Consequently, the reduction in water vapour in the upper atmosphere offsets both the increase in CO2 and the increase in water
vapour near the surface.
Not exact matches
The NASA / ESA Hubble Space Telescope has discovered water
vapour erupting from the frigid
surface of Jupiter's moon Europa, in one or more localised plumes
near its south pole.
[41] The water
vapour content of the air between the top of the air and the altitude of pressure P (atm) is decreasing roughly like P4.5 [42]: hence 80 % of the total water
vapour is between P = 1 and P = 0.75
near 2.3 km, and the total water content of the air closely follows the
surface temperature.
Water
vapour content is largely a function of temperature, particularly ocean
surface and
near -
surface temperature.
That increases the CO2 levels
near the sea
surface (but that is readlily dispersed by convection, as good as the water
vapour).
However, in the deep tropics, where the theoretical effects on the
surface energy budget of temperature - driven changes in evaporation and water
vapour are particularly strong, there is a
near quarter century record of both SST and tas from the Tropical Atmosphere Ocean array of fixed buoys in the Pacific ocean.
Clouds and precipitation are affected through modifications of the temperature and water
vapour content of
near -
surface air.