Sentences with phrase «on emissivity»

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.
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