Prior posts on clouds
Journal of Climate 2013 ; e-View
C. Zhou,1 M. D. Zelinka,2 A. E. Dessler,1 and P. Yang1
The cloud feedback in response to short-term climate variations is estimated from cloud measurements combined with off-line radiative transfer calculations. The cloud measurements are made by the Moderate Resolution Imaging Spectroradiometer (MODIS) on NASA’s Terra satellite and cover the period 2000-2010. Low clouds provide a strong negative cloud feedback, mainly due to their impact in the shortwave (SW) portion of the spectrum. Mid-level clouds provide a positive net cloud feedback that is a combination of a positive SW feedback partially canceled by a negative feedback in the longwave (LW). High clouds have only a small impact on the net cloud feedback due to a close cancellation between large LW and SW cloud feedbacks. Segregating the clouds by optical depth, we find that the net cloud feedback is set by a positive cloud feedback due to reductions in the thickest clouds (mainly in the SW) and a cancelling negative feedback from increases in clouds with moderate optical depths (also mainly in the SW). The global average SW, LW, and net cloud feedbacks are +0.30±1.10, -0.46±0.74, and -0.16±0.83 W/m2/K, respectively. The SW feedback is consistent with previous work; the MODIS LW feedback is lower than previous calculations and there are reasons to suspect it may be biased low. Finally, it is shown that the apparently small control that global mean surface temperature exerts on clouds, which leads to the large uncertainty in the short-term cloud feedback, arises from statistically significant but offsetting relationships between individual cloud types and global mean surface temperature.