Frost forms when the surface temperature of the object (tarp) cools to a temperature colder than the dew point, and both are below freezing. (Really it's the same process when dew forms, just above freezing temperatures). The dew point is the temperature at which the air becomes saturated and can no longer hold more moisture. The warmer the temperature the more water the air can hold.
So accumulation of frost does vary with moisture levels and temperature. You are probably more likely to see frost on your tarp at near freezing temperatures than you are at temps well below freezing, due to the amount of moisture the air can hold.
Bookmarks