The mean vertical distribution of temperature and the water vapor mixing ratio in the atmosphere are shown.
Figure 1 shows
the mean vertical distribution of temperature and the mixing ratio of water vapor in the atmosphere.
Not exact matches
NOAA measurements at South Pole station monitor the ozone layer above that location by
means of Dobson spectrophotometer and regular ozone - sonde balloon launches that record the thickness of the ozone layer and its
vertical distribution.
-- Traditional publishers catch a clue and go
vertical,
meaning opening stores and selling direct to customers instead of direct to the
distribution chain only.
«The global
mean climate responses to different forcings may differ because of the character of the forcings themselves (such as their geographical or
vertical distribution) and because different forcings induce different patterns of surface warming or cooling, thereby affecting the net top - of - atmosphere radiation imbalance, and thus the ocean heat uptake rate.»
The horizontal panel at the bottom shows the climate - sensitivity
distribution from before, with the
mean (3 °C) highlighted by a
vertical blue line.