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Only small portions of the Rus countries are south of the 50th. parallel & more than half of the Rus countries are north of 60th. parallel. Vast regions experience 6+ months of snow cover over a subsoil that is permafrost as deep as 300-400 meters. The average yearly temperature of nearly all of European Russia is below freezing. The average for most of Siberia is also below freezing as well. Most of Russia only has two seasons, Summer & Winter. There only very short intervals of distinction between them.
The Winter intense high-pressure systems cause winds to blow from the S & SW in all but the Pacific Region Siberian Kamchatka also called the Primorskoye Region. In the Summer low-pressure systems cause the prevailing winds to come out of the N & NW to most of the Rus landmass. It is this meteorological phenomenon that produces the Wintertime temperature variances between N & S. This may seen by the average January temperatures of -8̊ to -12̊C in St. Petersburg & Moscow, -25 to -35̊C on the Siberian Plain, and -40 to -55̊C at Yakutsk located in east-central Siberia at approximately the same latitude as St. Petersburg. The Winter average temperature on the Mongolian border at a latitude is some 10̊ farther South is no warmer. The Summer temperatures are more affected by latitude. The Arctic islands average 4̊ to 8̊C while the most Southern regions average 20̊ to 27̊ C. The Rus's potential for vast extremes is seen by the national record low of -94̊C, recorded at Verkhoyansk in north-central Siberia & a record high of 38̊C, recorded at several Southern locations along the Black Sea coast.
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