PPT-Temporal variability of aerosol properties at
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mountain sites a lagautocorrelation analysis Andrews E 12 Ogren JA 1 Bonasoni P 3 Marinoni A 3 Cuevas E 4 Rodríguez S 4 Sun
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Temporal variability of aerosol properties at: Transcript
mountain sites a lagautocorrelation analysis Andrews E 12 Ogren JA 1 Bonasoni P 3 Marinoni A 3 Cuevas E 4 Rodríguez S 4 Sun. Example from the Saharan Desert.. Deep Blue . Algorithm from this reference.. darkness. Blue sky. Blue sky bright aerosol. Bright aerosol . brighten dark surface. Dark aerosol . darken bright surface. Betty Croft. 1. , Jeff Pierce. 1,2. and Randall Martin. 1,3. 1. Dalhousie University, Halifax, Canada. 2. Colorado State University, Fort Collins, USA. 3. Harvard-Smithsonian Center for Astrophysics, Cambridge, USA. An Introduction to Aerosol Propellants 3 Aerosol Product System 4 Aerosol Product System 5 Aerosol Product System 6/MCI; 8 ;/MCI; 8 ;Aerosol Product System 7 Aerosol Product System 8 A 2. Column Retrievals with Ground-based Monitors. Randall . Martin (Dalhousie, Harvard-Smithsonian). with . contributions from. Melanie Hammer, . Shailesh. . Kharol. , Jeff Geddes (Dalhousie U). TEMPO Science Team Meeting. Clio Gielen. Michel Van Roozendael, . Francois Hendrick. , Caroline Fayt, . Christian Hermans, Gaia Pinardi, Didier Gilllotay, and Tim Vlemmix. + . Hugo . De Backer, . Veerle. De Bock, and Quentin . at . Lhasa. and . Kunming. during Asian summer monsoon. Jianchun Bian . (IAP/CAS). In the poster, balloon sounding water vapor, ozone, and particle (SWOP) campaign during the ASM will be introduced, including sonde, location and timing. . Yi Ming. Geophysical . Fluid Dynamics Laboratory. Princeton, New Jersey. . Most anthropogenic aerosols are in the NH mid-latitudes and tropics. MODIS annual-mean aerosol optical depth (AOD). Will the response be confined locally?. eulerian. model WRF/. Chem. Paolo Tuccella, Gabriele Curci, . Suzanne. . Crumeyrolle. , Guido Visconti. Direct and . Indirect. aerosol . effects. Clean. Polluted. Direct . effect. Indirect. . effect. 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 . 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. Kuroshio. Extension . System . B. Qiu. 1. , S. Chen. 1. , N. Schneider. 1. and B. Taguchi. 2. 1. Dept of Oceanography, University of Hawaii, USA. 2. Earth Simulator Center, JAMSTEC, Japan. Climate Implications of Frontal Scale Air-Sea Interaction Workshop, Boulder, 5-7 August . Axel Lauer, . Mattia . Righi, Veronika Eyring, and Johannes Hendricks. Deutsches . Zentrum für Luft- und Raumfahrt e.V. (DLR. ). , . Oberpfaffenhofen. , Germany. 27 May 2015. Scientific Questions. What . Elisabeth Andrews. CATCOS Aerosol Workshop, June 2016. What’s an Aerosol. ?. Definition: . Particle or liquid suspended in a gas.. Examples of atmospheric aerosols:. Dust. Combustion aerosol (forest fires, vehicles…). 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.
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