PPT-RETRIEVING BRDF OF DESERT USING TIME SERIES OF MODIS IMAGER

Author : pasty-toler | Published Date : 2016-03-03

Haixia Huang Bo Zhong Qinhuo Liu and Lin Sun Presented by Bo Zhong bzhong1gmailcom Institute of Remote Sensing Applications Chinese Academy of Sciences IGRSS

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RETRIEVING BRDF OF DESERT USING TIME SERIES OF MODIS IMAGER: Transcript

Haixia Huang Bo Zhong Qinhuo Liu and Lin Sun Presented by Bo Zhong bzhong1gmailcom Institute of Remote Sensing Applications Chinese Academy of Sciences IGRSS 2011 Vancouver . Similar to the current GOES imager ABI will be used for a wide range of qualitative and quantitative weather oceanographic climate and environmental applications ABI will offer more spectral bands higher spatial resolution and faster imaging than th Ke Chen Charly Collin Ajit Hakke-Patil Sumanta Pattanaik. Overview. Introduction and motivation. BRDF = surface BRDF + subsurface BRDF . [. Hanrahan. and Krueger 1993]. Subsurface BRDFs are directionally dependent. Fifth Meeting of the Science Advisory Committee. 18-20 November, 2009. Matt Smith, Kevin Fuell, Geoffrey Stano. National Space Science and Technology Center, Huntsville, AL. Background. GOES-R Proving Grounds Activities. . F. red Huemmrich, UMBC/GSFC . John Gamon, University of Alberta. We want to develop methods to use optical signals to estimate ecosystem carbon exchange. Examine the relationships between ecosystem production (GEP) and spectral reflectance. Linear & non-linear models. Dr. Mathias (Mat) Disney. UCL Geography. Office: 113, Pearson Building. Tel: 7670 0592. Email: . mdisney@ucl.geog.ac.uk. www.geog.ucl.ac.uk. /~. mdisney. Linear models and inversion. Inversion . I. : . linear approaches. Dr. Mathias (Mat) Disney. UCL Geography. Office: 113, Pearson Building. Tel: 7670 0592. Email: . mdisney@ucl.geog.ac.uk. www.geog.ucl.ac.uk. /~. mdisney. Linear models and inversion. Adam Brady. 2. 3. 4. 5. ?. 6. 7. 8. 9. ?. 10. 11. 12. …. 13. ?. Materials are More Than Color. When light strikes a surface, it scatters. Realistic rendering depends on how this . reflectance . is . Adam Brady. 2. 3. 4. 5. ?. 6. 7. 8. 9. ?. 10. 11. 12. …. 13. ?. Materials are More Than Color. When light strikes a surface, it scatters. Realistic rendering depends on how this . reflectance . is . Charly Collin – . Sumanta. . Pattanaik. – Patrick . LiKamWa. Kadi Bouatouch. Painted materials. Painted materials. Painted materials. Painted materials. Our goal. Base layer. Binder thickness. Robert C. Levy (NASA-GSFC). robert.c.levy@nasa.gov. Shana . Mattoo. , Leigh . Munchak. . and Richard . Kleidman. . (SSAI/GSFC). Lorraine Remer. . (UMBC/JCET), . Falguni. . Patadia. (MSU/GSFC), . . Robert . Holz. , Virginie . Buchard. , . Arlindo. Da Silva, Ed . Hyer. , and Jeff Reid. Summary. Terra provides the only morning orbit with a modern imager with no current replacement until METOP-SG in 2025. recent development and perspective. Hankui Zhang, David Roy and Crystal . Schaaf. . Feb 8, 2023. Landsat Science Team meeting, Reno, Nevada. Outline. Existing . c. -factor method – using global averaged MODIS BRDF parameters . Collection 6 ‘e-Deep Blue’ aerosol products. Andrew M. Sayer, N. Christina Hsu (PI). , Corey Bettenhausen, Nick Carletta, Jaehwa Lee, Colin Seftor, Jeremy Warner. Past team members: Ritesh Gautam, Jingfeng Huang, Myeong-Jae Jeong, Becky Limbacher, Clare Salustro. Collection 6 e-Deep Blue/Dark Target comparison and ‘merged’ aerosol products. 1. Images from NASA Earth Observatory, . http://earthobservatory.nasa.gov/Features/Aerosols/. Deep Blue group: . N. Christina Hsu (PI), .

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