TU1.L09 - RECENT ADVANCES IN FULLY POLARIMETRIC SPACE-SAR SENSOR DESIGN AND ITS APPLICATIONS
1. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 1 Hawaiian Village, Honolulu, Hawaii, 2010 July 25 – 30 IGARSS10-TU1.L09-3417 Tuesday, 2010 July 27, 8:20 – 10:00 "Recent advances in fully polarimetric Space-SAR sensor design and its applications” Invited Presentation Wolfgang-Martin Boerner University of Illinois at Chicago, Department of Electrical & Computer Engineering, Communications, Sensing & Navigation Laboratory Chicago, IL/USA IEEE International Geosciences& Remote Sensing Symposium
2. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 2 ABSTRACT In this overview, reasons are provided on why we do need to place multi-modal, multi-band single and multiple pass POLinSAR monitoring platforms into air and space. The questions “on what POLinSAR monitoring can provide that POL-SAR and IN-SAR by themselves cannot accomplish” is assessed; whereupon facts and justifications on placing POL-IN-BISAR satellite clusters into space are presented. Reasons for this technology becoming a basic requirement for current, near-future and much more so for future all-day & night year around monitoring of the terrestrial covers are analyzed in view of the un-abating and uncontrollable terrestrial population explosion, which has, does and for ever will result in unavoidable conflicts deteriorating unfortunately at times into terrorism. The pertinent questions on how to reduce the exorbitant cost for initiating this “home-globe security protection” technology are therefore also broached, and the expected benefits are laid out. The pertinent National and International airborne and space borne multi-modal, multi-band SAR remote sensing and security conflict surveillance support agencies are herewith invited for co-sponsoring our proposal, which is timely and fleets of orbiting multi-band space-borne POLinSAR platforms are urgently required.
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4. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 4 Multi-Altitude Near-Range and Remote Sensing in Wide-Area Environmental Surveillance for Real Time Monitoring of the Earth’s Biosphere: for an ecological investigation of the Earth through observation and identification of harmful anthropogenic influences due to the interaction of: OceansAtmosphere/Stratosphere/Mesosphere Biosphere Hydrosphere for an early warning system of natural and man-made environmental catastrophes and to take quick actions to buffer the impact to the catastrophe under the increasing pressures of a relentlessly un-abating population explosion: Severe weather Typhoons Earthquakes Volcanic Eruptions Global Weather Changes Degeneration into steppe Retreating Glaciers Pollution of Ground Water Pollution of Air Destruction of the Biosphere
5. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 5 Hydrologic cycle with volcanologic & seismic activity Volcano eruption with smock Earthquake drop-slip
6. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 6 Pacific and Indian Oceans
7. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 7 Taiwan From BBC news site
8. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 8 The terrestrial tectonology: Alfred Wegener’s tectonic plate theory and the two major seismic belts Belt 2, Circum-Pacific belt
16. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 16 ALOS / PALSAR TerraSAR-X RadarSAT-II Japanese Space Agency (JAXA) German Aerospace Center (DLR) / Astirum Canadian Space Agency (CSA) L-Band (quad), 2006 X-Band (quad), 2007 C-Band (quad), 2007
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18. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 18 ALOS is one of the largest Earth observing satellites ever developed, at 3850 kg. It is in a near-exact 45-day repeat sun-synchronous orbit, 690 km altitude above the equator. The active phased array SAR antenna is obliquely Earth-facing, aligned with the spacecraft velocity vector. The solar array is arranged at right angles to the orbit plane, consistent with the near-mid-day orbit phasing. The X-band down-link must be shared with optical instruments, which constrains SAR operation times.
24. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 24 4-compornent scattering power decomposition algorithm using rotated coherency matrix Rader line of sight Deorientation Rotation of imsge
25. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 25 4-compornent scattering power decomposition algorithm using rotated coherency matrix
26. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 26 4-compornent scattering power decomposition algorithm using rotated coherency matrix
27. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 27 Four-component decomposition New rotated decomposition Scattering power decomposition by rotation of coherency matrix forNiigata City area in Niigata Prefecture of Japan
28. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 28 Sapporo City, Hokkaido Prefecture, Japan (a) Original decomposition (b) Decomposition after T33 rotation (e) Patch C: forest (d) Patch B: oriented urban (c) Patch A: orthogonal urban Deorientation
29. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 29 Decomposed color coded image of Sapporo, Japan
30. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 30 Interest area 3800m 0m Monitoring of ongoing surface deformation along Cheleng-Pu fault Data fusion of DEM and RADARSAT SAR images By CSRSR. Taiwan
35. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 35 Recent electromagnetic signatures associated with the Chi-Chi and Chia-Yi earthquakes of 1999. Three-axes Fluxgate Magnetometer ULF Magnetometric & Electrometric Measurement Arrangement
36. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 36 Recent electromagnetic signatures associated with the Chi-Chi and Chia-Yi earthquakes of 1999. Simplified Schematic of the Site and Equipment Layout
37. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 37 ULF Tectonic & Spherics Signatures at About .1 to 20 Hz
38. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 38 Averaged Tectonic Stress Signatures during Northridge Earthquake
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40. Black circle: Earthquakes M >= 5.0 Earthquakes occurred in six blue circles (except HC, LP) were compared with the anomaly Taiwan
41. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 40 Recent electromagnetic signatures associated with the Chi-Chi and Chia-Yi earthquakes of 1999, May to December in Taiwan The raw data in LY station in March, April May, August, September, October, November and December, 1999.
42. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 41 Brief introduction of DIFF-RP-IN-SAR
43. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 42 Monitoring of ongoing surface deformation along Cheleng-Pu fault
44. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 43 The destruction along the Cheleng-Pu fault caused by the Chi-Chi earthquake of 1999 September 21
45. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 44
46. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 45 1022 EQs 2 earthquakes occurred on 10/22/1999 in Chiayi area Combined surface deformation of the two eqs were observed by SAR Interferometry (Bn=232m) Approx. 2 fringes can be observed from interferogram, representing 5~6cm slant range deformation
47. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 46 The destruction along the Cheleng-Pu fault caused by the Chi-Chi earthquake of 1999 September 21
48. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 47 The destruction along the Cheleng-Pu fault caused by the Chi-Chi earthquake of 1999 September 21
57. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 56 4-compornent scattering power decomposition algorithm using rotated coherency matrix Rader line of sight Deorientation Rotation of imsge
67. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 66 The destruction along the Cheleng-Pu fault caused by the Chi-Chi earthquake of 1999 September 21
86. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 85 South-East Asia
87. Feb 26, 2005 Mw6.7 Kuala Lumpur Mar 28, 2005 Ms8.4 2004 Apr 10, 2005 Ms6.7 Singapore 1907 PADANG 1861 1935 2002 1797 Jakarta 1833 2000 Krakatau A flurry of ruptures have occurred since 2000 WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 86
96. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 95 Krakatau 8/26/1883 Next major eruption within 20 years
97. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 96 Indian Ocean Tsunamis: 1833 & 2004 Hannah Fairfield/The New York Times, Science Section, January 4, 2005
99. Physical interpretation of rain cell signatures Partial backscattering at hydrometeors (precipitation volume) Attenuation of incident wave Received signals A Amplitude B z t B A Backscattered wave (attenuated) (B) Transmited wave Backscattered wave from hydrometeors (A) WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 98
100. Azimuth Range Slant range reflectivity profile („A-scope“) for the rain cell cut from a very recent TerraSAR-X measurement Power [dB] WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 99
119. Venue : Seoul is the capital of Korea and also conveniently located in the middle of several major northeast Asian metropolises. The city is and infinite discoveries with over 600 years history. The ancient capital of an ancient land, Seoul is a city where the traditional and the cutting-edge exist side-by-side in perfect harmony.
125. Submission : Authors are invited to submit two pages abstracts of original contributions in the form of paper summaries. The abstract should concisely describes the objectives, results and conclusions of the original work.
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128. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 119 IGARSS 2011Sendai, JapanIEEE GRSS Japan Chapter1 - 5 August, 2011 http://igarss11.org/ http://www.grss-ieee.org/
129. WIDEBAND INTERFEROMETRIC SENSING AND IMAGING POLARIMETRY 120 FOUNDATIONS AND RELEVANCE OF MODERN EARTH REMOTE SENSING & ITS ACTIVITIES Conclusions: The Electromagnetic Spectrum: A Natural Global Treasure Terrestrial Remote Sensing with PolSAR: The Diagnostics of the Health of the Earth at all weather and volcanic conditions and at day and night