PPT-Does Aerosol Loading in a Convective Environment Influence Cirrus Anvil Properties?

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. and Charlotte Radiology Belk Mobile Mammography Center Silver COMMUNITY RELATIONS Government United States Holocaust Memorial Museum Edelman US Holocaust Memorial Museum 20th Anniversary National Tour Tribute AOE COMMUNITY RELATIONS Government New Agenda. History. Case summary . Strategy. Anvil Media and Linkedln. Results. Case Study Questions. Anvil Media History . Kent Lewis Founded in 2000. Search Engine Marketing/ SEO. Purpose. The Anvil Effect. Limitations. R. Houze. University of Washington. CaPPM. Meeting, JPL, Pasadena, October 1, 2014. TRMM. GPM. CloudSat .  . EarthCare. TRMM and CloudSat analyses in the tropics: Advantages and . 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. Lazy Loading: . Gerekeni, gerektiğinde getir.. Eager Loading: . Hepsini getir. . Gerekenleri kullan.. Lazy Loading vs. Eager Loading. Lazy Loading vs. Eager Loading. dbo.Products. dbo.Categories. dbo.Suppliers. . E. CHAM5-HAM. B. Croft. 1. , J.R. . . Pierce. 1. , R.V. Martin. 1,2. , C. Hoose. 3. , and U. Lohmann. 4. 1. Dalhouse University, Canada. 2. Harvard-Smithsonian Centre for Astrophysics, USA. 3. Karlsruhe Institute of Technology, Germany. Jacob Anderson. Mentor: Gregory . Leptoukh. Research Objectives. Based on previous research determine the variables that most affect MODIS bias. Find which MODIS aerosol algorithm works better over coastal regions. Weather Systems – Fall 2015. Outline:. a. Stability Indices. b. Wind Shear and . Helicity. c. How to relate to predicted / observed convective weather. Convective Parameters. Weather Systems – Fall 2015. MODIS. , TRMM, and ECMWF-Interim Reanalysis Data. TERRA/AQUA PI: . Terry Kubar (UCLA/JIFRESSE). Co-I: . Ali . Behrangi. (JPL). Collaborator: . Graeme Stephens (JPL). MODIS Science Team Meeting – Atmosphere Team Breakout Session. &. related issues. P. . Mukhopadhyay. Climate v. Numerical Weather Prediction. NWP: . Initial state is CRITICAL. Don’t really care about whole PDF, just probable phase space. conservation of mass/energy to match observed state. Ref Vel. stratiform. Conv(all) rad_ref. Cloud analysis followed by 3dvar. Conv(uv spd) rw. Only 3dvar analysis. Applied DFI to Qv only, other mosit variable like Qs, Qc, Qr, Qg, Qi are remain unchanged and. 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 . Temporal, spatial and systematic patterns in aerosol properties at . Anmyeon. -do (AMY) . Dr. Elisabeth (Betsy) Andrews. NOAA/ESRL/Global Monitoring Division. Boulder, CO USA. November, 2013. Talk Outline. Kengo. . Matsubayashi. Japan Meteorological Agency. The Met Office. Outline. Motivation. Observation and evaluation method. Evaluation result. Summary. In many convection schemes, water substances are empirically modelled..