Image from Google, Map of Russia and Asia |
Image from Bing Images, Orographic lifting, adiabatic heating/cooling |
From Google images, Satellite view of Ural Mountains, Demonstrates rain-shadow on leeward side as well as wispy clouds pushing through the mountains |
From Google images, A closer view of clouds pushing over the Urals in adiabatic process |
Bing images, High lenticular clouds |
Google images, Extremely high cirrus clouds |
As stable air is pushed upward, the air is cooled to the dew point (lifting condensation level) and creates precipitation on the western slopes, this can also account for high cirrus clouds and lenticular cloud formations on the eastern side of the Urals. Unstable air pushes over the mountains and settles creating precipitation within the mountains, typically snow due to the sub-polar climate.
Image from class lectures, demonstrates and explains orographic lifting and precipitation |
The eastern side (leeward) of the Urals is in a rain shadow creating a much drier arid environment. This leeward side of the Urals can be punished with extremely cold Chinook winds from adiabatic warming of the air on the down slope.
Much like North America weather patterns move primarily from West to East with colder airs approaching from the north and warmer air from the south, this creates a slightly similar effect the Rocky Mountains have on the Front Range .
http://fast.ucdenver.edu/case/1202/Climate/Weather/Weather.html
earthobservatory.nasa.gov/IOTD/view.php?id=35963
http://accessscience.com/overflow.aspx?searchStr=Mountain&stype=4&term=Mountain&topic=EARTH:PHYS&p=5
http://www.russiansabroad.com/russian_history_96.html
www.rusnet.nl/encyclo/u/urals_physic.shtml