PPT-Aerosol-cloud-precipitation interactions in warm clouds: is

Photograph Tony Clarke VOCALS REx flight RF07 Robert Wood University of Washington with Rhea George Chris Terai Dave Leon Jeff Snider or Control of cloud droplet concentration in marine stratocumulus clouds. and Modeling of the Green Ocean . Amazon. . Green . Ocean Amazon . 2014. . GoAmazon2014. . Carbon Cycle Cloud Life Cycle Aerosol Life Cycle. Climate. Ecosystems. Atmospheric Composition. 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. Parameters. Jay Mace. Trevor Ferguson. Stephanie . Avey. Steve Cooper. Photo Credit: . patternsofnature.files.wordpress.com. e.. f.. The Southern Ocean is one of the cloudiest regions on Earth…. … and primarily populated by geometrically thin layers based in the boundary layer.. 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. Robert Wood. University of Washington. Radiative. “forcing” components. Cloud effects. Direct . Twomey. Mixed ph.. Semi-dir 2. nd. AIE. t. cld. .  . N. d. The SOCRATES Planning . Team. : . Greg . McFarquhar. (. mcfarq@atmos.uiuc.edu. ),. Roj. . Marchand. , . Robert . Wood, Chris . Bretherton. , Alain . Protat. , Patricia Quinn, Steven . Siems. , Simon Alexander, and Bob Weller. ACE is presently in pre-formulation and will be realized in some form in the early to mid . ’. 20s. . ACE is a response to the . The extreme sensitivity of the climate system to hydrological processes especially clouds and precipitation. ACE is presently in pre-formulation and will be realized in some form in the early to mid . ’. 20s. . ACE is a response to the . The extreme sensitivity of the climate system to hydrological processes especially clouds and precipitation. Robert Wood Graham Feingold Dave Turner. Warm cloud responses to aerosols. Microphysical, structural, and dynamical properties of low, liquid-phase clouds show sensitivity to aerosol loading, . but. the responses are not uniform. Aerosol-Cloud-Climate Interactions. . Spring Quarter 2015. Logistics. Class . webpage. . Class meets 1:30-2:50 Mondays and Wednesdays in Room 406, ATG Building. Instructor: . Deliberate Cloud Seeding. Cloud Seeding. Deliberate cloud seeding, with the goal of increasing precipitation by the injection of specific types of particles into clouds, has been pursued for over 60 years. . Robert Wood, Atmospheric Sciences,. University of Washington. Motivation. Aerosols can potentially influence earth’s radiation budget both by direct interaction with sunlight (aerosol . direct . effect), and also by altering cloud radiative properties (aerosol . . Spring Quarter 2015. Logistics. Class . webpage. . Class meets 1:30-2:50 Mondays and Wednesdays in Room 406, ATG Building. Instructor: . Prof. . Robert . Wood . [ATG . 718, Phone . 7. Ashley . Evanoski. -Cole & Christina McCluskey. ATS 786. 12 October, 2014. Clouds in Present Day Climate System. First time cloud and aerosol has been in the same chapter in an IPCC report!. Improved observations of clouds, resolving multilayer cloud systems.