Thanks, SoD, but what do you think of
this atmospheric radiation spectrum, recorded by Nimbus 4 spacecraft?
Not exact matches
The work is an estimate of the global average based on a single - column, time - average model of the atmosphere and surface (with some approximations — e.g. the surface is not truly a perfect blackbody in the LW (long - wave) portion of the
spectrum (the wavelengths dominated by terrestrial /
atmospheric emission, as opposed to SW
radiation, dominated by solar
radiation), but it can give you a pretty good idea of things (fig 1 shows a
spectrum of
radiation to space); there is also some comparison to actual measurements.
How can the earth be radiating a crude BB type
spectrum corresponding to the surface Temperature when Trenberth claims that only 40 W / m ^ 2 escapes to space in the
atmospheric window, and folks insist that the main body of the atmosphere (gases) does not emit thermal
radiation.
These so - called greenhouse gases absorb infrared
radiation, emitted by the Earth's surface, the atmosphere and clouds, except in a transparent part of the
spectrum called the «
atmospheric window», as shown in Figure 1.2.
Each higher and cooler layer in turn emits thermal
radiation corresponding to its temperature; and much of that also escapes directly to space around the absorption bands of the higher atmosphere layers; and so on; so that the total LWIR emission from the earth should then be a composite of roughly BB
spectra but with source temepratures ranging ove the entire surface Temeprature range, as well as the range of
atmospheric emitting Temperatures.
The incoming Sun's
radiation is 3.5 times greater in intensity than the outgoing Earth's
radiation, hence the Sun's infrared is 1.6 times greater in intensity than the Earth's
radiation and experiences the same
atmospheric absorption
spectra as the Earth
radiation.
Our recent study has focused on a molecule's radiative efficiency within the
atmospheric window region of the IR
spectrum, which can be thought of as a molecule's inherent ability to absorb
radiation in the
atmospheric window.
The absorption interval of CO2 molecules covers less than 20 percent of the
spectrum of thermal
radiation of the Earth's surface, while
atmospheric moisture absorbs thermal
radiation rather uniformly over the entire
spectrum.
But for the earth atmosphere apparently based on AIRS satellite observations, as well as computer calculations, what is seen, looking down is a clearly blackbody like
radiation spectrum, with holes in it corresponding to various
atmospheric components like H2O, CO2, and O3 primarily.