Since warmer air can hold more moisture,
the same air parcels are now farther from their moisture capacity.
Not exact matches
The «old» and «new» CO2 in an
air parcel is at the
same temperature.
A warm
parcel of
air will radiate more than a colder
parcel, even at the
same 390 ppm of CO2 in the
air due to the population of the different rotational and vibrational energy states of the GHGs from collisions with other atmospheric molecules in the LTE limit.
The
parcel of
air changes its own temperature and pressure at the
same rate as the temperature and pressure of the surroundings changes.
«Take two identical volumes (
parcels) of
air, taken from somewhere at a midlevel in the troposphere, with each
parcel containing an identical number of gas molecules and the
same amount of heat energy to start.
The constant speed moving
parcel of the ideal gas is the
same solution as still
air for hydrostatic equilibrium.
As it rises the
parcel of
air loses energy and expands until the temperature is the
same as the surrounding
air.
The expansion laterally increases pressure laterally but pressure from above stays the
same because even if the atmosphere were to expand there would be the
same number of molecules above the
air parcel.
Once it expands it pushes against the adjoining
parcels so pressure increases in the horizontal plane but pressure in the vertical plane remains the
same so the expanded and lighter
air parcel moves in the direction of least resistance which is upward.
Again, pressure in the vertical plane stays the
same so the contracted and heavier
air parcel moves in the direction of least resistance which is downward.
Since liquid water weighs the
same as the water vapor it condensed from, there is no change in the weight of the column of atmosphere above our
parcel of
air, whence the pressure remains unchanged, although the
parcel may change (very slowly) in volume.
Given two almost identical
parcels of
air at the
same temperature and pressure, the one with more water vapor will be less dense.