The document discusses different forms of condensation in the atmosphere. It explains that condensation occurs when water vapor in the air turns into liquid form due to an increase in water vapor or a decrease in temperature. The main forms of condensation discussed are dew, frost, fog, and mist. Dew occurs as water droplets on surfaces like grass and leaves early in the morning as the surface cools. Frost is similar to dew but forms tiny ice crystals when temperatures fall below 0 degrees Celsius. Fog and mist are condensation around dust particles that can reduce visibility, with fog defined as visibility under 1 km and mist over 1 km.