Evaluation of A New Mixed-Phase Cloud Microphysics Parameterization with the NCAR Climate Atmospheric Model (CAM3) and ARM Observations Fourth Quarter 2007 ARM Metric Report

• Main Authors: X Liu, SJ Ghan, S Xie, J Boyle, SA Klein
• Language: unknown
• Published: 2016
• Subjects: 54 ENVIRONMENTAL SCIENCES; CLIMATE MODELS; CLIMATES; CLOUDS; DEPOSITION; EVALUATION; METRICS; MIXTURES; NUCLEATION; RADIATIONS; SIMULATION; WATER; WATER VAPOR; WEATHER; Arctic
• Online Access: http://www.osti.gov/servlets/purl/948097; https://www.osti.gov/biblio/948097; https://doi.org/10.2172/948097

Mixed-phase clouds are composed of a mixture of cloud droplets and ice crystals. The cloud microphysics in mixed-phase clouds can significantly impact cloud optical depth, cloud radiative forcing, and cloud coverage. However, the treatment of mixed-phase clouds in most current climate models is crude and the partitioning of condensed water into liquid droplets and ice crystals is prescribed as temperature dependent functions. In our previous 2007 ARM metric reports a new mixed-phase cloud microphysics parameterization (for ice nucleation and water vapor deposition) was documented and implemented in the NCAR Community Atmospheric Model Version 3 (CAM3). The new scheme was tested against the Atmospheric Radiation Measurement (ARM) Mixed-phase Arctic Cloud Experiment (M-PACE) observations using the single column modeling and short-range weather forecast approaches. In this report this new parameterization is further tested with CAM3 in its climate simulations. It is shown that the predicted ice water content from CAM3 with the new parameterization is in better agreement with the ARM measurements at the Southern Great Plain (SGP) site for the mixed-phase clouds.