资源环境科技发展态势分析平台

Turbulence and drizzle-rate measurements from a large dataset of marine and continental low stratiform clouds are presented. Turbulence peaks at cloud base over land and near cloud top over the ocean. For both regions, eddy dissipation rate values of 10(-5)-10(-2) m(2) s(-3) are observed. Surface-based measurements of cloud condensation nuclei number concentration N-CCN and liquid water path (LWP) are used to estimate the precipitation susceptibility S-0. Results show that positive S-0 values are found at low turbulence, consistent with the principle that aerosols suppress precipitation formation, whereas S-0 is smaller, and can be negative, in a more turbulent environment. Under similar macrophysical conditions, especially for medium to high LWP, high (low) turbulence is likely to lessen (promote) the suppression effect of high N-CCN on precipitation. Overall, the turbulent effect on S-0 is stronger in continental than marine stratiform clouds. These observational findings are consistent with recent analytical prediction for a turbulence-broadening effect on cloud droplet size distribution.