Skip to content

Surface heating

How much of the sunshine ends up heating the air.

Surface heating over southern Germany on a strong summer day, as SoarScope shows itSurface heating over southern Germany on a strong summer day, as SoarScope shows it

Surface heating shows how much warmth the ground passes to the air above it, in W/m². That warmth is what starts thermals.

More heating means more energy for thermals. It follows the sun through the day, peaks around midday and drops in the afternoon.

Not all sunshine becomes heat in the air. Part is reflected, part goes into the ground, and part is used to evaporate water. Dry ground, bare fields and sunny slopes heat the air best; wet ground, forests and shaded slopes less. Cloud cuts the sunshine before it arrives. See Thermals.