Document Type
Data
Publication Date
11-10-2025
Abstract
Cloud optical properties and precipitation, which are crucial to weather and climate, are strongly influenced by cloud microphysical properties that are still poorly understood. Here, we develop a high-resolution time-correlated single-photon-counting lidar and apply it to observe cloud microphysical properties at one-centimeter range resolution in a convection chamber under well-controlled conditions. Together with concurrent in-situ measurements and theoretical analysis, our lidar observations indicate that although turbulent mixing tends to homogenize the cloud in the bulk region, entrainment and sedimentation cause inhomogeneities in droplet concentrations near the cloud top. Specifically, the topmost region is directly affected by entrainment, and lidar profiles show clear evidence of entrained air and detrained cloud filament. The transition region below exhibits vertical size sorting of cloud droplets caused by sedimentation. Our results suggest that using a single sedimentation velocity for all cloud droplets, as is done in many atmospheric models, overlooks key physics relevant to the microphysical structure near the cloud top. Our conceptual model used to describe these measurements can serve as a step towards improving the current modeling of processes in the cloud top region.
Recommended Citation
Yang, F.,
Sua, Y.,
Zheng, Z.,
Anderson, J.,
Sadi, H. F.,
Yeom, J.,
Singh, S. P.,
Hou, P.,
Cantrell, W.,
Lewis, E. R.,
Kostinski, A.,
&
Shaw, R.
(2025).
Data supporting “High-resolution lidar observations of sedimentation-induced size sorting of droplets near a laboratory cloud top”.
Retrieved from: https://digitalcommons.mtu.edu/all-datasets/63
Read Me File
Comments
Department of Energy Office of Science grant number DE-SC0012704 National Science Foundation grant number AGS-2133229 and AGS-2217182 Simons Foundation grant number PD-Grant-01249402