PPT-Evaluation of cirrus microphysics in CAM5 using aircraft data

C Bardeen A Gettelman E Jensen ATTREX Science Team Meeting October 24 2013 Ice Water Path Bardeen et al 2013 IWP Tropical Bias Global Tropics IWP Tropics JF Cloud Fraction amp Ice Water Content. There is no perfect safety solution but there is technology that can be implemented to make aviation safer than it historically has been What began as an idea of a whole airframe parachute system available to save the pilot and passengers in the eve is. . the . #1 app . on the Salesforce . AppExchange for integrating Salesforce and Gmail.. “. Cirrus Insight . brings . Salesforce . and Gmail together in an intuitive way to help people get work done faster. app on the Salesforce AppExchange.. “. Cirrus Insight brings Salesforce.com and Gmail together in an intuitive way to help people get work done faster.. ” - DeveloperForce. The top sales app and the top email app. CEC14 Berlin. Lawrence . J. ackson, Julia Crook & Piers Forster. Jones et al. (2011). Stratospheric SO. 2. Marine cloud brightening. To return global mean temperature to some earlier state, precipitation is reduced by too much. radiative. characteristics. . By . Sardar. AL-. Jumur. Supervisor. Steven . Dobbie. . Aims and objectives . Study the lifetime and evolution of tropical thin cirrus formed on glassy and non-glassy particles.. Linjiong Zhou. 1,2. ,. . Minghua. Zhang. 1. , Steve . Goldhaber. 3. 1. . SoMAS. , Stony Brook University. 2. LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences. 3. AMP, NCAR Earth System Laboratory. Betsy Berry and Jay Mace. University of . Utah. American Geophysical Union 2011 . Fall Meeting. More CCN→. more small droplets→ . less collision→ delayed raindrop formation . Smaller sizes are lofted higher where they freeze→ latent heat release leads to increased buoyancy and a stronger updraft. ANOTHER LEVEL OF SECURITY. ACCIDENT SCENE SAFETY. RECOGNIZE THE . PRESENCE. OF A BRS SYSTEM. AVOID THE POSSIBILITY OF . INADVERTENTLY INITIATING. THE SYSTEM. TAKE THE NECESSARY STEPS TO . DEACTIVATE. during November . 12-15, . 2015 and November 16-19, 2015. Robert Conrick, Qi Zhong, and Cliff Mass. University of Washington. . Pacific NW Weather Workshop 2017. Cases: November . 12-15, . 2015. Betsy Berry and Jay Mace. University of . Utah. American Geophysical Union 2011 . Fall Meeting. More CCN→. more small droplets→ . less collision→ delayed raindrop formation . Smaller sizes are lofted higher where they freeze→ latent heat release leads to increased buoyancy and a stronger updraft. * Corresponding author: Bernd Kärcher, DLR-Institut für Physik der Atmosphäre, Oberpfaffenhofen, D-82234Weßling, Germany. Email: bernd.kaercher@dlr.de 2 THE PAZI PROJECTThe project studied the for Detrained ice R. e. importance:. Cloud albedo. Anvil cirrus persistence. Redistribution of H. 2. O. Entrainment of aerosols into updrafts . . increasing ice concentration with height. Entrainment dry air at cloud top . the Characterization of Clouds, Aerosols and the . Cryosphere. in Climate . Models. Parameterization development. How have changing forcing agents influenced sea ice over the last few decades?. How do improvements to process level representation influence our interpretation of that climate change?. Hua Leighton. Collaborators: Robert Black, Frank Marks,. . . Xuejin. Zhang, . Gopal. . Sundararaman. Why do we care about microphysics?. Direct impact . . .