The Temperate climate zone is normally divided into two types:
1)Temperate Continental climates (which include arid climates within the Temperate zone), are normally located between 35 or 40 and 55 north latitude on the eastern side or interior of the large landmasses in Asia, Europe, and North America (no Temperate Continental climates occur in the southern Hemisphere). In this climate zone, summers are warm (to hot in some areas), and winters often long, cold, and snowy (in the more humid sectors). 
2)Temperate Oceanic Climates are normally located between 45 and 58 north latitude on the west sides or west coastal areas of the large landmasses in Asia, Europe, North America, extreme South America, and South Island, New Zealand. In this climate zone, summers are cool, and winters are cool, but not cold, and there is little frozen precipitation at lower elevations. Located in the higher latitudes on the windward sides of landmass, some oceanic climates can have much cloudy and overcast skies.
The vast majority of the world's human population resides in temperate zones, especially in the northern hemisphere because of its greater mass of land.
^"Climate of Switzerland". Swiss University. Retrieved October 4, 2012. The Alps act as a climate barrier: Southern Switzerland, which is mainly influenced by the Mediterranean Sea, is characterized by a much milder climate than Northern Switzerland.
^Brinch, Brian (2007-11-01). "How mountains influence rainfall patterns". USA Today (Tysons Corner, Virginia: Gannett). ISSN0734-7456. Retrieved October 4, 2012. As air ascends mountains, such as the Washington Cascades, it is forced to rise. The rising air cools, condenses, and drops rain on locations situated on the windward slopes, like Seattle. When the air descends the back side of the mountain toward Spokane, it is compressed, warming and drying it out. This sinking, dry air produces a rain shadow, or area in the lee of a mountain with less rain and cloudcover.