|
Penny M. Rowe (University of Idaho, Department of Geography)  Cloud feedbacks are among the largest sources of uncertainty in climate models. Cloud feedbacks are complicated because they involve both a cooling effect, through reflecting solar radiation back to space, and a greenhouse warming effect, through trapping infrared radiation. In addition, the magnitude of these effects depends on cloud properties, including cloud height, phase (liquid, ice, or mixed phase), and droplet or crystal size. Supercooled liquid clouds, in particular, exist in polar regions and in mid-level clouds globally and are an important component of the climate system. However, global climate models under-predict the amount of supercooled liquid clouds. To better understand cloud feedback processes in the climate system, it is essential to collect accurate measurements of supercooled cloud properties and to improve our understanding of how such clouds interact with infrared radiation at microphysical and macrophysical levels. Supercooled liquid water was observed at the South Pole at temperatures well below freezing (–320C). At the same time, a highly spectrally resolved measurement of the downwelling infrared radiance from the cloud was made. Despite the cloud being well-characterized, significant discrepancies were evident between measured and simulated infrared radiances that could not be resolved by adjusting conventional microphysical parameters. The reason for the discrepancies was a mystery. In this talk, we will discover that the supercooled liquid cloud mystery involves erroneous assumptions about the radiative properties of liquid clouds, and that these assumptions result in underestimation of the local greenhouse effect and errors in cloud property retrievals. Implications for other atmospheric and geographical conditions will be discussed. Following this will be a brief overview of other research and research goals, including cloud property and trace gas retrievals in the polar regions.
|