PPT-Radiative

Processes in Astrophysics Prof Wladimir Lyra Live Oak 1119G Office Hours Mon 4pm5pm Class hours MonWed 2pm315pm Wiens displacement law Luminosity is a function of radius and a strong function of temperature. R adiative - , Page 1 Radiative and Radiative - Convecti ve Equilibrium Introduction The energy balance of the Earth’ ytem i quite intricate with numerou Astrophysical and Laboratory Plasmas. Lecture 1: Temperature-Density regime. . Many physical processes. . Focus on . Atomic+Plasma. interactions. . Atomic properties are . intrinsic. , . independent of external factors (temp, den, etc.). tropical cyclones. Robert Fovell and . Yizhe. Peggy Bu. University of California, Los Angeles. rfovell@ucla.edu. 1. Thanks to. : . Greg . Thompson, NCAR/. DTC; Ligia . Bernardet. and Mrinal . Biswas. Corrections. Peter Schnatz. Stony Brook University. Radiative. Events. In scattering experiments, a photon may be emitted by a charged particle due to . Bremsstrahlung. radiation.. This type of radiation is due to the deceleration of a charged particle as it approaches the . SPECIFICS. OF STUDY. FINDINGS. Kohler,. 193. 6 (“The nucleus in and the growth of hygroscopic droplets”). Evaporate. 2kg of hoar-frost and . determined . Cl. content. ; used optics to . measure droplet size. 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. Zack . Pecenak. Evan Greer. Changfu. Li. Climate Change - . Implications. Problem. Ongoing . climate . change. Solution:. Climate engineering?. Solar Radiation Management. Increasing the albedo of snow or clouds is a form of SRM. the . Radiative Effects . of . Black Carbon Internal Mixing. Charles Li. Group Meeting Presentation. October 1, 2014. Group Meeting 10/1/14. 1. Black Carbon (BC) Direct Radiative Forcing:. +0.71 W m. imbalance . 1985-2012. Richard P. Allan. , . Chunlei. . Liu (University of Reading/NCAS Climate); Norman Loeb (NASA Langley); Matt Palmer (Met Office). r.p.allan@reading.ac.uk. @. rpallanuk. GEWEX 7. Feedbacks. . “Our understanding of the climate system is complicated by . feedbacks. that either . amplify. or . damp. perturbations…”. Feedbacks. . Describe the inter-related growth or decay of the components of a system.. Christopher . Melhauser. and . Fuqing. Zhang. The Pennsylvania State University. Department of Meteorology. Group Meeting – April 11, 2013. Focus. How does the diurnal radiation cycle impact the . of. aerosols over clouds . and. clear skies determined using CALIPSO . and. the A-Train. Robert Wood. , . Duli. . Chand. , Tad Anderson. University of Washington. VOCALS RF04, 21 November 2008. Effect of aerosol layer on TOA SW radiation. Contents Radiative Forcing of Climate Change Kerry Emanuel. Massachusetts Institute of Technology. Several Possibly Inter-related Enigmas of the Tropical Atmosphere. Why does moist convection often cluster?. What determines the number of tropical cyclones on the planet?.