Photovoltaic cells,
which absorb photons from sunlight and convert them to electricity, operate with only 20 percent efficiency.
Two key properties of fluorophores that determine brightness are the extent to which the excitation light is absorbed and the efficiency by
which absorbed photons are converted into emitted photons.
Not exact matches
Photons that enter the crystal at one end bounce back and forth between these «mirrors» a few thousand times before they can escape,
which increases their likelihood of getting
absorbed by an atom along the way.
Crystal quantum memory devices hoard data by
absorbing photons, each of
which carry one quantum bit, or qubit, of data.
This sends the crystal into a quantum superposition, in
which many thulium ions
absorb the
photon at once and vibrate at different frequencies.
By careful construction of the avalanche region, it is possible to build an APD
which generates an output, or gain, of 1500 electrons for every
photon which is
absorbed.
TiO2
absorbs photons,
which excite electrical charges in the catalyst.
Sunlight would strike the top electrode,
which would
absorb photons and catalyse the water - oxidation process.
Upon exposing a metallic surface to electromagnetic radiation that is above the threshold frequency or threshold wavelength (
which is specific to the type of surface and material), the
photons are
absorbed and current is produced.
But
photons can only travel so far through air or optical fibers before the material
absorbs the particles, limiting the distance over
which communication is possible.
The first stage
absorbs light in the form of
photons and uses it to produce energy storage molecules,
which are then used to power the second stage,
which fixes carbon from the air into carbon - based sugars, such as sucrose and starch.
When light hits a painting, some
photons are
absorbed by pigment molecules,
which split apart.
The universe is opaque to ultraenergetic
photons, or gamma rays,
which are
absorbed by the matter and radiation that lie between their source and Earth.
(Cognoscenti will have noticed that I have skipped past a third process, stimulated emission, in
which a
photon arriving at a molecule that is already excited causes it to emit, instead of
absorbing that
photon.
Vibrational modes in molecules with three or more atoms (H2O, CO2, O3, N2O, CH4, CFCs, HFCs...) include bending motions that are easier to excite and so will
absorb and emit lower energy
photons which co-incide with the infrared radiation that the Earth emits.
The higher energy ultraviolet
photons,
which can be
absorbed by O2 molecules in the stratosphere, break that oxygen - oxygen bond and the freed oxygen can combine with O2 to make ozone (O3).
I don't have a mathematical argument for my claim, just a physical one,
which is that as
photons pass through a gas they're either
absorbed or not.
The frequency at
which photons are emitted or
absorbed is small relative to the rate of energy redistribution among molecules and their modes, so the fraction of some molecules that are excited in some way is only slightly more or less than the characteristic fraction for that temperature (depending on whether
photons absorption to generate that particular state is greater than
photon emission from that state or vice versa,
which depends on the brightness temperature of the incident radiation relative to the local temperature).
The details on a molecular level determine how likely a given transition is likely to occur — in other words, the fraction of
photons of some frequency, polarization, and direction, that are
absorbed over some path through an amount of material, and the number of
photons of the same type
which are emitted per unit time.
When you say the optical depth is the depth at
which (on average) a
photon is
absorbed, shouldn't that be
absorbed or scattered.
Does this mean it can
absorb up to 4 IR frequency
photons (hence causing vibration), after
which it effectively becomes IR transparent?
So the surface of the Earth
absorbs two identical 15 micron
photons which carry the same energy, one originates from a colder CO2 molecule and the other from the surface of the Sun.
If the CO2 simply re-emits the LW
photons it
absorbs, then how does it heat the air, that is the N and O2,
which is what the greenhouse effect does?
The GHGs like CO2 do emit
photons,
which go up and down, but they are not the
photons that they
absorb.
You do know that plant life
absorbs photons and CO2,
which is buffered by inorganic carbonate, and convert it to organic carbon.
So when a molecule
absorbs a
photon (
which, by definition results in an excited vibrational and / or rotational state) the very process of re-establishing equilibrium means that some of that energy winds up in translation.
That implies that an excited electron in a greenhouse gas molecule in the atmosphere can not radiate toward the ground unless it can «find» another electron on the surface in a ground state
which is capable of
absorbing the
photon which is to be radiated.
The proposition is that every
photon that is emitted is certain to be
absorbed at some location in the universe and that an electron can not emit except when in resonance with another
which can
absorb.
Most
photons are
absorbed lower down and cause molecules to evaporate indirectly by providing energy to the skin layer,
which is then available to the evaporating molecules via convection and conduction.
Plants
absorbs high energy
photons,
which results in the combining of CO2 and H20 into CH2O and O2.
So in the Earth surface up there will be a reasonable flux of 15um
photons which can be
absorbed to increase the active population.
Phil, what do your calculations give for the distance in
which the first - generation
photons from the Surface up into the atmosphere are
absorbed to extinction in CO2's case?
In
which case the water vapor associated GHE is due to directly
absorbed photons?
So Gavin, you are claiming that in the GHE when a
photon comes in it sits around in the air until man releases CO2
which results in warming
which results in more water vapor
which THEN
absorbs the energy
photon to create feedback?
As I understand AGW, the theory goes that added CO2 combines with an energy
photon (ie the greenhouse effect) to warm the world, & heat the air
which results in more water vapor
which absorbs more
photons which results in Man caused warming feedback.
Calculations need to be done
which shows how many more
photons are
absorbed which cause how much more collision interactions, since this is where the heat comes from in the atmosphere.
ANY electro - magnetic radiation (waves or
photons), of ANY wavelength is capable of giving rise to waste «heat» when
absorbed in the proper medium; but THERMAL RADIATION is a special kind of EM radiation
which is produced entirely because of the mechanical oscillatory modes of ordinary materials, and is dependent on the Temperature for its characteristic Spectral envelope.
The discrete energy levels can only
absorb the exact wavelength corresponding to their energy separation, they don't
absorb a
photon which has too much energy and then discard the excess!