Furthermore each constituent of an atmosphere reacts slightly differently to
incoming radiant energy.
Not exact matches
That is one of the reasons that clouds get ignored as they generally are not widespread or dense enough to be considered to have a significant impact on
incoming solar
radiant energy.
It is the density, not the composition which gives more or less opportunities for such instances of
energy transfer between molecules whilst the
incoming and outgoing
radiant energy is negotiating the atmosphere.
CO2 is an IR - reactive molecule, converting
incoming radiant daytime IR
energy to kinetic temperature
energy thereby heating the surrounding N2 / O2 (non-IR reactive) atmospheric gases.
Cloud and Earth's
Radiant Energy System (CERES) instruments aboard NASA satellites measure incoming and outgoing radiant power at the top of the atmo
Radiant Energy System (CERES) instruments aboard NASA satellites measure
incoming and outgoing
radiant power at the top of the atmo
radiant power at the top of the atmosphere.
Imbalance =
incoming less reflected solar
radiant energy minus the heat
energy from surface and atmosphere escaping to space.]