Friday, July 21, 2017

The Gassy Messenger

The Gassy Messenger.


Modern climate science's fundamental premise (or assumption) is that the greenhouse gases (around 2% of the atmosphere) absorb radiant infrared (IR) heat (as derived by IR spectroscopy), and are a main climate driver because of this specialty. This premise has its origins with the John Tyndall 1859 thermopile infrared detection experiment. The (other) non-greenhouse gases (N2 nitrogen and O2 oxygen) are distinguished from the greenhouse gases by their (said*) inability to absorb (infrared) heat, as deduced from the same experiment: here absorption is confused with opacity.  Raman spectroscopy (a complement to IR spectroscopy) challenges this greenhouse gas non greenhouse gas paradigm, and reveals this assumption and conclusion from any IR spectroscopy measurement to be false. It can be shown that N2 and O2 are, due to their symmetric vibration totally transparent to all IR detectors, but are not transparent to Raman detectors. Ramon Spectroscopy shows: CO2  and the other greenhouse gases to be typical, and not special; and that N2 and O2 to be greenhouse gases. Further claims are also challenged with respect to CO2 special properties in this entry.  The only valid co-efficient or method to measure a gases heat absorption is by Specific Heat Capacity: where CO2 is a poor contender.   


In an earlier entry I cataloged where CO2's heat trapping property should but doesn’t repeat. Having found that CO2 doesn’t repeat (at least at any significant level so as to be measurable or notable) in this entry I am attempting to explain why CO2's heat trapping doesn’t repeat: why is it that we think it does. My conclusion is very disturbing: the foundation argument or premise of 'heat trapping, climate changing, CO2 does not appear to be consistent with the related fundamental laws and textbook knowledge of physics. I have found all of the foundation arguments can be (easily) challenged, just by studying these laws in detail. Inspired by the work of Galileo, I am tempted to call this entry ‘The Gassy Messenger’, but have opted for the said Dark Climate.


Below is a typical reference to a greenhouse effect definition:
Although Earth's atmosphere is 90% opaque to long wave IR radiation, the vast majority of the atmosphere is not composed of gases that cause the greenhouse effect. Molecular nitrogen (N2) and oxygen (O2) make up roughly 98% of our atmosphere, and neither is a greenhouse gas. So, although the greenhouse effect is very powerful, a very small fraction of Earth's atmospheric gases generate the effect.

This greenhouse effect definition is developed and argued from the following experiments or theoretical claims (and others).
One by one, in this entry I shall attempt to address all of them. 
1. The 1859 Tyndall experiment: which uncovered and determined specific atmospheric gases as IR 'absorbent', now known as the greenhouse gases; 
2. N2 and O2 have no dipole, so they are not greenhouse gasesreference
3. CO2 heat camber experiments: which demonstrate how the gas of  CO2 temperature rises faster than 'air', when in isolation, and when heated;  
4. CO‘s molecule structure: explanations suggesting it is the molecule structure (internal degrees of freedom) that determines the heat trapping ability of CO2.
5. The far infrared re emission (of heat energy).
6. Emphasis on Radiation, implied low emphasis of conduction and convection.

From these experiments and demonstrations a climate axiom is formed, the greenhouse effect.
However strong the findings of these experiments and demonstrations, they pose an atmospheric problem, paradox, even catastrophe. How can atmospheric convective phenomena - the likes of the sea breeze - be explained with the (heat trapping) greenhouse gas axiom? The greenhouse gases (water vapour, CO2, ozone, and methane) constitute only (around) 2% of the Earths atmosphere compared with the remaining 98% non greenhouse gases (molecular Nitrogen and Oxygen).
This axiom begs the question: if oxygen and nitrogen are non-greenhouse gases because they have no IR heat ‘blocking’/ absorbing signature, then how is it that the atmosphere is warm at all?
The sea-breeze used to be - and still is in any standard geography or aviation meteorology textbook - that when a ‘parcel’ of ‘air’ (which contains all the gases in the atmosphere) is heated by the land, it become less dense, rises, and this rising draws cold air in from the sea.  How can this sea breeze be explained when around 98% of the gases of air are non-heat absorbent, and have no heat relationship?
From other similar paradoxes in physics: the mysterious Dark Energy and Dark Matter, I chose to term this climate greenhouse paradox ‘the dark climate', and its 'dark gases’, and have set out to try and explain how this paradox is so. Where have the gases of our atmosphere gone?’ Why are they thermal neutral? Either the greenhouse gas axiom is right (and if this so, we must except this dark climate paradox), or the axiom are wrong and their founding experiments misinterpreted or misattributed. 

