Fig. 12
From: Implementation of a GNSS meteorological model to the estimation of the Haines Index
Differences between stability factors (in green) computed from radiosonde measurements (R) and simulated from GPT2w (GPT2w) as a function of the number of days during 2016 at the study area at mid-latitudes in South America, from the Atlantic coast up to the Andes pre-mountain range. Differences between moisture factors are plotted in blue. The results for Low-variant HI are shown in the left column and for Mid-variant HI in the right column