Abstract. Vertical ascent rate VB of meteorological balloons
is sometimes used for retrieving vertical air velocity W, an important
parameter for meteorological applications, but at the cost of crude
hypotheses on atmospheric turbulence and without the possibility of formally
validating the models from concurrent measurements. From simultaneous radar
and unmanned aerial vehicle (UAV) measurements of turbulent kinetic energy
dissipation rates ε, we show that VB can be strongly
affected by turbulence, even above the convective boundary layer. For
“weak” turbulence (here ε≲10−4 m2 s−3), the
fluctuations of VB were found to be fully consistent with W
fluctuations measured by middle and upper atmosphere (MU) radar, indicating that an estimate of W can
indeed be retrieved from VB if the free balloon lift is determined. In
contrast, stronger turbulence intensity systematically implies an increase in VB, not associated with an increase in W according to radar data,
very likely due to the decrease in the turbulence drag coefficient of the
balloon. From the statistical analysis of data gathered from 376 balloons
launched every 3 h at Bengkulu (Indonesia), positive VB
disturbances, mainly observed in the troposphere, were found to be clearly
associated with Ri≲0.25, usually indicative of turbulence, confirming
the case studies. The analysis also revealed the superimposition of
additional positive and negative disturbances for Ri≲0.25 likely due to
Kelvin–Helmholtz waves and large-scale billows. From this experimental
evidence, we conclude that the ascent rate of meteorological balloons, with
the current performance of radiosondes in terms of altitude accuracy, can
potentially be used for the detection of turbulence. The presence of
turbulence complicates the estimation of W, and misinterpretations of
VB fluctuations can be made if localized turbulence effects are
ignored.