In this (following) entry I shall go through each experiment, one by one, and show that the assumption is wrong, and that each experiment is either wrong, misinterpreted or misattributed. I shall conclude that the (total) atmosphere is made up of only Greenhouse gases – i.e. that oxygen and nitrogen are also heat absorbent. I will show that COis thermally typical, and not at all special - and restore the textbook sea breeze explanation (not that it had changed). 

1. The 1859 Tyndall experiment: IR spectroscopy

It was the – little known –1859 Tyndall experiment that first identified and isolated what he interpreted to be, and what we now know as the greenhouse gases. Below is a summary of his experiment, note that oxygen and nitrogen were found not to (what he thought at the time to) ‘absorb’ infrared.  To this day it is inferred by this experiment that greenhouse gases are by nature, infrared absorbing.
Tyndall explained the heat in the Earth's atmosphere in terms of the capacities of the various gases in the air to absorb radiant heat, also known as infrared radiation. His measuring device, which used thermopile technology, is an early landmark in the history of absorption spectroscopy of gases.[7] He was the first to correctly measure the relative infrared absorptive powers of the gases nitrogen, oxygen, water vapour, carbon dioxide, ozone, methane, etc. (year 1859). He concluded that water vapour is the strongest absorber of radiant heat in the atmosphere and is the principal gas controlling air temperature. Absorption by the other gases is not negligible but relatively small. Prior to Tyndall it was widely surmised that the Earth's atmosphere has a Greenhouse Effect, but he was the first to prove it. The proof was that water vapor strongly absorbed infrared radiation.[8] Relatedly, Tyndall in 1860 was first to demonstrate and quantify that visually transparent gases are infrared emitters.[9] 

In the following clip Dr. Ian Stewart demonstrates the basic Tyndall experiment.

 Tyndall’s experiment can easily be repeated and his findings reasoned in a modern context – just as we can Galileo’s 1609-1610 telescopic observations of the Moon, Jupiter, and Venus. The apparatus used is the readily, and relatively cheaply available in the from of the non-contact infrared thermometer or by its more advanced relative, as shown in the clip above,  the thermal imaging camera. Though these modern day ‘gadgets’ are more advanced and more adjustable than that available in Tyndall’s time, they operate using the same sensor technology, the thermopile
Youtube clip of the thermopile: 


The following gives some detail to the thermopile and makes the link to today’s common IR detectors.
A thermopile is an electronic device that converts thermal energy into electrical energy. It is composed of severalthermocouples connected usually in series or, less commonly, in parallel.
Thermopiles do not respond to absolute temperature, but generate an output voltage proportional to a local temperature difference or temperature gradient.
Thermopiles are used to provide an output in response to temperature as part of a temperature measuring device, such as the infrared thermometers widely used by medical professionals to measure body temperature. They are also used widely in heat flux sensors (such as the Moll thermopile and Eppley pyrheliometer)[1][2][3] and gas burner safety controls. The output of a thermopile is usually in the range of tens or hundreds of millivolts.[4] As well as increasing the signal level, the device may be used to provide spatial temperature averaging.[5]
Infrared Thermal Imaging Cameras or Infrared Cameras are essentially infrared radiation thermometers that measure the temperature at many points over a relatively large area to generate a two-dimensional image, called a thermogram, with each pixel representing a temperature.

1.1 Limitations of IR detectors

 Today could be said to be the age of infrared: we use it in many applications including meteorology and astronomy; it allows us to ‘see’ where we are otherwise blind.
But to use it, the operator should have an understanding of the underlying (laws of) physics the IR instrument responds to. They must understand its limitations; just as a pilot understands the limitations of an altimeter or compass and how they too can give misleading information.
To cover this new knowledge these limitations, all IR measuring instruments come with an operating manual, that are readily available to read on the Internet. There are also training videos such as the one below on IR camera's and transparency.

What these publications spell out (among other things such a opacity and transparency) is that the instrument measures infrared radiation and not temperature, and that they only read what the instrument can ‘see’ (at the set frequency). This is to say: if at the set frequency of the instrument something is opaque to IR, it can see it, and it can therefore measure it; and if something is transparent, it cannot see it, and therefore cannot measure it. 
As with the above clip, one operating manual that clearly spells this out (and more) is the ‘infrared basics’ manual found on the internet – from which I shall paste the most relevant.

