Not exact matches
This study's simulations show that the
drying rate changes according to the shape of the
air - water interface located
near the
surface.
A low - altitude flow of warm, moist
air from an ocean area combined with a flow of cold,
dry polar
air high up creates maximum instability, which means that parcels of
air heated
near the
surface rise rapidly, creating powerful updrafts.
(1) Most of the warming would actually occur
near the
surface in areas with shallow cold
dry air masses, such as in Siberia and northern Canada where it would not have a large effect.
A group of researchers at Princeton University found that wind farms may change the mixing of
air near the
surface,
drying the soil
near the site.
Tornadoes often form when warm, moist
air near the Earth's
surface rises and interacts with cooler and
drier air higher in the atmosphere.