An object will Absorb any incident radiation based solely
on its emissivity, it does not matter where the radiation came from.
The value of tau (optical depth) and Ed / Eu do not depend
on emissivity.
It depends
on the emissivity of the atmosphere.
The amount of energy radiated depends
on the emissivity.
I used this example to demonstrate how the amount of the greenhouse effect depends
on the emissivity
Not exact matches
This study used variations in the thermal
emissivity of the surface observed by the Visible and Infrared Thermal Imaging Spectrometer
on the European Space Agency's Venus Express spacecraft to identify compositional differences in lava flows at three hotspots.
Applying aperture photometry
on the azimuthally averaged deconvolved PACS images and using a modified blackbody of the form Bν · λ − β, as expected for a grain
emissivity Qabs ~ λ − β with β equal to 1.2 (representing amorphous carbon, Mennella et al. 1998), we derived a dust temperature between 108 ± 5 K at 20 ′ ′ and 40 ± 5 K at 180 ′ ′.
Specifications: Laser sighting for accurate aiming Infrared Temperature Range -58 ° to 986 °F -LRB--50 ° to 530 °C) Infrared Accuracy ± 2 % of reading or ± 1 °F or 1 °C Selectable temperature units °F / °C 14:1 Distance - to - spot size ratio
Emissivity adjustable from 0.1 to 1.0 Bright large blue back - lit LCD display Lock for continuous temperature scanning Select Laser
On / Off Uses one 9V battery (included) to provide nominal 30 hours of continuous operation Automatic power OFF
Raytek, one of the leading infrared instrument manufactures has the following
emissivity tables
on their website.
With generic carbon blend heaters, you'll get an
emissivity rating that's significantly lower than Solocarbon heaters, making ours the most effective far infrared heater
on the market.
Just to follow - up
on John Finn's question (# 10), if one puts in a rough value for the
emissivity of the earth (whatever that might be), so one is no longer assuming it is a perfect blackbody, then does the resulting estimate for climate sensitivity correspond to what one would expect in the absence of any feedback effects?
Here's an interesting thought for the ice experts, maybe Andy could pick this up, since he's done a very decent job of following up
on my question: I've read suggestions that increased sea
emissivity from the Arctic waters would gain relative to the loss of albedo from increasingly ice - free seas.
Even assuming that the visible reflectivity of the paint is 100 %, and the infrared
emissivity is also 100 %, and ignoring that GHGs would trap some of the emitted IR, the maximum influence would be
on the order of 0.14 % (7e11 / 5e14; I hope I did the math and counted the decimal places right) decrease in radiative forcing.
The effective
emissivity from the surface of the ocean above that little millimeter or two of air gap is about 0.857,
on average, so the oceans would require a 2.18 instead of 5.35 as the multiplier resulting in 1.5Wm - 2 at the surface.
Modern aluminum curtainwalls and windows often have thermally broken frames, solar control and low -
emissivity coatings
on the glass, gas fills such as argon in the glazing space, and increasingly use insulating spacers.
Absorptivity and
emissivity are molecular properties or normalized efficiencies, while absorption and emission depend
on the number of molecules and photons explicitly, and therefore
on the environment.
The OSI SAF team focuses
on scatterometer winds (and soon microwave winds), Sea Surface Temperature (SST) and sea Ice Surface Temperature (IST), radiative fluxes: Solar Surface Irradiance (SSI) and Downward Longwave Irradiance (DLI), sea ice concentration, edge, type,
emissivity, drift.
The thickness of the convective part of the atmosphere depends
on the absorptivity /
emissivity of atmosphere but does not drop below 4 - 5 km even when the
emissivity gets extremely low.
Introduction Key diagrams
on the Earth's energy budget depicts an exchange of energy between the surface and the atmosphere and their subsystems considering each system as if they were blackbodies with
emissivities and absorptivities of 100 % 1, 2.
The real «flat plate» GHE is between 11 and 17 K depending
on your estimate of present albedo and planetary
emissivity in the absence of GHGs.
Well,
on the picture taken with the camera
emissivity set to 0.95, the twinwall temp shows 54.4 F and the painters tape 72.4 F.
IR picture showing painters tape (bright spot at 72.4 F)
on the twinwall glazing with
emissivity set to 0.95.
So, I 1) attached a surface mount thermocouple to the outside of the twinwall to measure the «actual» surface temperature, and 2) applied a roughly 1.5 by 1.5 inch piece of blue painters tape a few inches below the thermocouple — this is the often used technique of placing a patch of something with know
emissivity over an unknown
emissivity surface, and then measure the temperature
on the known patch.
The
emissivity of solid water (ice) varies from about 0.3 (reflecting much light and other radiation) to about 0.8 depending
on its crystal structure.
The absorptivity /
emissivity of surfaces may get more clearly less than one at the lower end of the LWIR region, i.e. around 4 - 5 um but that has very little influence
on the energy radiated by Earth surface, because most of the energy is radiated at longer wavelengths anyway.
The
emissivity of a substance has nothing to do with how much radiation has been reflected or absorbed
on its way to that substance.
