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Published byNadia Bryer Modified over 10 years ago
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AEROCAN support for Activity 4 (Implications of Measurements on Simulations of Atmospheric Processes and Climate) N. T. O'Neill, S. Hesaraki, Universite de Sherbrooke, Sherbrooke, Canada Norm O'Neill, NETCARE workshop, U. of Toronto, Nov. 19, 2013
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AEROCAN (Canadian Sunphotometer Network) Resolute Bay Saturna Island Bratt’s Lake Waskesiu Churchill Kuujjuarapik Halifax Sherbrooke Egbert Pickle Lake Fort McKay & McMurray Kelowna Chapais Eureka (PEARL, OPAL) Toronto Yellowknife Iqaluit Sable Island Lethbridge
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NSHSRL MMCR CRL, AMS MMCR KARL Polar summer sites AERONET AEROCAN / AERONET Polar summer
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NSHSRL MMCR CRL, AMS MMCR KARL Starphotometers Moonphotometers Polar winter sites Polar winter
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Sampling of Oleg’s PSD inversions What parameters do we compare with the models?
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These results about a factor of 2 larger than modeling values used in recent publications or about a factor of 5.5 larger in terms of (per particle) backscatter cross section.
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Pan-Arctic AOD Climatology Barrow-NOAA Barrow-AERONET PEARL OPAL Thule Resolute Bay Alert Hornsund Ny-Alesund Kangerlussuaq Saha et al., 2013
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MODIS July 8, 2002 FMC
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Cloud screening 9
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10 Cloud screening (EUR: Mar 10, 2011)
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11 Cloud screening (EUR: Mar 13, 2011)
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