PPT-INVESTIGATION OF SURFACE ALBEDO AND FORCINGS DUE TO EVAPORATIONAL COOLING

Author : arya | Published Date : 2023-10-27

MODEL DEVELOPMENT AND FUTURE RESEARCH BEN SUMLIN AND PHILIP BURT ATMS 746360 Kaokoland Namibia Photo by Michael Poliza OUTLINE METHODS RESULTS AND MODEL DEVELOPMENT

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INVESTIGATION OF SURFACE ALBEDO AND FORCINGS DUE TO EVAPORATIONAL COOLING: Transcript

MODEL DEVELOPMENT AND FUTURE RESEARCH BEN SUMLIN AND PHILIP BURT ATMS 746360 Kaokoland Namibia Photo by Michael Poliza OUTLINE METHODS RESULTS AND MODEL DEVELOPMENT FUTURE WORK METHODS DEFINITIONS. M. W. Frierson. Department of Atmospheric Sciences. Day 3: 04/06/2010. ATM S 111, Global Warming: Understanding the Forecast. Climate . Forcings. . vs. Climate Feedbacks. Climate . forcings. : . Things that change global temperatures directly. ?. 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. 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. and other adventures in chemistry-climate interactions. Loretta J. Mickley. Pattanun. . Achakulwisut. , . Becky. Alexander, Tom . Breider. , . Bryan . Duncan. , . Rynda. . Hudman. , Daniel Jacob. ,. . 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 . 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 . Sulagna. Ray. . Program in Atmospheric . & Oceanic . Sciences. Princeton . University, Princeton, . NJ, USA. Andrew Wittenberg. Geophysical Fluid Dynamics Laboratory/NOAA . Princeton, NJ, USA. . . 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:. 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. 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. 5.1 Cumulative . heating or Cooling. The capping inversion traps in the ABL any . heating and . water evaporation from the surface. As a result. , heat . accumulates within the ABL during day, . or whenever . ?. 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. Sam Coakley. Advisor: Travis Miles, Ph.D.. Tropical cyclone impact on US. https://. www.ncdc.noaa.gov. /billions/summary-stats. Total cost 1980-2019: $954.4B. Total deaths 1980-2019: 6,507. Tropical cyclone impact on US.

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