Seasonal subsurface heat conduction can have a large influence on Triton’s N, frost distribution. Increasing surface thermal inertia reduces the thickness and extent of seasonal N, frosts. If the thermal inertia of the nonvolatile substrate is greater than about 30% of the value for nonporous Hz0 or CO,, or if nonporous Hz0 or CO, is overlaid by a porous regolith of low thermal inertia but less...