Supplementary data to 'Topothermohaline convection – from synthetic simulations to reveal processes in a thick geothermal system'

Simulation animations show the time-dependent processes in a basin through the parameters of Darcy flux, temperature, salt concentration, salinity, and age. The cases reflect the effects of water table amplitude, bottom heat flux and bottom salt concentration. There is a case study of Buda Thermal Karst, Budapest, Hungary.