Not exact matches
In the icy bodies around our
solar system,
radiation emitted from rocky cores could break up water molecules and support hydrogen - eating microbes.
The visible
solar radiation mostly heats the surface, not the atmosphere, whereas most of the infrared
radiation escaping to space is
emitted from the upper atmosphere, not the surface.
The material is transparent to the visible sunlight that powers
solar cells, but captures and
emits thermal
radiation, or heat, from infrared rays.
The fluctuations between 1945 to 1975 are due to mostly human -
emitted sulphates blocking sunlight (thus counteracting the still - rising GHGS), and also due to fluctuations in
solar radiation.
The steady increase to 1940 is partly due to increases in human -
emitted greenhouse gasses, but also partly due to increases in
solar radiation.
Surface radiative energy budget plays an important role in the Arctic, which is covered by snow and ice: when the balance is positive, more
solar radiation from the Sun and the Earth's atmosphere arrives on the Earth's surface than is
emitted from it.
Solar flares are brief, rapid bursts of high - energy
radiation emitted by the sun.
...» The variable part of the
solar radiation flux is mainly
emitted by the chromospheric parts of the CAs.
The sun, which is quite hot (about 5800K),
emits most of its energy at between 0.2 microns and 4 microns (
solar or short wave
radiation, or plain sunlight), while the Earth's surface
emits the most energy at wavelengths between 5 and 50 microns (the so - called thermal Infrared region of the spectrum).
The imbalance is not between IR absorbed and IR
emitted by a layer of atmosphere, but between the incoming shortwave
solar energy from space and the outgoing longwave energy
emitted to space, due to the increasing difference between the ground temperature and the temperature of the level from which re-
emitted radiation can escape to space.
Therefore, for practical purposes, the sole source of excess heat if we increase CO2 is IR
emitted by the surface from absorbed
solar radiation,.
With some LW absorbing optical thickness, the atmosphere can
emit radiation to space, so some heat will flow into the atmosphere from where
solar heating occurs to get to space.
In the case of an increase in greenhouse gases (which cause a warming), that implies that the planet will be absorbing more
solar radiation than it
emits as longwave
radiation.
Clouds play a very complicated first order role in scattering
solar radiation as well as absorbing and
emitting terrestrial
radiation, again, the greenhouse effect.
Actually, though, most of the OLR originates from below the tropopause (can get up around 18 km in the tropics, generally lower)-- with a majority of
solar radiation absorbed at the surface, a crude approximation can be made that the area
emitting to space is less than 2 * (20/6371) * 100 % ~ = 0.628 % more than the area heated by the sun, so the OLR per unit area should be well within about 0.6 % of the value calculated without the Earth's curvature (I'm guessing it would actually be closer to if not less than 0.3 % different).
In the absence of
solar heating, there is an equilibrium «skin temperature» that would be approached in the uppermost atmosphere (above the effective
emitting altitude) which is only dependent on the outgoing longwave (LW)
radiation to space in the case where optical properties in the LW part of the spectrum are invariant over wavelength (this skin temperature will be colder than the temperature at the effective
emitting altitude).
Actually to reach a new, higher equilibrium temperature, the Earth surface (including oceans) must warm and thus the radiative budget MUST be unbalanced, less
radiation must be
emitted in space compared to the (unchanged) incoming
solar radiation.
This is why (absent sufficient
solar or other non-LW heating) the skin temperature is lower than the effective radiating temperature of the planet (in analogy to the sun, the SW
radiation from the sun is like the LW
radiation, and the direct «
solar heating» of the part of the atmosphere above the photosphere may have to due with electromagnetic effects (as in macroscopic plasmas and fields, not so much
radiation emitted as a function of temperature).
Px272 Lect 3: Forcing and feedback Balance of
solar incoming, and earth
emitted outgoing
radiation Increments.
«We see, for the first time in the field, the amplification of the greenhouse effect because there's more CO2 in the atmosphere to absorb what the Earth
emits in response to incoming
solar radiation,» Daniel Feldman, a scientist in the Berkeley Lab and the study's lead author, said in a news release.
Effectively, infrared
radiation emitted to space originates from an altitude with a temperature of, on average, — 19 °C, in balance with the net incoming
solar radiation, whereas the Earth's surface is kept at a much higher temperature of, on average, +14 °C.
If the
solar radiation is W, the surface will receive 2W, (W from the sun and W from the atmosphere), and must therefore
emit 2W.
