High clouds reflect light, cooling the earth, while lower clouds trap heat.
Not exact matches
At a
high enough electron density, each
cloud reflects high - frequency radio waves like a mirror.
During the dry season, with no fog layer to
reflect sunlight, the smaller
cloud cover allows plants to receive much
higher radiation, increasing evaporation and photosynthesis rates, another process missed by the GCMs.
Indeed, conventional wisdom held that
higher levels of aerosol pollution in the atmosphere should cool the earth's climate because aerosols can increase cloudiness; they not only reduce precipitation, which raises the water content in
clouds, but they also increase the size of the individual water droplets, which in turn causes more warming sunlight to be
reflected back into space.
And one other piece of bad news: Warming
clouds tend to shift
higher in the atmosphere, where they trap more heat while
reflecting no more sun than they would have lower down.
This user - friendly activity has students do some informal free - writing in response to an educational film, then
reflect on their writing usingword
cloud» rpus christi, txcatholic online) in his poemthe virgin,» the poet william wordsworth praised the blessed virgin mary with the following words:
cloud computing is an information technologyit) paradigm that enables ubiquitous access to shared pools of configurable system resources,
higher - level dating word
cloud stock illustration.
The
higher - frequency «solar photons», if
reflected by something on the surface (be it an ice - sheet, a body of water, or someone's windshield) will happily change course and zip right out of the atmosphere again, completely unaffected by GHGs (though not by
cloud, of course.)
But a change of -1.7 % in (
high level)
clouds over 1 decade caused a change of 1.2 W / m2 in
reflected SW and ~ 3 W / m2 more IR radiation to space over the 30N / S band.
Well, these days 107 W / m ^ 2 of solar forcing energy is
reflected back into space by
high clouds (77 W / m ^ 2) and the surface (30 W / m ^ 2).
And, as the satellite observations of Spencer and Braswell showed, as the planet warms over a period of several months,
clouds act as a net negative feedback (the
reflecting low - altitude
clouds increase more than the absorbing
high - altitude
clouds with warming).
I know a
cloud reflects high energy sunlight up, lessening the heat influx and
reflects IR radiation from the surface and so increasing the IR influx.
The rising zones, meanwhile, soar
high into the atmosphere, and contain
clouds of ammonia ice crystals that
reflect sunlight, and block the view of the darker layers below, just like
clouds here on Earth.
I believe the IPCC claim that
high cloud is a positive feed back (traps heat) and low
cloud is a negative feed back (
reflects sunlight) and following IPCC simple logic we find that AGW will cause less rain and more droughts sooooooooooooooooo if we have less rain we have less low
clouds therefore we must have more
high cloud.
The fact that the actual measured planetary warming is less than the lowest IPCC model prediction warming and is found only at
high latitudes (which is not predicted by the IPCC models) logically supports the assertion that the planet's response to a change in forcing is to resist the change (negative feedback, planetary
clouds in the tropics increase
reflecting more sunlight in to space) rather than to amplify the change (positive feedback) due increased water vapour in the atmosphere.
As the planet warms, increasing levels of water vapour in the atmosphere caused by
higher evaporation levels form more
clouds and snow increasing the albedo of the planet,
reflecting heat back into space more efficiently, thus working to regulate the temperature downward.
If it gets too hot, the oceans heat up, evaporation increases,
high altitude
clouds form, and they
reflect back sunlight and shade the surface more, compensating and regulating temperatures so that life survives.
The IR peak in El Nino
reflect the
higher tropospheric temperature and relatively reduced
cloud cover in the central Pacific.
Studying Chinese summer thunderclouds the researchers found that an increase in aerosols led to larger and more persistent convective
cloud systems, with larger anvils at several kilometers of altitude that may
reflect more sunlight, but trap even more heat — as their
high - resolution model showed.
However, in the Southern Ocean around Antarctica, the
high - altitude
clouds usually clear out of the way to reveal lower altitude
clouds below — which continue to
reflect sunlight from their white tops, causing little effect on the solar radiation reaching the surface.
In general,
high clouds cool the climate during the day, by
reflecting the Sun's light, but warm it during the day and night by trapping heat lost from the Earth's surface — the net effect is one of warming.
The statement of P&B is somewhat odd as the
high - latitude marine areas are almost continuously covered by low
clouds; and for the cloudless case the Fresnel formulas show that the light from a Sun low over the horizon is
reflected almost as much by water than by the irregular surface of the ice pack.
Like other
high, thin
clouds, contrails
reflect sunlight back into space and cool the planet.
However, the ENSO total
cloud cover correlations more accurately
reflect its mid-level and
high - level
cloud cover patterns for land, with a correlation coefficient of 0.135.
Quite off the mark, surface temperatures are mostly average because there is still some ice
reflecting sunlight, but sunlight is very intense due to low
cloud extent and
high sun elevations, and does not show immediately above the ice, but further up.
Clouds with low bases are most efficient in reducing the daytime maximum temperature and DTR mainly because they are very effective in
reflecting the sunlight, while middle and
high clouds have only moderate damping effects on DTR.
But, the amount of energy deposited is also low, as
clouds have a
high albedo,
reflecting some fraction of the energy back to space and absorbing another fraction, which heats the air above the surface.
«These
clouds account for the
high reflectivity of Venus, but because they also
reflect infrared back to the surface (unlike water
clouds, which absorb and emit)»
(The graphic does not account for the portion of Sunlight that gets through the Atmosphere, and is then
reflected back to Space by
clouds and other
high - albedo surfaces such as ice and white roofs.
(2) A portion of the Sunlight is
reflected by
clouds and other
high - albedo surfaces and heads back through the Atmosphere towards Space.
When H2O concentration gets
high enough, water condenses out, forming
clouds, which block /
reflect sunlight (this is NEGATIVE feedback) reducing the temperature of the earth.