PPT-CalWater 2 Chemical / Aerosol Forecast

Jessie Creamean Andrew Martin Thursday January 22 2015 Current Conditions I High AOD plumes Jan21a and Jan21b are in dry slot of mature in N Central Pac These likely correspond to plumes Jan20a and Jan20b respectively. 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. Jingqiu . Mao . (GFDL/NOAA), . Songmiao. Fan (. GFDL/NOAA), . Ying . Chen (. Fudan. U, China). A . dominant source of nutrient iron to open . ocean, critical for plankton in surface waters:. -Biological pump of CO2. Schedule. Who and when?. Dissemination. How? . Content. Products and information. What will be communicated?. Consistency. Will there be a template?. CalWater. 2 – Implementation | Meteorological Forecasting. Yan . Zhang. 1. , . Hongbin. . Yu. 2. , . Alexander . Smirnov. 1. , . Tom . Eck. 1. , . Mian. . Chin. 3. , . Lorraine . Remer. 3. , . Qian. . Tan. 1. , . Robert . Levy. 4. 1 GESTAR/USRA, 2 ESSIC, 3 NASA/GSFC, 4 SSAI. Three meteorology forecasters located at AOC for duration of field operations. Senior or lead forecaster. Junior or student forecaster. NWS representative. One chemical forecaster. One of meteorology forecasters if experienced. 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 . Chem. “Aerosol Chemicals to Aerosol Optical Properties” Module using data from the MILAGRO campaign. J. C. Barnard, J. D. Fast, G. Paredes-Miranda, W. P. Arnott, and A. . Laskin. Atmos. Chem. Phys. 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. CalNex. R. Bradley Pierce. NOAA/NESDIS/STAR. Allen . Lenzen. 1. , . Todd . Schaack. 1. , . Tom . Ryerson. 2. , . John . Holloway. 2. , . Ilana. . Pollack. 2. , . Ann . Middlebrook. 2. , . Roya. . Bahreini. eulerian. model WRF/. Chem. Paolo Tuccella, Gabriele Curci, . Suzanne. . Crumeyrolle. , Guido Visconti. Direct and . Indirect. aerosol . effects. Clean. Polluted. Direct . effect. Indirect. . effect. 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 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 . 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 – . Jessie Creamean. Andrew Martin. Sunday, . January . 25, . 2015. Executive Summary. Today for . G-1 flight over . BBY, low level (< 3 km) pollutants and clear skies . In next 5 days, high AOD plumes currently over Pacific disperse and/or hit Canada, missing CA .