PPT-Simulation aerosol-clouds interaction over Europe with the

Author : stefany-barnette | Published Date : 2017-01-23

eulerian model WRF Chem Paolo Tuccella Gabriele Curci Suzanne Crumeyrolle Guido Visconti Direct and Indirect aerosol effects Clean Polluted Direct effect Indirect

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eulerian model WRF Chem Paolo Tuccella Gabriele Curci Suzanne Crumeyrolle Guido Visconti Direct and Indirect aerosol effects Clean Polluted Direct effect Indirect effect. 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. VIIRS Aerosol Cal/Val Team. VIIRS Aerosol Science and Operational Users Workshop November 21-22, 2013. 1. Outline. VIIRS Aerosol Products. Environmental Data Record (EDR). Intermediate Product (IP). Istvan. Laszlo. NOAA. VIIRS Aerosol Science and Operational Users Workshop . November 21-22, 2013.  . National Center for Weather and Climate Prediction (NCWCP). College Park, MD. Name. Organization. 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. Robert Wood. University of Washington. Radiative. “forcing” components. Cloud effects. Direct . Twomey. Mixed ph.. Semi-dir 2. nd. AIE. t. cld. .  . N. d. 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. 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. 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?. 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. Jón. Egill . Kristjánsson. (Univ. Oslo). Many thanks to: Alf . Kirkevåg. (. met.no. ), . Corinna. . Hoose. (Univ. Oslo), Leo Donner (GFDL). Problem Definition. Most GCMs give an aerosol indirect effect which is too high compared to results from residual calculations – . Robabeh. . Yousefi. . 1,2. , Fang Wang. 1. , . Quansheng. Ge. 1. , Abdallah Shaheen. 3. , . Juerg. Luterbacher. 4,5. 1. Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing100101, China;. 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 . 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. 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.

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