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Onboard Radar Processing Concepts for the DESDynI Mission Yunling Lou, Steve Chien, Duane Clark, Joshua Doubleday, Ron Muellerschoen, and Charles Wang Jet Propulsion Laboratory California Institute of Technology Pasadena, California IGARSS 2010 26-30 July, 2010 Honolulu, Hawaii
Agenda ,[object Object],[object Object],[object Object],[object Object],[object Object]
DESDynI Mission Radar Measurements Overview July 2010 Biomass Canopy Height 8 Tbit onboard storage 1 Gbps TDRSS link ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Simard et al (2006,2008)   ,[object Object],Polarimetric SAR ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Pass 2 Pass 1 Repeat Pass InSAR 580 to 1160 Mbps 2000 Mbps Raw Data Rate
Potential Benefits of Onboard Processing Technology for DESDynI Mission July 2010 ,[object Object],Solid Earth Ecosystem Structure Cryospheric Science Potential Onboard  Products Compressed interferogram* Forest biomass Soil moisture Vegetation classification Land use classification Sea ice classification Freeze/thaw maps Potential Downlink  Data Volume  Reduction Factor 10, but only for limited scenes that can be stored  on board  1000 1000 for sea ice  (non-interferometric) Potential Disaster  Response Products Earthquake Flooding Lava flow Forest fuel load Hurricane damage in forest Flooding Ice melting Ship channel freeze/thawing
Other Potential Advantages of Onboard Processing for Earth Science Radar Missions July 2010
Proposed Onboard Processing Scenario for DESDynI Mission’s Radar Instrument July 2010 ,[object Object],[object Object],[object Object],[object Object],Onboard Processor Analyze and detect features Reprioritize downlink if needed Modify data acquisitions if needed DESDynI Onboard Autonomy Software Form SAR image Generate onboard product? Compress SAR image in preparation for calibration and  post-processing on the ground  Generate low resolution product (e.g. sea ice classification at 100 m resolution) Downlink data volume reduced by a factor of 1000 Downlink data volume reduced by a factor of 10 Ground Receiving Station No Yes
Example Mission Scenario with Autonomous Sciencecraft Experiment Image taken by Spacecraft Event Detection No event Detected: Delete Image Event Detected Onboard Science Analysis Track a wide range of science events – floods, volcanoes, cryosphere, clouds,… Key Insight:  No need to replicate ground science analysis – just detect activity ASE uses state of the art Machine Learning to detect events in the presence of noise
High Level Architecture of the  Onboard Processor ,[object Object],[object Object],[object Object],July 2010 Product generation ≤  2.5 Gbps PMC cards for high  speed data transfer Fiber Pre-processor (Micro-processor) FPGA Processor 1 FPGA Processor 2 Post-processor (Micro-processor) Ethernet Raw radar data Control interface Control processor SAR image formation & Image compression Custom boards cPCI Chassis RocketIO interfaes
Approach to Onboard Product Development ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],July 2010
Onboard Product Examples: Forest Fire Extent July 2010 LHH ,  LHV ,  LVV Tracking forest fire extent with UAVSAR L-band polarimetric data products Fire scars
Onboard Product Examples: Forest Fuel Load July 2010 LHH ,  LHV ,  LVV UAVSAR data over Kings Canyon
July 2010 Low Fuel Load Forests Distribution of 1-hr Branch Fuel Load ,[object Object],[object Object],Onboard Product Examples: UAVSAR Fuel Products
July 2010 Medium Fuel Load Forests Distribution of 10-hr Branch Fuel Load Onboard Product Examples: UAVSAR Fuel Products
July 2010 High Fuel Load Forests Distribution of 100-hr Branch Fuel Load Onboard Product Examples: UAVSAR Fuel Products
Onboard Product Examples: Earthquake Damage Assessment July 2010 By comparing two post-earthquake amplitude images, we are able to identify old features (green) that have been removed (perhaps damaged buildings) and new features (red) that have been built (perhaps tent cities) over a two-week period. Amplitude Change Detection  with UAVSAR’s 16-day Repeat Pass Data over Port Au Prince Airport, Haiti  Jan 27, 2010 Feb 13, 2010
Onboard Product Examples: Glacier Melting July 2010 L-band polarmetric image of the Kangerlugssuaq ice fjord in Eastern Greenland.  The grounding line of the glacier is easily identifiable in the image LHH ,  LHV ,  LVV Grounding line
Input Data: Training, Cross Validation & Evaluation SVM Output Visual Imagery Low statistical correlation with input data (noisy), high visual feature correlation April 22, 2006 Courtesy Google Earth Labels for training and cross validation statistics.  National Land Cover Data 2001, condensed to 4 coarse classes.  Polarimetric data, incidence angle, etc: training and final classification input.  Support Vector Machine Onboard Product Examples: Vegetation Classification with Support Vector Machine water dense veg. light  veg. bare/ urban
Future Work ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],July 2010

