1. RECENT EXPERIENCES UTILIZING TERRASAR-X FOR THE MONITORING OF NATURAL DISASTERS IN DIFFERENT PARTS OF THE WORLD July 29, 2011 Yuki Okajima Kazuo Yoshikawa Takashi Shibayama PASCO CORPORATION
2.
3.
4.
5. 2. Overview of TerraSAR-X ・ X-band SAR satellite launched by DLR in 2007 ・ Highest spatial resolution of 1m. ・ Repeat cycle and revisit time are 11 days and about 3 days respectively. ・ Suitable for emergency observations thanks to cloud free SAR sensor’s characteristic. Imaging mode SpotLight StripMap ScanSAR Specifications
6. 3. Emergency Response to Natural Disasters 2008 Jan Monitoring of GLOF (Glacial Lake Outburst Flood) in the Himalayas Feb Eruption of Sakurajima volcano(Showa crater), Kagoshima Prefecture May Damage interpretations around Kitagawa, the Great Sichuan Earthquake Jun Changes in Iwate-Miyagi inland earthquake slip Aug Heavy rain flooded area estimation Aichi (town district Hishiike Kouda) Aug Overflow of Kosi River in Nepal 2009 May Disaster in Northern Brazil (near the Parnaíba River) May Estimation of flood disasters due to cyclone “Aila” in Bangladesh 2010 Jan Estimation of earthquake victims in Haiti Mar ~ Apr Iceland volcano monitoring 2011 Jan M onitoring eruptions of Shinmoedake volcano in Kirishima Feb Earthquake monitoring in Christchurch, New Zealand Mar Providing information about the Great East Japan Earthquake Major Initiatives
7.
8. 4.2 Detection of Collapsed Buildings References 1) Masashi MATSUOKA and Fumio YAMAZAKI: APPLICATION OF A METHODOLOGY FOR DETECTING BUILDING-DAMAGE AREA TO RECENT EARTHQUAKES USING SATELLITE SAR INTENSITY IMAGERIES AND ITS VALIDATION, J. Struct. Constr. Eng., AIJ, No. 558, 139-147, Aug., 2002 Diagram of Using Intensity Imagery - Before Earthquake Backscaterring of microwave radiated from a satellite is strong due to dual-bounce scattering between roads and buildings. - After Earthquake Backscattering becomes weak because microwave spreads toward various directions due to collapsed buildings. ⇒ Collapsed buildings are detectable by the difference of backscattering coefficient.
9. 4.3 Detection of Collapsed Buildings (cont.) [ TerraSAR-X ] [Optical Image] Oct. 13, 2009 Oct. 11, 2009 Jan. 20, 2010 Jan. 13, 2010 (c) Infoterra GmbH, Distribution [PASCO] (c) Infoterra GmbH, Distribution [PASCO] (c) GeoEye (c) GeoEye Weak backscattering appear dark in the image. After After Before Before
14. 5.3 Data Acquisition and Analysis Okinawa Tokyo ④ Obser vation ⑤ downlink ⑥ transfer ⑦ Analysis Sendai City Tokyo
15.
16.
17. 5.6 Estimated Inundation Areas with a Post-Disaster Image Conversion of DN value into backscattering coefficient Areas more than a certain elevation to be masked to reduce commission errors caused by radar shadow. Define a threshold to determine the possible water areas (underlying conditions, such as incidence angles, taken into account) Inundation areas where the value is lower than the threshold are extracted and change maps are created. - TerraSAR-X Observations - Inundation Area Detection Method 37.3° HH StripMap Descending 4 April 2011 37.3° HH StripMap Descending 24 March 2011 37.3° HH StripMap Descending 13 March 2011 Inc. Angle Polarization Acq. Mode Orbit Direction Acq. Date (JST)
19. 5.8 Estimated Inundation Areas with a Post-Disaster Image Water-pumping effort Field survey for ground truth Our analyses were used by River Bureau of Land, Infrastructure and Transportation Ministry to plan drain pump installation and confirm the outcome of their pumping efforts.
20. 6. Summary ・ We have 22 emergency responses for major natural disasters, including Haiti Earthquake and The Great East Japan Earthquake in 4 years since the launch of TerraSAR-X. ・ Our analyses and maps of the disasters were provided to the national and local government and utilized for the damage assessment and recovery efforts. ・ We keep our disaster monitoring system strengthened and distribute information and analyses of major disasters in order to further contribute to protect people’s life and safety .