It is very well known that the sky scattering of visible light decrease with the wavelength, it is bigger in the blue portion of the spectrum( the reason why the sky is blue ) and is lower on the red portion of the spectrum, this scattering is even lower on the infrared section and lower still in the short radio wave section of the spectrum. A less known effect of this scattering is its masking effect on small objects that are on the atmosphere, we know that in daylight this effect hides the stars and many other astronomical objects, but also that effect mask/hides small objects that are in the atmosphere, as high altitude birds, bugs, balloons, etc. This masking effect is very easy to test by making atmospheric observations with binoculars and then doing the same observations placing red filters in front of the binoculars, by doing that many more details will be spotted just by placing red filters in front of the binoculars. So you can say that the spotting efficiency of binoculars increase by just placing red filters in front of them. The effect is even more dramatic when moving to the infrared, you can spot easily Mars in daylight using a camera enabled to receive infrared and using a 950nm IR pass filter. Moving then to the short radio wave section will allow you to spot many more objects that are masked by the sky scattering of visible light, because simply the scattering is lower in short radio waves. These simple ideas lead to the design of very effective instruments for optical atmospheric observations. Anybody that wants to make optical atmospheric observations should take in count the masking effect mentioned above. Then we have three options listed in order of effectiveness to make optical atmospheric observations: 1- Scan the sky using short radio waves, a radar and then aligned/centered with this radar place a telescope or high optical magnification scope, with this configuration any object spotted by the radar will be optically visible in the telescope section. 2- Scan the sky using a modified camera IR enabled, using a 950nm or 1000nm IR pass filter, then also aligned/centered with the field of view(FOV) of this camera place a telescope or high optical magnification scope, with this configuration any object spotted by the infrared camera and centered in its FOV will be optically visible in the telescope. Even when this option is less effective than using radars it is very effective spotting small objects in the sky, for example Mars will be easily spotted in daylight using such a setup, many "local" objects will be spotted too. 3- Scan the sky using a scope with red filters. This is an example of how very simple ideas from elementary physics actually drive the design of very effective instruments. The systematic use of the instruments listed in options 1 and 2, mainly option 2 in atmospheric observations actually are helping in the discovery and study of new atmospheric characteristics.