PPT-How radiative processes can influence

tropical cyclones Robert Fovell and Yizhe Peggy Bu University of California Los Angeles rfovelluclaedu 1 Thanks to Greg Thompson NCAR DTC Ligia Bernardet and Mrinal Biswas. 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 . 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.). 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. by . means of MBE method. Ashida. . lab. M1 . K. amizono Kenta. Introduction. All-optical switching devices. Excitons . and light in the high-quality system . Background . Previous results. Temperature dependence of DFWM spectrum. . 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.. 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. and Photocurrent. . in a Blue LED. Ben Stroup & Timothy Gfroerer, Davidson College, Davidson, NC. Yong Zhang, University of North Carolina at Charlotte, Charlotte, NC. Contrast Imaging. Motivation: Solar Cells. 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. DYNAMO/CINDY. 2011. C.-H. . Sui, . Yi-An Chen, . Shu-Yu . Hou. National Taiwan University. NSA. SSA. (73.1E,0.7S). (. 72E,-7.3N. ). (73.5E,4.2N). (. 79E,6.9N. ). (. 80.5E,0.07N. ). (. 80.5E,-8N. ). Male. 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.. 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 . Day . 7. : 10-16-13. Climate Dynamics (PCC 587): Climate . Forcings. Outline of This Topic. Climate . forcings. Things that directly change global temperature. How to put different effects on the same ground. 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..