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The influence of wind speed on surface layer stability and turbulent fluxes over southern Indian peninsula station
2016
Proceedings of the Indian Academy of Sciences, Earth and Planetary Sciences
Surface to atmosphere exchange has received much attention in numerical weather prediction models. This exchange is defined by turbulent parameters such as frictional velocity, drag coefficient and heat fluxes, which have to be derived experimentally from high-frequency observations. High-frequency measurements of wind speed, air temperature and water vapour mixing ratio (eddy covariance measurements), were made during the Integrated Ground Observation Campaign (IGOC) of Cloud Aerosol
doi:10.1007/s12040-016-0735-5
fatcat:nket7grpuzdrbku2xla2pseega