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Archive for April, 2011

One question that has intrigued me for a while – how much of the transmittance (and change in transmittance) from CO2 in the atmosphere is caused by weak lines, and how much is caused by the “far wings” of individual lines. Take a look back at Part Nine. Here is the calculated change in transmittance [...]

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In Part One we looked at the calculation of total atmospheric optical thickness. In Part Two we looked at the claim that the surface and atmosphere exchanged exactly equal amounts of energy by radiation. A thermodynamics revolution if it is true, as the atmosphere is slightly colder than the surface. This claim is not necessary [...]

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In Part One we looked at the usefulness of “tau” = optical thickness of the atmosphere. Miskolczi  has done a calculation (under cloudless skies) of the total optical thickness of the atmosphere. The reason he is apparently the first to have done this in a paper is explained in Part One. The 2010 paper referenced the [...]

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Many people have requested an analysis of Miskolczi’s theories. I start with his more recent paper:  The Stable Stationary Value of the Earth’s Global Average Atmospheric Planck-Weighted Greenhouse-Gas Optical Thickness, Energy & Environment (2010). It’s an interesting paper and clearly Miskolczi has put a lot of time and effort into it. I recommend people read the paper [...]

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The subject of atmospheric heating rates is one which is worth spending time on. What is a heating rate? To see the usefulness of a heating rate let’s consider the per capita income of a country. Per capita income compares the ratio of total $ to the total population. If we compare the total income [...]

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In Part One we saw how a very simple energy balance model with some very basic assumptions provided some insight into how the surface and atmospheric temperatures are determined. We assumed that the atmosphere was transparent to solar radiation (radiation less than 4 μm), that the atmosphere was totally opaque to terrestrial radiation (greater than 4 μm), [...]

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Most good textbooks introduce simple models to help the student gain a conceptual understanding. In Elementary Climate Physics, Prof. F.W. Taylor does the same. Now the atmosphere is mostly transparent to solar radiation (shortwave) which is centered around 0.5 μm, and quite opaque to terrestrial radiation (longwave) which is centered around 10 μm. Note that absorptivity is [...]

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In his excellent book, A First Course in Atmospheric Radiation, Grant Petty introduces a number of spectral measurements of atmospheric radiation which are very illuminating. In this article I am going to reproduce them, along with a lot of Petty’s comments and explanations – hard to improve on what he has to say. (See the [...]

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