PPT-Strong Sensitivity of Aerosol Concentrations to Convective

E CHAM5HAM B Croft 1 JR Pierce 1 RV Martin 12 C Hoose 3 and U Lohmann 4 1 Dalhouse University Canada 2 HarvardSmithsonian Centre for Astrophysics USA 3 Karlsruhe Institute of Technology Germany. p.connolly@manchester.ac.uk Introduction: Convective invigoration describes a pathway by which aerosols modulate cloud evolution, precipitation and radiation (Rosenfeld et al. 2008). This idea sugges 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. . Convective Dynamics. 4.5. Bright Bands, Bow Echoes and Mesoscale Convective Complexes. Photographs ©  Todd Lindley. . Bright band associated with stratiform precipitation in a squall line system. Bright band associated with stratiform precipitation. Physico. -Chemical Properties of Caribbean Aerosols during RICO: African Dust and Pollution from North America. Olga L. . Mayol-Bracero. Institute for Tropical Ecosystem Studies. University of Puerto Rico, Río . (The 10. th. . Adjoint. Workshop). Roanoke. , West Virginia. June . 1. -5, . 2015. The Use of Ensemble-Based Sensitivity with Observations to Improve Predictability of Severe Convective Events. Brian . Robert A. Houze, Jr.. University of Washington. with: K. L. Rasmussen, M. D. Zuluaga, and S. R. Brodzik. European Geosciences Union General Assembly, Vienna, Austria 17 April 2015 . The TRMM Satellite. 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. Robert A. Houze, Jr.. University of Washington. with: K. L. Rasmussen, M. D. Zuluaga, and S. R. Brodzik. Presented at:. AGU Fall Meeting, San Francisco, 18 December 2015 . The TRMM Satellite. 1997-2014. Matthew Toohey. 1. Kirstin . Krüger. 1,2. , . Claudia . Timmreck. 3. , . Hauke . Schmidt. 3. 1 . GEOMAR. , Helmholtz Centre for Ocean Research Kiel, Germany. 2 . Now at . University . of Oslo, Norway. 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. (The 10. th. . Adjoint. Workshop). Roanoke. , West Virginia. June . 1. -5, . 2015. The Use of Ensemble-Based Sensitivity with Observations to Improve Predictability of Severe Convective Events. Brian . Monitoring Supersite in Korea , Suk-Jo LeeDepartment of Environmental Engineering, Chonnam National University, 300 Yongbong-dong, Gwangju 500-757, Korea ABSTRACT Hourly measurements of PM, organic Figure caption. Significance and Impact. . . Approach and Findings. .. citation. Department of Energy • Office of Science • Biological and Environmental Research. Figure. EXAMPLE. Scientific Challenge . 1. Mian Chin. NASA Goddard Space Flight Center, USA. Huisheng. . Bian. University of Maryland at Baltimore County/NASA GSFC, USA. Qian Tan. Bay Area Environmental Research Institute/NASA Ames, USA. Ghassan Taha.