Not exact matches
A measure of the difference
in sea level
pressure between the western (e.g., Darwin, Australia) and central / eastern (e.g., Tahiti) equatorial Pacific, representative of the east - west
changes in atmospheric circulation associated
with the El Nino / Southern Oscillation phenomenon.
«West Coast sea surface and coastal air temperatures evolved
in lockstep
with changing patterns of
atmospheric pressure and winds.»
Therefore, the August - Roche - Magnus equation implies that saturation water vapor
pressure changes approximately exponentially
with temperature under typical
atmospheric conditions, and hence the water - holding capacity of the atmosphere increases by about 7 % for every 1 °C rise
in temperature.
But, just
in case you were semi-serious:
With oceans covering 70 % of the earth's surface, you could never
change atmospheric humidity — water vapor
pressure is a function of
atmospheric temperature, increasing as temperature rises.
Dynamical effects arising from
changes in atmospheric pressure also play a role
in distributing meltwater, as do geostrophic ocean currents that flow along the lines where
pressure gradients are counterbalanced by the Coriolis effect associated
with the Earth's rotation.
The seasonal climate may relate to
changes in the ocean circulation pattern prior to 4.6 Ma that resulted
in an increased temperature and
atmospheric pressure gradient between the east coast of North America and the Atlantic Ocean, but this climate phase seems to be only a temporary condition, as underlying and overlying sediment are both consistent
with drier conditions.
The physics that must be included to investigate the moist greenhouse is principally: (i) accurate radiation incorporating the spectral variation of gaseous absorption
in both the solar radiation and thermal emission spectral regions, (ii)
atmospheric dynamics and convection
with no specifications favouring artificial
atmospheric boundaries, such as between a troposphere and stratosphere, (iii) realistic water vapour physics, including its effect on
atmospheric mass and surface
pressure, and (iv) cloud properties that respond realistically to climate
change.