tilkkondensatsiooni
Tilkkondensatsiooni, often referred to as drip condensation, is a phenomenon where water vapor in the air comes into contact with a cold surface and transforms into liquid water droplets. This process is driven by the difference in temperature between the air and the surface. When moist air touches a surface cooler than its dew point, the water vapor in the air loses energy and changes its state from a gas to a liquid.
This type of condensation commonly occurs in enclosed spaces or on surfaces that are not adequately insulated.
The formation of tilkkondensatsiooni can be exacerbated by high humidity levels and insufficient ventilation. In residential