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. 2024 Mar 26;14:7175. doi: 10.1038/s41598-024-57458-4

Figure 4.

Figure 4

Diurnal variation, as a function of LMST, of the derived surface water activity concerning liquid (with aw error bars) and measured ground temperature provided by MEDA during one full Martian year. For illustration, the environmental data are overlayed with the hydration lines of calcium and magnesium sulfates, and calcium perchlorate deliquescence and efflorescence lines. The water activity aw is derived assuming equilibrium, from the relative humidity (RH), with respect to liquid, as aw = RH/100, All data points to the left of the ice saturation line (RHice = 100%) are saturated with respect to ice and may allow frost formation70. The Deliquescence RH (DRH) and hydration state lines of some perchlorates and sulfate salts are included for reference19,72.