The key is that they
emit downwards and upwards, and the downward emission adds to the surface forcing, so the surface sees several hundred W / m2 of IR in addition to
solar radiation and has to be warmer to compensate.
Because the climate system derives virtually all its energy from the Sun, zero balance implies that, globally, the amount of incoming
solar radiation on average must be equal to the sum of the outgoing reflected
solar radiation and the outgoing thermal infrared
radiation emitted by the climate system.
GHGs warm by absorbing
solar radiation and surface IR
radiation, and cool by
emitting upwards to space.
The constant gain of
solar energy by Earth's surface is systematically returned to space in the form of thermally
emitted radiation in the infrared portion of the spectrum.
Girma August 12, 2012 at 2:03 am said:» Note that assuming the
radiation energy
emitted by the earth is equal to the
solar energy it absorbs»
Note that assuming the
radiation energy
emitted by the earth is equal to the
solar energy it absorbs, we have:
It is indicated that Earth surface adsorbs 168 W / m ^ 2 of
solar radiation in visible light region, but
emits 390 W / m ^ 2 in LW region (from which 324 W / m ^ 2 is returned as «back
radiation»).
The difference between the
solar radiation absorbed and the thermal
radiation emitted to space determines Earth's
radiation budget.
The
emitted wavelengths are mainly between 5 and 100 μm (0.0002 and 0.004 inch), and they interact differently with the atmosphere compared with the shorter wavelengths of
solar radiation.
Next: «
Solar radiation at the frequencies of visible light largely passes through the atmosphere to warm the planetary surface, which then
emits this energy at the lower frequencies of infrared thermal
radiation.
That way the collector absorbs
solar radiation with high efficiency but
emits far less thermal
radiation.
It neither receives
solar radiation nor
emits infrared
radiation into space.»
Thus, long - term variations of TSI (with account for their direct and secondary, based on feedback effects, influence) are the main fundamental cause of climate changes since variations of the Earth climate is mainly determined by a long - term imbalance between the energy of
solar radiation entering the upper layers of the Earth's atmosphere and the total energy
emitted from the Earth back to space.»
Solar radiation (what the sun
emits) passes through the atmosphere as ultra violet and visible light.
So they let most of the incoming
solar radiation through but absorb most of the shortwave
radiation emitted from the surface (and at all levels).
That jibes with the idea of a cooling trend during
solar minimum; fewer spots means fewer faculae, so the Sun
emits less Earth - warming
radiation.
Sunspots and other forms of
solar activity are produced by magnetic fields, whose changes also affect the
radiation that the Sun
emits, including its distribution among shorter and longer wavelengths.
It is assumed that all the
solar radiation from relevant absorption band makes it to the CO2 boxes through all the other boxes and does this constantly with no loss and if it did the model might be correct, as it is there are tens of thousands of other boxes between each CO2 box so the absorption and the storing and the re
emitting of this narrow band can not be total or anywhere near total and the incoming source is not constant nor does all all the
solar radiation actually make it the CO2 boxes, it would only be a proportion the rest being intercepted and dissipated beforehand.
This means the Earth absorbed more energy from
solar radiation than it
emitted as heat back to space.
«Clouds also block some of the longwave
radiation that would be
emitted back to space, so that a decrease in global cloud amount would increase the amount of
solar radiation reaching the Earth's surface (more heating), but also increase the amount radiated back to space (more cooling).»
Sunspot Activity When the number of sunspots is high, the Sun
emits higher amounts of
solar radiation.
Forests also
emit large amounts of water vapour, which reflects
solar radiation back into space.
Positive radiative forcing occurs when the Earth absorbs more energy from
solar radiation than it
emits as thermal
radiation back to space.
And biomass burning — which occurs mainly as a result of tropical forest fires, deforestation, savannah and shrub fires —
emits large amounts of organic carbon particles that block
solar radiation.
29 21.3 Climate Changes Human Impact on Climate Changes The Greenhouse Effect • The greenhouse effect is a natural warming of both Earth's lower atmosphere and Earth's surface from
solar radiation being absorbed and
emitted by the atmosphere.
The ocean is a key component of the climate system, absorbing
solar radiation and exchanging, absorbing, and
emitting oxygen and carbon dioxide.
At night, the ground cools down by
emitting infrared
radiation, whereas during the day, the infrared cooling is secondary to
solar heating.
The visible
solar radiation mostly heats the surface, not the atmosphere, whereas most of the infrared
radiation escaping to space is
emitted from the upper atmosphere, not the surface.