PPT-Radiometric Calibration of Current and Future Ocean Color S

Author : phoebe-click | Published Date : 2016-06-26

R Foster S Hlaing A Gilerson S Ahmed Robert Foster ME LEED AP Optical Remote Sensing Laboratory The City College of New York CoRP Science Symposium September 910

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Radiometric Calibration of Current and Future Ocean Color S: Transcript

R Foster S Hlaing A Gilerson S Ahmed Robert Foster ME LEED AP Optical Remote Sensing Laboratory The City College of New York CoRP Science Symposium September 910 2014 Introduction amp Motivation. Vocabulary. Ocean Current. Coriolis Effect. Rip Current. Upwelling. Major Ocean Currents. An . Ocean Current. is a large volume of water flowing in a certain direction.. Wind-driven currents are called surface currents.. The atmosphere is evil. Clouds. Humidity. Gasses. Pollution/haze. Different sun angles. clouds. Block pretty much everything in the V-MIR.. Shadows.. Annoying as heck.. Only solution, radar data. humidity. A. Hawkins. K. . Langhoff. J. . Shevlin. Jacksonville High School. As You Come In…. How old would you say this object is? Explain in a couple of sentences your reasoning for selecting the age that you did.. G. . Jaross. 1. , . C. . . Seftor. 2. , . G. Taha. 3. , . J. . . Warner. 2. , . G. . Chen. 2. , . Z. . Chen. 2. , . A. . Vasilkov. 2. , . L. . Moy. 2. , . M. . Kowitt. 2. , P. . . Bhartia. 1. 1. NASA GSFC, . Sky . Calibration. Aquarius: D. M. Le Vine. MWR: J. C. Gallo. Definition. Cold Sky Calibration: The observatory rotates 180 deg around its pitch axis from the normal Earth-viewing mode to a “sky” viewing mode. temperature difference. P. J. Minnett, A. Chambers & N. . Perlin. Rosenstiel . School of Marine and Atmospheric Science, . University . of Miami, . USA. Earth Observation for Ocean-Atmosphere Interactions Science Frascati, October 2014. What is a current?. 1. An Ocean Current . is a directed, continuous movement of ocean water generated by various forces.. 2. Currents are caused by various factors:. Temperature. Different salinity levels. SRJC, Physics 43, Spring 2011. Aaron Krive, Kevin . Chee. History. Radioactive decay of Uranium was discovered in 1896 by French Scientist Henry . Becquere. .. Possibility of dating using radioactivity was proposed by British scientist Lord Rutherford in 1905.. LDCM Science Team Meeting. USGS EROS. August 16-18, 2011. Dennis Helder, Dave Aaron. And the IP Lab crew. Outline. Interpolation: What has been done to calibrate the Landsat archive?. Extrapolation: How is calibration going to extend to the LDCM era?. SRJC, Physics 43, Spring 2011. Aaron Krive, Kevin . Chee. History. Radioactive decay of Uranium was discovered in 1896 by French Scientist Henry . Becquere. .. Possibility of dating using radioactivity was proposed by British scientist Lord Rutherford in 1905.. USGS EROS. rmorfitt@usgs.gov. Work Performed by. SGT: Mike Choate, . Mark . Lubke, . Obaidul. . Haque. , . Ajit. . Sampath. , Jim . Storey. , . and . Esad. . Micijevic. SDSU: . Dennis . Helder. , and Ashish Shrestha . Fig 1 Principle of operation Bragg EffectThe Bragg Effect describes the amplification effectof a back-scattered electromagnetic wave havingtwice the wavelength as the ocean wave eg for a 30MHz radar s A: Sunlight – Producers require sunlight for photosynthesis. Ocean life is determined by many factors:. B: Temperature – most animals live near the surface where it is warmer. Ocean life is determined by many factors:. S. ensor . I. n. T. ercomparison. and . U. ncertainty assessment for . O. cean . C. olour. . R. adiometry (. INSITU. -. OCR. ). working . toward. high accuracy . and consistency of . essential climate .

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