AEROSOL over CLOUD - IUP

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490nm POLARIZED RADIANCE 0,0360 0,0340 0,0320 0,0300 0,0280 0,0260 0,0240 0,0220 0,0200 ω 0 = 0.860, 0.880, 0.902, 0.925, 0.947, 0.974 reff = 0.2µm Molecular Absorption Scattering angle: 102° 0,02 0,04 0,06 0,08 0,10 0,12 0,14 no surface Z=0.5km Z=1.5km Z=2.5km Z=3.5km Z=4.5km Z=5.5km Z=6.5km Z=7.5km Z=8.5km Z=9.5km Z=10.5km AOD(490nm)=0.5 m'=0.020 m'=0.015 m'=0.025 m'=0.010 m'=0.030 m'=0.005 RADIANCE Z=1.5km AOD(490nm)=1.0 Z=3.5km Z=5.5km Aerosol Properties are extrapolated in the blue Z km 4.0 3.0 Altitude: <strong>over</strong> land and ocean 3.5
June 2006 - December 2008 Comparison with CALIOP <strong>over</strong> land
Page 1 and 2: POLARIZATION & ANISOTROPY of REFLEC
Page 3 and 4: Over Ocean,the POLDER instrument ca
Page 5 and 6: Why polarization is useful for aero
Page 7 and 8: LEVEL 3 Total Fine Mode Non-Spheric
Page 9 and 10: Benefits from Polarization: •Dete
Page 11: Refractive index of the large spher
Page 15 and 16: 865nm Detection (and quantification
Page 17 and 18: B QuickTime and a TIFF (Uncompresse
Page 19 and 20: The debate : How good (or bad) are
Page 21: Red dots: AERONET oceanic sites 420
Page 26 and 27: AOT of PARASOL/POLDER-2 AOT of PARA
Page 28 and 29: Fine Mode AOT 550nm Total AOT 670 n

AEROSOL over CLOUD - IUP

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