Selective Emitters
“Infrared energy is an electromagnetic energy, just like visible light, radio waves, and x-rays. If I shine a flashlight at my chest it does not go through, but if I shine an x-ray at my chest it goes right through. The only difference between visible light and x-rays is the wavelength. So, by changing the wavelength of measurement, some objects may be more or less transparent at some wavelengths, and more or less opaque at others. Glass is a good example of this. Glass is transparent at short wavelengths, but is opaque at wavelengths longer than about 4.8 microns. Because glass is highly transparent at short wavelengths, this means that thin glass has a low emissivity value at short wavelengths. Because glass is highly opaque at long wavelengths, this means that glass has a high emissivity value at long wavelengths. The reflectivity of glass varies with wavelength, too. Glass is both opaque and highly non-reflective at wavelengths between about 6.6 and 8.2 microns, and so this is the wavelength band where glass has the highest emissivity value and where glass most closely approximates a blackbody material. (Page 7)
Thin film plastics are the classic example of selective emitters. These materials are made up of long chains of hydrogen and carbon atoms. The repetitive and uniform molecular structure of these materials means that the molecules and atoms all vibrate with a uniform series of harmonic frequencies. Infrared wavelengths coincident with these harmonic frequencies are preferentially absorbed (not reflected or transmitted) by the plastic material, and conversely, these materials emit infrared energy preferentially at the wavelengths coincident with these harmonic frequencies. When we look at a plastic sandwich bag we can see right through it, but if our eyes were filtered at 3.43 microns, which is the harmonic frequency for the H-C atomic bond, then the sandwich bag would appear completely opaque. When measuring the temperature of a selective emitter it is critical that a wavelength be selected to coincide with a strong emission band. This is a wavelength where the infrared emissions approach blackbody conditions, and where the material is highly opaque and non-reflective. Other examples of selective emitters are all gasses, and all highly transparent materials. Many crystalline materials, such as silicon and engineered ceramics, are also selective emitters. The uniformity and geometry of the molecular structure dictates the emissive nature of the material. Thin film coatings also act like selective emitters. In the metals industry, metal strips are often coated with a thin film. Oil-based paint, water-based paint, oil and wax are all examples of thin film coatings that can act like selective emitters. These materials are highly transparent at some wavelengths, and they are highly opaque and non-reflective at other wavelengths. The emissivity of the coated material is therefore highly influenced by the wavelength of measurement. The optimum wavelength of operation for an infrared thermometer will vary depending upon the coating material, the thickness, the required temperature range, and the need to view the coating or to view through the coating.

Without this theory, measurement would seem like a kind of magic, especially when measuring the temperature of a warm object through glass as opposed with through thin air.  One only has to look at police night vision images of culprits hiding under plastic covers thing they are safe and hid  - not so in the infrared.
In light of this theory, and application of modern day instruments, the early Tyndall conclusions seem to be outdated: his conclusions need updating.

1.2 The Tyndall / Dr Stewart IR thermopile experiment revisited:

This clip, and the original 1859 Tyndall Experiment, is not a demonstration of heat absorption, but rather a demonstration of the physical transition properties of (infrared) light and its affect on different substances.

What we see is the image of a flicking candle in the IR camera, and as the CO2 is let into the (sealed) cylinder the bright candle image turns to a blue colour. It is concluded, just as Tyndall did that the CO2 absorbs the infrared or is accentually trapping the heat from the candle. From the above literature and application of the instrument and alternative conclusion should/could read: The bright candle image turns to a blue colour as the CO2 is opaque to the infrared the frequency the camera is measuring at and that the gases before the CO2 is let in are transparent at that frequency. To test this reasoning we could have equally placed glass in front of the candle and got the same of similar result as the CO2  It should be noted that Tyndall used rock salt crystal to contain the gases – rock salt crystal is transparent at that frequency. In the Stewart demonstration rock salt is not used, but (IR transparent) thin plastic ‘clean full’ is. This can clearly be seen at time.. That the image colour turned blue shows the detector measuring the IR radiation emitted from the CO2  and thus its temperature. We could deduce from the colour that the CO2  that it is cold (which it should be coming from a pressurized state) or at least the temperature of the ambient gases it displaced.
 If this interpretation is wrong, then we could equally conclude that window glass is a equally ‘greenhouse’ solid just as CO2  is a greenhouse gas. We don’t, it isn't.

2. N2 and O2 have no dipole, so they are not greenhouse gases.

This is the claim that excludes N2 and O2 as being a so called greenhouse gas:

Nitrogen (N2) is symmetrical AND made of identical atoms.Even with rotation or vibration, there is no unequal sharing of electrons between one N atom and the other. So N2 has no dipole, and an EM photon passes by without being absorbed. Similarly, for O2. reference

Yes N2 and O2 are both transparent to IR spectroscopy, but this fact it begs the question (as stated above): how can the atmosphere be warm if 98% of it (N2 and O2) are not IR (heat) ‘absorbent'? How can N2 and Obe non greenhouse gas, yet they have a heat capacity coefficient?
Something must be wrong with this conjecture. 
To solve this paradox an alternative measuring instrument or method other than IR spectroscopy must be sourced to reveal the true IR properties of N2 and O2 (and all other gases). Such an instrument does exist, Raman spectroscopy.

