For two years we observed the vertical distribution of clouds and aerosols in Jakarta, Indonesia, with ground-based Mie scattering lidars. A histogram of the cloud based height shows a notable maximum at an altitude of approximately 5 km, especially in the wet season. The planetary boundary layer height we inferred from the upper boundary of the aerosol layer was approximately 1.5-2 km in the wet season and 2-3 km in the dry season.
CITATION STYLE
Sugimoto, N., Matsui, I., Shimizu, A., Pinandito, M., & Sugondo, S. (2000). Climatological characteristics of cloud distribution and planetary boundary layer structure in Jakarta, Indonesia revealed by lidar observation. Geophysical Research Letters, 27(18), 2909–2912. https://doi.org/10.1029/2000GL011544
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