Käännöksiä ei löytynyt valitulle kohdekielelle.
| Komparatiivi | more downsloping |
| Superlatiivi | most downsloping |
(meteorology) Air descending a slope, resulting in adiabatic warming and reduction in relative humidity.
Plateau-cooled air falls into the Makhtesh Ramon, traced by radiation fog, just after dawn. Radiative cooling of the desert highlands chills the air, making it more dense than the air over the lowlands. Cooler air can also hold less water vapour; it condenses out as tiny fog droplets, which re-evaporate as the air warms. Here, the falling air is warming adiabatically, and so the fog re-evaporates as it falls.