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FR1.L09.2 - ONBOARD RADAR PROCESSING CONCEPTS FOR THE DESDYNI MISSION

  • 1. Onboard Radar Processing Concepts for the DESDynI Mission Yunling Lou, Steve Chien, Duane Clark, Joshua Doubleday, Ron Muellerschoen, and Charles Wang Jet Propulsion Laboratory California Institute of Technology Pasadena, California IGARSS 2010 26-30 July, 2010 Honolulu, Hawaii
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  • 5. Other Potential Advantages of Onboard Processing for Earth Science Radar Missions July 2010
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  • 7. Example Mission Scenario with Autonomous Sciencecraft Experiment Image taken by Spacecraft Event Detection No event Detected: Delete Image Event Detected Onboard Science Analysis Track a wide range of science events – floods, volcanoes, cryosphere, clouds,… Key Insight: No need to replicate ground science analysis – just detect activity ASE uses state of the art Machine Learning to detect events in the presence of noise
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  • 10. Onboard Product Examples: Forest Fire Extent July 2010 LHH , LHV , LVV Tracking forest fire extent with UAVSAR L-band polarimetric data products Fire scars
  • 11. Onboard Product Examples: Forest Fuel Load July 2010 LHH , LHV , LVV UAVSAR data over Kings Canyon
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  • 13. July 2010 Medium Fuel Load Forests Distribution of 10-hr Branch Fuel Load Onboard Product Examples: UAVSAR Fuel Products
  • 14. July 2010 High Fuel Load Forests Distribution of 100-hr Branch Fuel Load Onboard Product Examples: UAVSAR Fuel Products
  • 15. Onboard Product Examples: Earthquake Damage Assessment July 2010 By comparing two post-earthquake amplitude images, we are able to identify old features (green) that have been removed (perhaps damaged buildings) and new features (red) that have been built (perhaps tent cities) over a two-week period. Amplitude Change Detection with UAVSAR’s 16-day Repeat Pass Data over Port Au Prince Airport, Haiti Jan 27, 2010 Feb 13, 2010
  • 16. Onboard Product Examples: Glacier Melting July 2010 L-band polarmetric image of the Kangerlugssuaq ice fjord in Eastern Greenland. The grounding line of the glacier is easily identifiable in the image LHH , LHV , LVV Grounding line
  • 17. Input Data: Training, Cross Validation & Evaluation SVM Output Visual Imagery Low statistical correlation with input data (noisy), high visual feature correlation April 22, 2006 Courtesy Google Earth Labels for training and cross validation statistics. National Land Cover Data 2001, condensed to 4 coarse classes. Polarimetric data, incidence angle, etc: training and final classification input. Support Vector Machine Onboard Product Examples: Vegetation Classification with Support Vector Machine water dense veg. light veg. bare/ urban
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Hinweis der Redaktion

  1. 1-hour fuel: fallen needle, leaf needle, and small twigs – source of surface fire
  2. 10-hour fuel load: small branches and woody stems. Due to their resistance to drying and greater heat capacity, 10-hour fuels often do not combust in low-intensity surface fires. When moisture is low, however, 10-hour fuels can carry hot fires and help ignite larger (100- and 1000-hour) fuels. Ten-hour fuels are readily consumed when fuel moistures are low.
  3. Larger downed woody debris is common 100-hour forest fuels. These fuels take longer to dry, deterring their consumption under most conditions. Likewise, 100-hour fuels are slow to gain moisture, so they can combust after prolonged drought, even with recent precipitation. When 100-hour fuels ignite they can burn for hours, in mixtures of flaming and smoldering combustion. Decay of 100-hour fuels can alter their response and makes them combust more readily than intact fuels.
  4. NLCD: water(black), dense veg(dark gray), low veg(light gray), bare/urban(white) Training Samples: ~6000 randomly chosen samples (pixels) from many images in the area. Selected image is just one example image (500x500 pixels). SVM: multi-class strategy: one-vs-one; gaussian radial-basis kernel Inputs: hh, hv, vv (all in db scale, topography 'removed'), incidence angle, local incidence, 7x7 pixel average, 7x7 gaussian weighted average, 7x7 variance, hhvv phase, sin(phase), sin(local inc), sin(flat inc), rvi: 8hv / (hh+vv+2hv)