For example, a plane wing moving through
air on a windy day could be represented by a differential equation.
Parker hypothesizes that airports are mixing rural
air on windy days; I'm merely observing that airports are on urban fringes and are being folded into the urban area in many cities.
Not exact matches
The apartment was spacious very clean and well fitted out.The large balcony with a fabulous view was like having two extra rooms, and this was good
on the couple of rainy
windy days because we were sheltered but still able to enjoy the warm
air outside.
The Parker paper directly addresses your «bubbles» idea: if the UHI influence was large, then it would be larger
on still
days as opposed to
windy ones, because
on windy ones the bubble of warm
air would get blown away more readily.
On windy days, the admixture of
air from the suburban area reduces the
windy -
day temperature (so there is a calm -
day —
windy -
day signal).....
However,
on windy days, I expect the UHI effect to be vitiated by mixing of
air from outside the region of the city with the relatively warmed
air; and I expect the windiness to reduce the stratification of the boundary layer («mix it up») and thus reduce the cooling effect of the NSTI.