PPT-Intrinsic surface albedo describes the characteristic hemispherical reflectance of the

Author : alexa-scheidler | Published Date : 2018-10-30

Near nadir imagers do not provide the multiangle observations necessary to capture the multiangle reflective character described by the surface BRDF Therefore the

Presentation Embed Code

Download Presentation

Download Presentation The PPT/PDF document "Intrinsic surface albedo describes the c..." is the property of its rightful owner. Permission is granted to download and print the materials on this website for personal, non-commercial use only, and to display it on your personal computer provided you do not modify the materials and that you retain all copyright notices contained in the materials. By downloading content from our website, you accept the terms of this agreement.

Intrinsic surface albedo describes the characteristic hemispherical reflectance of the: Transcript

Near nadir imagers do not provide the multiangle observations necessary to capture the multiangle reflective character described by the surface BRDF Therefore the Landsat albedo algorithm couples atmospherically corrected 30m Landsat . Louisiana Moon Glint—Preliminary Review. 12 January 2014. Steve Miller. CSU/CIRA. Moon Glint Angle. Ocean Surface. θ. < ~30˚. θ. . G. lint Angle. θ. < ~10˚.  When the Moon-Satellite geometry is favorable, there is the possibility for brightening of the water surface from lunar reflectance, just as in the day.. Steve Miller . (. Steven.Miller@colostate.edu. ). Updated: 27 July 2012. Lunar Spectral Irradiance Model. Miller and Turner, 2009. IEEE Trans. . Geosci. . Rem. Sens., 47(7), 2316-2329. . A . lunar irradiance prediction model . ?. Rebekka. . Posselt. , Aku Riihelä. With support from: . Richard Müller, Jörg Trentmann. Outline. CM SAF Event Week, Surface radiation retrieval. 2. PART I. Solar radiation (SIS, SID). MagicSol. Principles & Practice of Remote . Sensing. EM . Radiation (. ii). Dr. Mathias (Mat) Disney. UCL Geography. Office: 113, Pearson Building. Tel: 7679 0592. Email: mdisney@ucl.geog.ac.uk. http://www2.geog.ucl.ac.uk/~mdisney/teaching/GEOGG141/GEOGG141.html. at UNR. 29 July 2013. By Pat Arnott. Computer to read spectrometer data.. Spectrometers are at . Dambar’s. left hand.. Irradiance sensor. (looks up). Radiance sensor. (looks down). Bryan steadies the albedo measuring device. Intercomparisons. Lessons Learned. K. Thome. 1. , N. Fox. 2. 1. NASA/GSFC , . 2. National Physical Laboratory. Summarize lessons learned during joint field campaigns to . Tuz. . Golu. , Turkey. 10 countries and 13 organizations. Led by – Pat McCormick and Alex Gilerson. May 7, 2015. Algorithm Development Outline. Theme I - Climate. Snow Cover & Properties Retrieval From Satellite Microwave. Near-real-time Cloud Detection From Weather Satellites . Anat. . Levin, . Daniel . Glasner. , . Ying . Xiong. , . Fredo. . Durand, . Bill Freeman, . Wojciech. . Matusik. , Todd . Zickler. .. Weizmann Institute, Harvard University, MIT. 2. A. ppearance fabrication. Eric . Vermote . et . al.. NASA . Goddard Space Flight Center Code . 619. Eric.f.vermote@nasa.gov. . . LCLUC Spring Meeting, April 12-14, Hilton, Rockville, MD. Home . page: . http://modis-sr.ltdri.org. (from: METRIC: Mapping Evapotranspiration at high Resolution using Internalized Calibration). University of Idaho, Kimberly, Idaho. University of Nebraska-Lincoln. Landsat – Polar Orbiting. A new image each 16 days. AERosol. AND CLOUD . RETRIEVALS OVER SNOW. Kokhanovsky. VITROCISET Belgium SPRL, . Bratustrasse. 7, 64289 Darmstadt, Germany. a.kokhanovsky@vitrocisetbelgium.com. . CLOUD. AEROSOL. CONCLUSIONS. CLOUDS. . Albedo increases due to more ice coverage to something like about 0.35 which is then equivalent to a 6% change (3 % change in mean geometric distance from the Sun). Qualitative Albedo Feedback loop:. MODEL DEVELOPMENT AND FUTURE RESEARCH. BEN SUMLIN AND PHILIP BURT. ATMS 746/360. Kaokoland, Namibia. Photo by Michael . Poliza. .. OUTLINE. METHODS. RESULTS AND MODEL DEVELOPMENT. FUTURE WORK. METHODS: DEFINITIONS. The characteristic roots of the (. p×p. ) matrix . A. are the solutions of the following determinant equation: . Laplace expansion. is used to write the characteristic polynomial as. :. Since (.

Download Document

Here is the link to download the presentation.
"Intrinsic surface albedo describes the characteristic hemispherical reflectance of the"The content belongs to its owner. You may download and print it for personal use, without modification, and keep all copyright notices. By downloading, you agree to these terms.