PPT-Radiative transfer simulations of the
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ATR42 and Falcon 20 SW and LW radiation profiles above the ENEA Lampedusa supersite during the ChArMEx ADRIMED SOP1a campaign Daniela Meloni Laboratory for Earth
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Radiative transfer simulations of the: Transcript
ATR42 and Falcon 20 SW and LW radiation profiles above the ENEA Lampedusa supersite during the ChArMEx ADRIMED SOP1a campaign Daniela Meloni Laboratory for Earth Observations and Analyses ENEA. R adiative - , Page 1 Radiative and Radiative - Convecti ve Equilibrium Introduction The energy balance of the Earth’ ytem i quite intricate with numerou Numerical sagging Focusing on the radiative heat transfer modeling B. Le Corre L. Bau, A. Collin , Y. Meshaka , G. Jeandel International Congress on Glass Prague - July 2013 FEDER FEDER What is 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. . Sanshiro. Shibata (Konan Univ.). Collaborator: . Nozomu. . Tominaga. (Konan Univ., IPMU). Introduction. Models for the prompt emission. Internal shock model. A standard scenario for a long time.. 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. ATR-42 . SW and LW irradiance profiles above. Lampedusa Island. Daniela Meloni. with . contributions. from:. ChArMEx. /ADRIMED . SOP1a meeting, . Paris, 5-6 . June. 2014. ATR-42 . flights. . above. 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.. 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. 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?.
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