Higher pressure increases the temperature of
air parcels below.
Not exact matches
In nature, the dry adiabatic lapse rate of
air in the atmosphere is maintained because the system is differentially heated from
below causing
parcels of
air to constantly move up and down.
Evaporation injects potential energy into an
air parcel in the form of latent heat thereby reducing density and weight to
below the global average.
At the surface, increased pressure from injecting water vapour into a
parcel of
air via evaporation causes the
parcel to rise so that surface pressure
below it falls.
ii) If pressure within an
air parcel rises then the contents expand to occupy a larger space but that decreases density and weight which reduces pressure at the surface
below.
Evaporation initially reduces the density of the
air within a convective cell
below the global average and condensation simply restores the density within the cell to the global average so it is trite to suggest that the condensation process additionally reduces density and surface pressure outside the
parcel.
If the environmental lapse rate is larger than the dry adiabatic lapse rate, it has a superadiabatic lapse rate, the
air is absolutely unstable — a
parcel of
air will gain buoyancy as it rises both
below and above the lifting condensation level or convective condensation level.