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Observing 2006-2010 ground deformations of Merapi volcano (Indonesia) using ALOS/PALSAR and ASTER TIR data
Saepuloh A.a,b, Urai M.a, Widiwijayanti C., Aisyah N.d
a Advanced Industrial Science and Technology (AIST), Japan
b Department of Geology, Bandung Institute of Technology (ITB), Indonesia
c Earth Observatory of Singapore, Nanyang Technological University (NTU), Singapore
d Center for Volcanology and Geological Hazard Mitigation (CVGHM), Indonesia
[vc_row][vc_column][vc_row_inner][vc_column_inner][vc_separator css=”.vc_custom_1624529070653{padding-top: 30px !important;padding-bottom: 30px !important;}”][/vc_column_inner][/vc_row_inner][vc_row_inner layout=”boxed”][vc_column_inner width=”3/4″ css=”.vc_custom_1624695412187{border-right-width: 1px !important;border-right-color: #dddddd !important;border-right-style: solid !important;border-radius: 1px !important;}”][vc_empty_space][megatron_heading title=”Abstract” size=”size-sm” text_align=”text-left”][vc_column_text]Understanding precursory signal leading to a large and explosive eruption, such as Merapi eruption in 2010, is the key to a successful hazard assessment in the future. Towards resolution of this problem, time series of Differential Interferometric SAR (D-InSAR) of ALOS/PALSAR data together with thermal radiance at summit area were analyzed to characterize magmatic process. The D-InSAR could detect deformation changes in between two eruption episodes of Merapi in 2006 and 2010. The maximum uplifting rate ∼0.7 mm/day is observed twice: two years and one month before eruption in October 26, 2011. The first uplift is related to magma ascent and the later is precursory to an imminent eruption. Thermal radiance of ASTER data not only served as indicator on the arrival of fresh magma near the surface, but also to confirm whether or not the deformation signal is related to the imminent eruption. © 2011 IEEE.[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Author keywords” size=”size-sm” text_align=”text-left”][vc_column_text]ALOS/PALSAR,ASTER,ASTER data,D-inSAR,Deformation signal,Explosive eruption,Ground deformations,Hazard Assessment,Indonesia,Interferometric SAR,Magma ascents,Magmatic process,Merapi volcanos,Mt. Merapi,Precursory signals,Thermal radiance[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Indexed keywords” size=”size-sm” text_align=”text-left”][vc_column_text]ALOS/PALSAR,ASTER,Deformation,Mt. Merapi,Thermal radiance[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Funding details” size=”size-sm” text_align=”text-left”][vc_column_text][/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”DOI” size=”size-sm” text_align=”text-left”][vc_column_text]https://doi.org/10.1109/IGARSS.2011.6049545[/vc_column_text][/vc_column_inner][vc_column_inner width=”1/4″][vc_column_text]Widget Plumx[/vc_column_text][/vc_column_inner][/vc_row_inner][/vc_column][/vc_row][vc_row][vc_column][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][/vc_column][/vc_row]