PPT-Atmospheric

circulation of h ot Jupiters on highly eccentric orbits Tiffany Kataria 1 Adam Showman 1 Nikole Lewis 1 Jonathan Fortney 2 Mark Marley 3 Richard Freedman 3 September 15 . Atmospheric Research 51 1999 245265 The behavior of total lightning activity in severe Florida thunderstorms Earle Williams a Bob Boldi Anne Matlin Mark Weber Steve Hodanish Dave Sharp Steve Goodman Ravi Raghavan :. Radiosondes, Dropsondes and . Driftsondes. Kate Young . & . Junhong. . Wang. kbeierle. @. ucar.edu. NCAR Earth Observing Laboratory. National Center for . Atmospheric Research. Weather/Climate. with . climate variability and change . Seminar in Atmospheric Science, EESC G9910. Diagnosing ENSO from atmospheric composition (ozone measured from space). Ziemke. et al. ., 2010; . Oman et al. ., 2011. Naba. K . Mondal. Tata Institute of Fundamental Research. Mumbai 400005, India. Brief History. Atmospheric neutrino experiments study neutrinos produced by cosmic ray interactions in the atmosphere.. Atmospheric . Corrections. Atmospheric Effects on EMR. Kodiak Island, AK – Volcanic ash and clouds (MODIS image). Learning Objectives. What are the main ways that the atmosphere affects light traveling through it?. Evaluation of moisture characteristics associated with heavy daily rainfall. Dependence on region/season. Progressing to hourly rain gauge data and additional precursor diagnostics (e.g. wet bulb & dew point temperature). Atmospheric pressure. Pressure. Why do predators often have . SHARP . teeth and claws?. Why does wearing skis stop . you from . SINKING. into the snow? . IGCSE Pressure . Relate pressure to force and area, using appropriate examples . (work funded through the Great Lakes Restoration Initiative). Dr. Mark Cohen. NOAA Air Resources Laboratory (ARL). College Park, MD, USA. Briefing Slides for GLRI Monthly Call. January 9, 2013. Atmospheric deposition is believed to be the largest . and Climate (Chap 6). Atmospheric General Circulation. Also: Global or planetary circulation. . The general circulation (GC) of the atmosphere is the totality of motions that characterize the . large scale. Preprocessin. g: Atmospheric Correction. . “Correction” for Sun Angle Differences.  is the solar zenith angle and varies as a function of latitude, day of year, and time of day. Radiance is proportional to cos . :. Radiosondes, Dropsondes and Driftsondes. Kate Young & Junhong Wang. NCAR Earth Observing Laboratory. National Center for . Atmospheric Research. Weather/Climate. Societal Impacts. Pollution/Air Chemistry. Mr. Ross Brown. Brooklyn School for Law and Technology. How do we understand the weather?. 4 January 2015. Do now: Take out your Reference Tables.. What is the . dewpoint. when the dry-bulb temperature is 24°C and the wet-bulb temperature is 15°C. Graduate Research Assistant with Dylan Millet: 2008 9.13.2017. Think and Do 9.132017. Tape your paper to a board. Get watercolor paints, paper towel, and watercolor container from the back. Think about your favorite place. Start looking up images of that place.