2.1 Raman Spectroscopy

Raman Spectroscopy is a known complement to IR spectroscopy for analysing the vibrational properties of substances: it ‘sees’ what IR spectroscopy can't. reference
Raman spectroscopy is well explained in the following clips. I suggest you play them more than once to yourself as they are very insightful and offer perfect solution to the dark climate paradox.

Youtube clip on Raman spectroscopy
Youtube clip on IR vs Raman spectroscopy 

 2.2 N2  and O2 Raman Spectroscopy

A hypothesis was set: N2 and O2 have an infrared signature. To confirm this hypothesis either an experiment with a sample of the  atmosphere would be conducted measuring for  N2 and O2 in the IR region of the EM spectrum, or secondary research would point to a similar result. In the absence of an experiment, secondary results were searched using a google image search with the key words Raman spectcoscopy atmosphere. A positive image ('Fig. 11' below) was quickly found.  This figure and its caption clearly comes from an unrelated journal publication, but the image reveals what many others in the same search reveal - such as:  Heat Treating: Proceedings of the 16th Conference.Jon L. Dossett, Robert E. Luetje, 1996 page 228.

'Figure 11: Resonance Raman spectrum from outdoor measurement on nitro methane in vapor phase at an irradiation wavelength of 220 nm. The sample temperature was approximately 328 K, the outdoor temperature was 274 K, and the atmospheric pressure was about 755 Torr. The spectrum was accumulated during 1000 laser pulses.'

Notable are the Oand Npeaks at wavenumber 1556cm-1 and 2331cm-1 respectively. These wavenumbers correspond to wavelengths 6.43 microns and 4.29 microns respectively - in the near infrared region of the EM.
Another image found is the below (Fig. 18) showing again the 1556 O2,  and other peaks at higher wavelengths along the spectrum.
Fig. 8. 
UV Raman spectra are shown at 300 and 93 K in 18O2 atmosphere for the Fe/MFI sample exchanged with NaOH and then subsequently exchanged with NH4+ and reduced in hydrogen. At 300 K the band corresponding to peroxide oxygen increases and the band corresponding to superoxide decrease relative to their intensities at 93 K (51).

From these images it can be concluded that N2, and O2 (and other gases) are infrared opaque or absorbent, and are too greenhouse gases.  
To verify that the above observation is rational, and predictable a cause or explanation to these 'peaks' should be sourced. To do this I simply had to show the vibration mode for both N2 and O2 are symmetrical. As the quote said at the top of this section said 'Nitrogen (N2) is symmetrical AND made of identical atoms'  I had part of an answer, but with another google search I found this direct to my question academic reference: Chemistry 362 Dr. Jean M. Standard

3 . Are the stretching modes of the diatomic molecules O2 and N2 infrared active? Why or

why not? Are the stretching modes of O2 and N2 Raman active? Why or why not?

The stretching mode of a homonuclear diatomic molecule does not lead to a change in the dipole moment of the
molecule; hence, the stretching mode is not IR active.
The stretching mode of a homonuclear diatomic molecule does lead to a change in polarizability of the molecule;
hence, the stretching mode is Raman active. Another way to consider this is that since O2 and N2 possess
centers of symmetry, the stretching mode must be Raman active because it is IR inactive.

It should be noted that the very fact that Nitrogen (N2) is symmetrical AND made of identical atoms is the reason it is transparent to IR spectroscopy: it is symmetrical by nature, and so will never show up, as a law of physics, even in part, like other molecules such as CO2 .

2.3 Conclusion

I can only conclude that N2 and O2 are not at all IR transparent, it is an instrumentation and knowledge problem.
If this Raman spectroscopy discovery is found true, then the 2% (volume) of said greenhouse gases should be revised and relegated to 100%, by adding N2 and O2 (and others if so). Any assumptions or premises made by any climate models, climate knowledge, or claims that the atmosphere consists of around 2 % (volume) special greenhouse gases will need reviewed – as said above.

3. CO2 heat camber experiments: which demonstrate how the gas of  CO2 temperature rises faster than 'air', when in isolation, and when heated;  

Yet to be developed.
In brief: these experiments demonstrate CO2 's relatively low heat capacity. These experiments should be conducted with a hypothesis testing the heat capacity of CO2 compared to air and rising temperatures.

4. CO‘s molecule structure: explanations suggesting it is the molecule structure (internal degrees of freedom) that determines the heat trapping ability of CO2.

Yet to be developed:
In brief, this claim is halted by the following fact: '...the resulting specific heat capacity is a function of the structure of the substance itself. In particular, it depends on the number of degrees of freedom that are available to the particles in the substance, each of which type of freedom allows substance particles to store energy.

5. The far infrared re emission (of heat energy).

Yet to be developed:
In brief, there is relatively low (heat) energy the far infrared.

6. Emphasis on Radiation, implied low emphasis of conduction and convection.

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