PPT-CS 294-73 (CCN 27241)

Software Engineering for Scientific Computing httpwwwcsberkeleyedu colellaCS294 Lecture 4 Development Tools Revision Control Systems Modern scientific computing is no longer a solo effort. Orographic. Precipitation. William R Cotton. Dept of Atmospheric Science. Colorado State University. In the case of wintertime . orographic. clouds, we expect that increased concentrations of CCN will increase the cloud droplet number concentration, reduce cloud droplet diameters, reduce riming growth of ice, and thereby reduce precipitation. . Photograph: Tony Clarke, VOCALS . REx. flight RF07. Robert Wood. University of Washington. with help/data from Dan Grosvenor, Daniel McCoy, Chris . Terai. , Matt . Lebsock. , Dave Leon, Jeff Snider, Tony Clarke. Robert Wood. University of Washington. W. ith contributions . from . Eowyn. Baughman, Dan . Grosvenor, Daniel McCoy, Chris . Terai. , Matt . Lebsock. , Dave Leon, Jeff Snider, Tony . Clarke, . Duli. VOCALS RF07: Over broken clouds and very thin Stratus clouds at south end of POC region, by Tony Clarke. Coalescence scavenging: . the importance of cloud-driven aerosol sinks. Robert Wood. ,. . University of Washington. Photograph: Tony Clarke, VOCALS . REx. flight RF07. Robert Wood. University of Washington. “Background” cloud droplet concentration critical for determining aerosol indirect effects. Quaas. et al., AEROCOM . TO ENHANCED CCN CONCENTRATIONS . William R. Cotton. Department of Atmospheric Science, Colorado State University. Approaches to hailstorm simulation. 2 moment bulk microphysics. Hybrid approach: Bulk 1-M or 2-M microphysics with bin representation of hail. Model accounts for:. Entrainment. Surface production (sea-salt). Coalescence scavenging. Dry deposition. Model does not account for:. New particle formation – significance still too uncertain to include. 30/06/1997 To authorize the disposal of goods accepted in the course of a business for repair or other treatment but not redelivered; and for purposes connected therewith. [1 January 1970] (Original 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. supersaturation. and 499 nm AOD, both observed from ≤1 km altitudes during ARCTAS Canada and averaged over 10 seconds. Note the reversed . x,y. axes from . Andreae’s. (. 2009) . similar plot. While the regression is given for the bin averages, the regression for the individual data is only slightly different. (right) Horizontal variability of the CCN and AOD. See . Patient in a CCN Practice Presents with Behavioral Health Issue. (during . “. normal. ”. office hours M-F). Ready to enter treatment for addiction now. Depressed, has an eating disorder, or is emotionally overwhelmed. 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 NonDisc-AccessibilityNoticeAddendum 09/2016pg 1of 4NONDISCRIMINATION AND LANGUAGE ACCESSIBILITY NOTICENondiscrimination NoticeVIVA HEALTH color national origin age disability or sex VIVA HEALTH does and CCN activity. Sara Lance. WFM Pilot Study, Preliminary Observations. Aug 24, 2017. Aerosol Impacts: Climate (‘Global Dimming’). Haze blown off the Eastern coast of China, over Bo Hai Bay and the Yellow Sea.