Images from the latter can show
how ozone amounts differ from season - to - season and how clouds are formed over volcanoes on the planet.
Not exact matches
«While
ozone depletion from dichloromethane is currently quite modest, it is uncertain
how the
amount of this gas in the atmosphere will change in the future.
The experiment would have the same
amount of energy in each case; but
how efficient each frequency energy would alter the temperature of, say,
ozone.
There was one WUWT thread which discussed the organic molecules plankton puts into the air, and
how they can reach the upper atmosphere, and, (because they included elements ending in «ine,» such as Bromine, Fluorine, Chlorine, and Iodine,) alter the
amount of
Ozone, which in turn effected the types and powers of sunlight.