You can compute an index for evaluating the Bolivian High (BH) activity either by using 200 hPa stream function (or geopotential) anomalies averaged over the BH region or following the methodology of the below article: (https://link.springer.com/content/pdf/10.1007%2FBF01030418.pdf).
See Figure 2 from article that Gabriel sent to you. You can note a better BH configuration at 200 hPa and during austral summer as it is modulated by local diabatic heating.