PPT-1 Changes in global net radiative

Author : danika-pritchard | Published Date : 2017-03-28

imbalance 19852012 Richard P Allan Chunlei Liu University of ReadingNCAS Climate Norman Loeb NASA Langley Matt Palmer Met Office rpallanreadingacuk rpallanuk

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1 Changes in global net radiative: Transcript


imbalance 19852012 Richard P Allan Chunlei Liu University of ReadingNCAS Climate Norman Loeb NASA Langley Matt Palmer Met Office rpallanreadingacuk rpallanuk GEWEX 7. R adiative - , Page 1 Radiative and Radiative - Convecti ve Equilibrium Introduction The energy balance of the Earth’ ytem i quite intricate with numerou radiative. forcing. Heald. et al. 2013 ACPD. Ashley Pierce. Aerosol seminar, February 24th. 1. outline. Aerosols and climate change. IPCC on aerosols. Direct . Radiative . Effect vs. . Direct Radiative . 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 . . 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. Radiative. Fluxes . over Rugged Terrain from Satellite Measurements. Tianxing. Wang . (txwang.rs@gmail.com). Guangjian. Yan . (gjyan@bnu.edu.cn). Xihan. Mu . (muxihan@163.com). Ling Chen . radiative. forcing of black carbon aerosol: constraints from pole-to-pole (HIPPO) observations across the Pacific. Qiaoqiao. Wang, Daniel J. Jacob, J. Ryan . Spackman. , Anne E. . Perring. , Joshua P. Schwarz, . Longwave. High. Clouds. Shortwave. High. Clouds. Shortwave. Low. Clouds. . . Δ. Optical Depth: -4 %. Δ Total Cloud Frac.: -0.50 %. . . Δ CTP: -8.30 hPa. . . Δ. Optical Depth: 2.0 % K. -1. Richard P. Allan . University of Reading, Department of Meteorology NCAS-Climate/NCEO . Thanks to . Chunlei Liu, David Lavers, Matthias Zahn, Norman . Loeb, . John Lyman, Greg Johnson, . Brian . Soden. Hitachi-. HiTec. Electronic Excitation Model. A. ~. X. ~. g. Excitation. (. Absorption. ). Radiationless. decay. (vibrational relaxation). g. Fluorescence. . (Fast . radiative. decay). Internal conversion. radiative. forcing. Heald. et al. 2013 ACPD. Ashley Pierce. Aerosol seminar, February 24th. 1. outline. Aerosols and climate change. IPCC on aerosols. Direct . Radiative . Effect vs. . Direct Radiative . E. ffects. Lan Gao. 01/23/2017. ATMS 790. Trade cumulus clouds embedded in haze over Northern Indian Ocean, photo taken by Eric Wilcox. 1. Materials. T. wo articles:. . This review paper summaries the general and broad view of black carbon (BC) effects on the Earth climate.. 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. Based on the ITER-like and Snowflake divertor configuration of CFETR (Phase I, R = 5.7 m), SOLPS simulation is performed to understand the performance of radiative quasi-snowflake . divertor . with argon seeding..

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