Or in other words, what's
the proportion of albedo loss relative to CO2 forcing?
Not exact matches
What's more, many other human activities, from building cities to planting crops, alter
albedo, and these activities have a much greater impact because they affect a far greater
proportion of Earth's surface.
What other things in the Earth system will change when it warms up that will affect how much SW radiation is reflected back into space [eg ice -
albedo feedback, cloud changes] or affect what
proportion of emitted LW radiation is allowed to escape to space [eg Water Vapour, cloud changes].
«Models fail to reproduce the observed annual cycle in all components
of the
albedo with any realism, although they broadly capture the correct
proportions of surface and atmospheric contributions to the TOA
albedo.»
Albedo is the
proportion of incoming radiation that is reflected from surface back to where it came from.
According to the ice -
albedo feedback mechanism as the Earth warms more ground and water would be uncovered which would absorb a higher
proportion of the incoming solar radiation thus raising the temperature and melting more ice and snow.
Albedo is the
proportion of solar radiation reflected back into space.
The
proportion of incident radiation reflected by a substance is called its
albedo.
The central business districts
of some urban areas can therefore have quite high
albedo rates (
proportion of light reflected);
The definition
of albedo is the
proportion of reflected SW.
Which means that the
proportion of heat in the ocean as opposed to the atmosphere might be slightly different (big deal because the oceans store so much heat), that
albedo might be slightly higher because you have less areas covered by forests which are darker than clear land and thus absorb more sunlight, and so on.