PPT-Radiative Properties of Eastern Pacific Stratocumulus Cloud

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. 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. 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. FORMATIONS. IDT 7062. By Renee Payne. Tutorial Navigation. . The Home button will returns you to the Title page. . . . . The Forward arrow button takes your to the Next page.. 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. 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.. Photograph: Tony Clarke, VOCALS . REx. flight RF07. Robert Wood. University of Washington. with help/data . from Chris . Terai. , Dave Leon, Jeff Snider. Radiative. impact of cloud droplet concentration variations. Control of Cloud Droplet Concentration in Marine Stratocumulus Clouds Photograph: Tony Clarke, VOCALS REx flight RF07 Robert Wood University of Washington with help/data from Chris Terai , Dave Leon, Jeff Snider Control of Cloud Droplet Concentration in Marine Stratocumulus Clouds Photograph: Tony Clarke, VOCALS REx flight RF07 Robert Wood University of Washington with help/data from Chris Terai , Dave Leon, Jeff Snider 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 Xiaoming Hu. 1. , Sergio A. Sejas. 2. , Ming Cai. 3. , . Zhenning. Li. 4. and Song Yang. 1. 1. School of Atmospheric Sciences, Sun . Yat-sen. University, Guangzhou, China. 2. NASA Langley Research Center, Climate Science Branch, Hampton, Virginia, USA. . Overview of Model: Convection. . The convection scheme of . Emanuel and . Živkovic. -Rothman. . (1999) . uses a buoyancy sorting algorithm . and . represents an entire spectrum of convective clouds, from shallow, non-precipitating cumulus to deep precipitating cumulonimbus. Precipitation re-evaporates and drives an unsaturated downdraft that imports enthalpy and moisture into the subcloud layer. Re-evaporation of cloud water, resulting from entrainment of dry air, drives penetrative downdrafts within the clouds. The cloud base mass flux is continuously relaxed so as to produce near neutrality of a parcel lifted dry adiabatically, and then moist adiabatically, to the first level above its lifted condensation level. This maintains a form of boundary layer . (. NOAA).. PART 1: Plate boundaries of 12 major plates. Kious. and Tilling, USGS. PART 1: Topographic/Bathymetric trends (eastern margin of the Pacific plate). (modified from NOAA).. PART 1: Trends in earthquake and volcano distribution; hot spot trends. 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?.