This layer of the atmosphere forms
when radiation from the sun strips electrons from, or ionizes, atoms and molecules in the atmosphere between about 75 and 1,000 kilometers above Earth's surface.
The use of dark, nonreflective materials for parking, roofs, walkways, and other surfaces raises ambient temperatures
when radiation from the sun is absorbed and transferred through convection and conduction back to surrounding areas.
Not exact matches
The spacecraft's telescopes are sensitive to
radiation from the hot outer atmospheres of stars like the
Sun and white dwarfs, formed
when stars about the size of the
Sun reach the end of their lives.
When charged particles
from the
sun hit a planet's atmosphere, they usually create
radiation such as X-rays.
These systems are especially important
when our cells are stressed — for example,
when we are exposed to extreme temperatures or UV
radiation from the
sun — as quite a lot can go wrong if cells are unable to respond to environmental stressors.
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.
When sunlight
from the
Sun hits these solar panels, the photons exert a small but significant amount of force (
radiation pressure).
When it comes to
sun protection, spirulina has been shown to protect skin and eyes
from harmful UV
radiation.
Now,
when the energy received directly
from the
Sun at the surface of Venus is less than 10 % of what we receive on Earth, then there is less than 10 % coming back as back
radiation — far less in fact.
When sunspots are on the limb of the
Sun — just rotating onto or off of the face — the plage are prominent
from our vantagepoint, creating a significant increase in
radiation that far outweighs the dip of
radiation caused by the rest of the sunspot's transit.
Here's a hint: begins with a G. 3) So after all that blabing about moon, mercury and venus it is still hard to see how the obscure part of Venus (which is not recieving any direct
radiation from the
Sun) is still over 400 Celcius when on a plante much closer to the same sun temperatures plunge to a a hundred negative... since the Greenhouse effect does not exist it must be MAGIC, pardon me, SCIEN
Sun) is still over 400 Celcius
when on a plante much closer to the same
sun temperatures plunge to a a hundred negative... since the Greenhouse effect does not exist it must be MAGIC, pardon me, SCIEN
sun temperatures plunge to a a hundred negative... since the Greenhouse effect does not exist it must be MAGIC, pardon me, SCIENCE.
Visible light, oops, I didn't explain that, visible light is
radiation from the
Sun you can't feel but you can see, that's why we call it light, and that's why
when there is no
radiation from the
Sun it is dark, because the light has gone.
Memphis October 17, 2012 at 10:56 am Myrr
when are you going to realise that NOBODY thinks that only visible
radiation comes
from sun.
This phenomena is
when the
radiation coming
from the
sun penetrates and stays in our atmosphere longer because of ozone depletion caused by harmful gases like carbon dioxide.
When SW
radiation from the
Sun interacts with matter (the Earth, for example) it imparts energy to the receiving molecules which can increase the thermal energy of the matter — it fills the «energy gap» required to reach the next energy level (warm).
I didn't mention the obvious fact that you stated, that the heating will cease,
when the upper atmosphere warms enough to restore the equilibrium between
radiation leaving the earth and arriving
from the
sun.
When the
sun is no longer shining the surface of the earth will cool because upward
radiation is continuing, and IR is taking energy
from the earth into outer space.
Phrased differently, the previously frozen sea ice acts as an insulator between the salt water below the sea ice and the Arctic air above the sea ice — preventing BOTH evaporation losses
from the water AND
radiation losses to the 12 hours of night air
when the
sun doesn't shine.
If the south wall had a suitable overhang to block direct solar
radiation from the high summer
sun, the movable insulation could be moved partly or completely aside
when solar daylighting is desired during the daytime.