Using TOA fluxes by cloud type to evaluate the ... - ceres - NASA

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Is TOA cloud rad. effect consistent with liq. water path?

Annual mean liquid water path averaged

over 1988-2007.

CanAM4 is much larger in mid-lat storm

tracks. Why isn't reflected solar too large?

Dataset: O'Dell, J. Climate, 2008

0 g/m^2 250 g/m^2

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Is TOA cloud rad. effect consistent with liq. water path? Annual mean liquid water path averaged over 1988-2007. CanAM4 is much larger in mid-lat storm tracks. Why isn't reflected solar too large? Dataset: O'Dell, J. Climate, 2008 0 g/m^2 250 g/m^2

Compensating biases in clouds Zhang et. al., 2005; 60S-60N DJF, 2001-2002 CRE=A(F clr -F cld )

Page 1 and 2: Using TOA fluxes by cloud type to e
Page 3: Top of atmos. cloud radiative effec
Page 7 and 8: Radiative effects by cloud type Har
Page 9 and 10: An example from a CloudSat/CALIPSO
Page 11 and 12: Relation between albedo and cloud f
Page 13: Summary • Time mean cloud and rad

Using TOA fluxes by cloud type to evaluate the ... - ceres - NASA

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