Turbulence characteristics over tropical station Gadanki (13.5°N, 79.2°E) estimated using high‐resolution GPS radiosonde data

Abstract

Seasonal variation of the turbulence parameters, refractivity structure constant C n 2 , eddy dissipation rate ɛ, and eddy diffusivity K , is presented using 3 years (April 2006 to March 2009) of high vertical resolution GPS radiosonde measurements over the tropical station Gadanki (13.5°N, 79.2°E). First, a correlation analysis was done in order to study the relative contributions of temperature ( T ) and relative humidity (RH) to the refractive index gradient ( M ). A strong positive (negative) correlation between M and RH ( T ) gradients is noticed up to 10 km. Above 10 km, a strong positive correlation between M and T gradients is seen, except at altitudes near the tropopause. In the present study we flag the turbulent layers using the Thorpe sorting method and estimate the structure constant C n 2 for the turbulent layers. The probability of occurrence of C n 2 is derived from the cumulative distribution at each height and is found to decrease from 10 −7 to 10 −17 m −2/3 with height. The probability of the occurrence of C n 2 conditioned to the occurrence of turbulence as a function of height is derived, and it is found that only the mean and the 90th percentile profile reach an altitude of ∼27 km. The demarcation between the boundary layer and the free atmosphere as well as between the troposphere and the stratosphere are quite clear from the turbulence profile, which allows us to identify the boundary layer and tropopause heights from turbulence profiles. Thus, the present analysis introduces an alternative approach to identify the height of the boundary layer as well as the tropopause and also to characterize the probability of turbulence and thickness of turbulent eddies in the atmosphere with a finer scale size (down to 5 m) for the first time from a tropical latitude.