John Murrell's Weather for Astronomy pages
Sky Transparency or Aerosol Optical Depth
( and a bit about air masses and scattering)
29th June 2018
Updates and new link
Have you ever wondered why on some cloud free nights you can see forever - well as far as Andromeda (M31) our neighbouring galaxy and on some nights while there are no clouds you can see very little ? One of the principal reasons is that the sky transparency varies from night to night depending how transparent the air is over your observing site. Transparency should not be confused with 'seeing' which is how steady the air is, poor seeing will cause the image of a star to move and planetary detail to be invisible.
This page was inspired by the article on 'Clear(er) Skies Ahead' in the August 2008 edition of Sky and Telescope. As usual this article while explaining the technicalities quite well is heavily biased to observers in the USA and Canada. The Internet resources referenced in the article only contain data on Sky Transparency in North America and do not cover Europe. This page is designed to redress this balance and provide some links to resources that cover the UK & Europe.
This page is a child of my Weather Page that contains many more resources related to Weather for Astronomy.
Sky Transparency or Aerosol Optical Depth (AOD) is where Meteorology and Astronomy meet as a result terms from both sciences appear on this page. As a result there is the potential for confusion as both use the phrase Air Mass to mean different things !
There is also confusion between the use of altitude for altitude (i.e. angle) of the object being observed and altitude as the height of the observer above sea level. In some cases elevation is used for the height of the observer above sea level but you need to check.
Astronomical and Metrological Air Masses
In Astronomy Air Mass is the amount of air that you observe through. Assuming that you are observing from near Sea Level if you observe vertically upwards ( your Zenith ) you will be looking through one air mass of air. As you move further from your zenith you are looking diagonally through the atmosphere so you are looking through more air this increases the nearer the horizon you look until at the horizon with an altitude of zero degrees you are looking through around 40 times as much air or 40 air masses. The number of air masses is not infinite as the Earth and the Atmosphere is curved so when you look horizontally your line of site still ends up in space. There is also the effect of refraction but that just complicates matters and you should not normally be observing anywhere near the horizon.
Meteorologists however use the term Air Mass in a different way. They treat the air in the atmosphere as parcels known as Air Masses which have similar characteristics depending on where they originated and where they have traveled. For instance air from the South will have traveled over Europe and will tend to be warm, dry, contain dust and may well be polluted. If the air comes from the West at least for the UK the Air Mass will have traveled over the sea and will be cooler and contain more water. A more detailed explanation of Meteorological Air Masses can be found on the UK Meteorological Office Education page on air masses. Meteorologists also use the term visibility but this is used to define how far you can see in a horizontal direction, the air higher up may have different characteristics and this may not provide a reliable guide.
Light that travels through air is attenuated by two different mechanisms, the first is Rayleigh Scattering from air molecules. This cannot be reduced except by going higher above sea level so you reduce the amount of air molecules between you and the light source. Rayleigh scattering is what makes the sky blue and is varies as the 4th power of the wavelength of light so the blue light is scattered much more than the red light. The diagram on the left shows the amount of light scattered at different wavelengths together with an approximation of the colours ( these should be the rainbow colours but violet seems to be missing !). The loss is shown as a linear scale so needs to be converted to magnitudes for astronomical use.
The second mechanism is Rayleigh Scattering from pollution molecules, known as aerosols in the atmosphere, normally man made Nitrogen Dioxide and Sulphur Dioxide, these typically result in the Milky White sky that is so familiar to European observers. The level of pollution depends very much on where a particular Air Mass has been in it's meteorological history. Salt crystals can also cause Rayleigh scattering if there are strong winds over the ocean.
The loss of transparency due to pollution is of interest to climatologists as the scattering of light results in some of the incoming solar radiation being dissipated in the atmosphere rather than on the surface. Atmospheric scientists measure the amount of light that is lost by a factor called the 'Aerosol Optical Depth' while astronomers use a more familiar unit of magnitudes per air mass. Luckily conversion is easy just multiply the AOD value by 1.086 to convert it to magnitudes per air mass.
Sky & Telescope have two useful pages that go into the subject in more detail, the first is a page on extinction & transparency and the second a more detailed page on AOD including sources of data for North America.
There is also a descriptive page on 'Visibility and Atmospheric Aerosols on uk.sci.weather that is available here. The paragraph on 'Astronomy visibility and seeing' is a little confused as it seems to confuse visibility ( ie transparency) with seeing that is of course related to changes in refraction in the atmosphere causing the image to move or blur.
Higher levels of AOD will have more effect on low contrast objects such as nebulae but little effect on bright objects such as the Moon & planets. However it should be noted that the effect is very dependant on wavelength. Observations in the deep red such as the Hydrogen Alpha line at 658nm will be little effected but those in the Blue Green such as the Oxygen III line at 501nm and the Hydrogen Beta Line at 486nm will be much more effected.
If there is no scattering due to pollution the AOD will be zero, the article in S&T describes values of AOD of 0.2 as mediocre and 0.4 as poor but values can get a lot higher than this. The site below shows values as high as 3 !
While there are a number of sites on the Internet that provide values of AOD on a historic basis there appear to be none in Europe that provide current values either from ground stations or from satellite observations. However there is an European site that has a daily forecast of AOD which allows you to view the forecast in 3 hour time steps. While not as accurate as actual observations this is better than nothing and is not effected by cloud as are ground and satellite observations.
The Forecasts of AOD from - Monitoring Atmospheric Composition and Climate are no longer available. There is a new EU Copernicus site that now has the current forecasts of AOD and also Particulate Matter. The new site is here due to the design of the site it is not possible to provide links to the individual sub pages on Aerosol forecasts or Particulate Matter. The link above should land you on a page similar to that below:
From here you need to select Aerosol Forecasts by clicking on the image, the Particulate matter forecasts can also be useful. The Aerosol forecast leads to the Aerosol Optical Depth page as follows:
From here you can select a smaller area such as 'NW Europe' if you are in the UK. This shoulds give a page similar to the following:
You can then use the controls to alter the base time using the drop down box, the forecast time using the arrows at the bottom. Only the 550nm depth is shown and the calibration is shown below the image. The AOD for 'white areas' in the image is not shown - I assume it is less than the pale blue rather than missing data.
You can also view the individual components that make up the AOD forecast using the Aerosol Type drop down. It defaults to the combined total.
Finally the 'Filter Results' drop down allows you to look at other gasses in the atmosphere as well as fires.
Make good use if it while we are still in the EU - it is not clear if we will have access after Brexit.
While the guide above gives some indication of the results of the reduction in transparency as a result of high AOD values it is possible to calculate more precise values that take into account not only the altitude of the star or planet you intend to observe but also the wavelength that you may wish to image at.
If you have Microsoft Excel or Open Office 'Calc' on your computer you can download a spreadsheet to carry out the calculations here. Note: the calculations in this spreadsheet do not allow for the reduction in air mass for high observing sites despite this being described in the extinction & transparency reference article in S&T. The S&T article references a page from the International Comet Quarterly titled Correcting for atmospheric extinction, this page has been moved and can now be found here.
This spreadsheet is a 'tidied up' version of the original Sky & Telescope spreadsheet that can be found here, the calculations are the same but have been protected so you cannot accidently change them. One minor change is that the observing site height can now be entered in feet or meters.