PPT-How to retrieve surface radiation and surface albedo from s

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. Radiation - Emission. thermal radiation . is the emission of electromagnetic waves when matter is at an . absolute temperature greater than 0 K. emission is due to the . oscillations and transitions of the many electrons . Structure and Composition. Concepts to learn. The general concepts found in this section are:. The earth's atmosphere is a very . thin layer . wrapped around a very large planet.. Based on . temperature. Dongdong. Wang, Tao He. Yi Zhang, Meredith Brown. Prof. Shunlin Liang. University of Maryland. May 21 2015. 1. Producing Incident Shortwave Radiation and . Photosynthetically. Active Radiation Products Over Land Surfaces . 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. . Nick Hoekzema . Oliver Stenzel. Lena Petrova. Wojtek. . Markiewicz. Maya . Garcia-Comas. Nick Thomas . Klaus Gwinner . Ai . Inada. . Optical depth from shadows in orbiter images of Mars. . the optical depth . How does heat energy get from the Sun to the Earth?. There are no particles between the Sun and the Earth so it CANNOT travel by conduction or by convection. . ?. RADIATION. How can we relate our new understanding to the greenhouse effect?. Near nadir imagers do not provide the multi-angle observations necessary to capture the multi-angle reflective character described by the surface BRDF. Therefore, the Landsat albedo algorithm couples atmospherically corrected 30m Landsat . . 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:. Sept 19, 2015 in Price George’s County, MD.. What is the reason for the contrails?. E. xample on integrating . information . from class. .. How . to determine the length . of . a day. ?. First refresher on the concept of solar zenith angle and its determination.. UV. /Visible Tropospheric Ozone Retrievals using GOME. -2 Data. . Xiong Liu, Peter . Zoogman. Kelly Chance, Caroline . Nowlan. xliu@. cfa.harvard.edu. . 3. rd. TEMPO Science Team Meeting. Huntsville, . Earth’s Surface. Atmosphere. Solar Incident. Reflected by Atmosphere. Reflected by Surface. Simplified (isotropic) shortwave radiation model. S = incident. R = cloud. reflection. A = absorption. 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. Surface albedo. NDVI. Remotely sensed . information on surface . albedo . and . NDVI. . is used . in climate modeling and research. .. Above parameters . and surface . temperature. and . radiative. ?. 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.