What you really want is a wavelength selective low
emissivity coating
on your collector.
Every portion of the Earth's surface emits radiation continuously, dependent
on the temperature and
emissivity.
He argued against locating the weather station
on a nearby lawn: The
emissivity -LSB-...]
So
on the one hand, eminent warmists declare «the S - B law applies to any infrared absorbing gases»,
on the other hand, nobody can provide the S - B law's
emissivity for CO2.
To convert temperature to W / m ^ 2 requires assuming an
emissivity which depends to an incredible degree
on the choice of finish.
For example, road tar surfaces receive radiation (solar spectrum) from incident «sunlight»; some of which is absorbed and some reflected, so the surface warms, and re-radiates in a completely different thermal spectrum that depends
on the surface temperature and its spectral
emissivity.
An average cirrus
emissivity relationship between 12 and 11 μm is developed here using the Moderate Resolution Imaging Spectroradiometer (MODIS) satellite instrument and is used to «retrieve» the PSD based
on six different PSD schemes.
CO; 2 Observations of the Infrared Radiative Properties of the Ocean «[I] t is necessary to understand the physical variables contributing to sea surface emitted and reflected radiation to space.The
emissivity of the ocean surface varies with view angle and sea state, the reflection of sky radiation also depends
on view angle and sea state, and the absorption of atmospheric constituents such as water vapor, aerosols, and subdivisible clouds affect transmittance.»
And since the solar input is equal in both cases, then the initial terrestrial output would also be equal, relying only
on surface temperature (and
emissivity).
On the other hand, the atmosphere next to the Earth's surface comprises an IR emitter which has Absolute Emissivity between c. 0.6 and 0.7 depending on humidity and temperature (assumed to be the same as the surface) The «black body» amplitude, self - absorbed GHG bands shut off the corresponding wavelength emission from the surface, making its Operational Emissivity c. 0.4 to 0.
On the other hand, the atmosphere next to the Earth's surface comprises an IR emitter which has Absolute
Emissivity between c. 0.6 and 0.7 depending
on humidity and temperature (assumed to be the same as the surface) The «black body» amplitude, self - absorbed GHG bands shut off the corresponding wavelength emission from the surface, making its Operational Emissivity c. 0.4 to 0.
on humidity and temperature (assumed to be the same as the surface) The «black body» amplitude, self - absorbed GHG bands shut off the corresponding wavelength emission from the surface, making its Operational
Emissivity c. 0.4 to 0.3.
The
emissivity of the Earth is over 0.97 and a perfect black body is 1.0 so, for all intents and purposes, the Watts / m ^ 2 calculated by the Carleton spreadsheet based
on Plank's Law may be off by only a small number of Watts / m ^ 2 and my main claim is that there are hundreds of Watts / m ^ 2 streaming down from the Atmosphere, so a few Watts here or there is a drop in a bucket.
(Because of the T ^ 4 dependence of radiative power
on temperature, an
emissivity of 0.99 rather than 1 leads to ~ 0.7 deg K of change in the predicted temperature.)
This is enough to raise the surface temperature quite a bit (the exact value depends
on what assumptions you make about
emissivity & albedo).
Something I did not see in the comments was mention of
emissivity, which would have a direct impact
on the sensible temperature of the air and surface of the earth.
The earth is almost a perfect blackbody emitter in the mid & far - IR and since Kirchkoff's Law imply that the
emissivity and absorptivity must be equal at each wavelength, the means that essentially all of the radiation that is incident
on these objects is absorbed.
Hottel gives CO2
emissivity direct from charts based
on direct measurements of total emission.
More expensive ones allow adjustment of the
emissivity, or rough & ready calibration by measuring the temperature of masking tape (
emissivity ~ 0.95)
on the object to be measured, or by drilling a hole at least 6 times as deep as its diameter which approximates a blackbody (
emissivity 0.98 +).
As early as 1859, Gustav Kirchhoff proposed that «At thermal equilibrium, the
emissivity of a body (or surface) equals its absorptivity» and as far as I can understand, nobody objected and his proposition was accepted as part of «Kirchhoff's Law», and, to me, it seems logical and should be unavoidable as it is based
on «energy conservation».
Emissivity will vary greatly from year to year depending
on snow cover, clouds, crops, deforestation, etc..
Emissivities were evaluated experimentally based
on direct measurement of total emission for a number of gases including CO2 and water vapour; these gases absorbed in certain regions of the IR spectrum and this was the data which was used.
Note in Equation B that I have made explicit the dependence of
emissivity on the temperature of the atmosphere at that time, and the dependence of absorptivity
on the temperature of the surface.
All the authors
on radiative heat transfer states that the carbon dioxide
emissivity at 1000 °C is not more than 0.157; so where is the physical property of the carbon dioxide that enables it to have an
emissivity ten times higher than that of a blackbody?
The problem which Siddons high - lighted was regolith absorption and storage of heat which when gradually or suddenly released would confound an assumed surface temperature based
on an assumed
emissivity.
If H2O has less
emissivity in the radiative presence of CO2 doesn't that reduce the positive feedback from H2O which AGW depends
on.