based: Pixel Offset Techniquementioning
confidence: 99%
“…In the last decade two-pass InSAR has been extensively applied to volcanoes. Studies include observations of inflation and deflation of inferred magma chambers, e.g., [14]- [17], sill and dike intrusion, e.g., [18]- [20], faulting, e.g., [21] and eruption, e.g., [22], [23]. In the early days of InSAR, it was generally only possible to capture an entire eruption in an interferogram, except in the case of long-lived eruptions, like Kilauea.…”
Section: B Two-pass Insarmentioning
confidence: 99%
“…The general OT procedure first removes the global component using a bilinear equation [42]. Different strategies (e.g., high-pass filtering [41,43]) can then be applied to mitigate the error offsets in the local component. Finally, the remaining offsets are transformed into surface deformation, in accordance with the spatial resolution of the SAR images.…”
Section: Introductionmentioning
confidence: 99%