Moisture that evaporates from the ocean tends to be
lighter than water vapor released into the atmosphere by plants.
Not exact matches
The air at the top of the troposphere is colder
than the air at the ground because of a.
water vapor b. expansion of gas c.
light energy d. ozone
Since
water vapor is
lighter than the main constituents of air, air containing
water vapor is
lighter and so rises above less humid air.
A parcel of air containing
water vapor is
lighter than air without as much.
This is because
water vapor is
lighter than air.
Adding the influence of
water vapor concentration to the density profile makes the difference between the densities of the two cases a little larger, because
water vapor lowers the density as H2O molecules are
lighter than average for dry air.
The
vapor pressure of this heavy
water is less
than for «normal»
light water.
The end result is there's virtually no heating beyond the first few micrometers and the molecules near the surface just keep picking up more and more energy as latent heat until they have enough energy to vaporize and then they leave the surface and quickly convect upwards because
water vapor is
lighter than air.
Dave Springer says: ``... the molecules near the surface just keep picking up more and more energy as latent heat until they have enough energy to vaporize and then they leave the surface and quickly convect upwards because
water vapor is
lighter than air.
Pekka: Your description patently conflicts with the following geophysical realities: a)
Water vapor is
lighter than air and adds extra lift to thermally forced convection.
Because
water vapor is
lighter than dry air (mostly nitrogen and oxygen), that layer of air can move upward in the attic.