Not exact matches
This powerful kilonova blast emits as much
visible and
near - infrared light every second as the
Sun does every few years.
«There is nearly as much energy in the far - red and
near - infrared light that reaches Earth from the
Sun as there is in
visible light,» said Bryant.
Visible features are caused by sound waves deep inside the
sun's core, and they are simultaneously shaped by the activity
near the solar surface.
«We're accustomed to seeing how our
Sun appears in
visible light, but that can only tell us so much about the dynamic surface and energetic atmosphere of our
nearest star,» said Tim Bastian, an astronomer with the National Radio Astronomy Observatory in Charlottesville, Va. «To fully understand the
Sun, we need to study it across the entire electromagnetic spectrum, including the millimeter and submillimeter portion that ALMA can observe.»
And the highest intensity of the electromagnetic radiation coming form our
sun is in the
visible and
near infrared part of this spectrum.
Here is what the IPCC stated: «The
Sun powers Earth's climate, radiating energy at very short wavelengths, predominately in the
visible or
near -
visible (e.g., ultraviolet) part of the spectrum.
The heat we feel from the
Sun is the
Sun's heat in transfer, it is not the
Sun's light in transfer, we can not feel
near infrared or
visible light.
And say ultraviolet and
visible light are small portion of LTM and LTM is mostly IR light So the
Sun is almost entirely emitting LTM and LTM is comprised of what could be called shortwave: Ultraviolet thru
visible to
Near Infrared.
Visible and near - visible radiation from the sun easily gets through, but thermal radiation from the surface can't easily get ba
Visible and
near -
visible radiation from the sun easily gets through, but thermal radiation from the surface can't easily get ba
visible radiation from the
sun easily gets through, but thermal radiation from the surface can't easily get back out.
Shortwaves from the
Sun like
visible and uv and
near infrared do not have this great power to move molecules of matter into vibration, they can not heat matter, they are classed as Light and not Heat.
In the AGW Greenhouse Effect energy budget the main wavelengths from the
Sun are
visible, a bit of shortwave uv and 1 %
near infrared.
The AGW claim from the comic cartoon KT97 and kin The Greenhouse Effect says that Shortwave, (
near UV,
visible and
near infrared, but mostly
visible) heats up land and oceans, that no longwave infrared from the
Sun gets through the invisible undefined and unexplained barrier said to be like the glass of a greenhouse, and then the Shortwave heated land and oceans radiate out longwave infrared, (which in real physics is heat, also called thermal infrared).
This is my way of showing that
Sun radiative energy is mostly in the «shortwave»
visible and
near -
visible region (about 0.3 μ to 1μ) and that radiative energy from the warmed Earth is mostly in the «longwave» infrared region (about 6μ to 20μ).
The first, the
Visible Light Window, on the left side of the graphic, allows visible and near - visible light from the Sun to pass through with small losses, and the second, the Longwave Window, on the right, allows the central portion of the longwave radiation band from the Earth to pass through with small losses, while absorbing and re-emitting the left and right po
Visible Light Window, on the left side of the graphic, allows
visible and near - visible light from the Sun to pass through with small losses, and the second, the Longwave Window, on the right, allows the central portion of the longwave radiation band from the Earth to pass through with small losses, while absorbing and re-emitting the left and right po
visible and
near -
visible light from the Sun to pass through with small losses, and the second, the Longwave Window, on the right, allows the central portion of the longwave radiation band from the Earth to pass through with small losses, while absorbing and re-emitting the left and right po
visible light from the
Sun to pass through with small losses, and the second, the Longwave Window, on the right, allows the central portion of the longwave radiation band from the Earth to pass through with small losses, while absorbing and re-emitting the left and right portions.