Which fog type is characterized by moisture accumulating on sloping land features?

Upslope fog forms when moist air is forced to rise over sloped terrain. As the air ascends the slope, it cools, leading to condensation and the formation of fog. This process is driven primarily by orographic lift, where warmer, moist air rises and cools at higher elevations, resulting in the accumulation of moisture in the form of fog.

This is in contrast to other types of fog where different processes are involved. Heat fog generally occurs in the summer when ground heat causes rapid evaporation of moisture. Radiation fog forms overnight when the ground cools rapidly, causing moisture in the air to condense near the surface. Advection fog happens when warm, moist air moves over a cooler surface, resulting in condensation. Each of these processes has its own unique characteristics, but upslope fog specifically pertains to the interaction of air with sloping land forms.