Everything about Temperate totally explained
In
geography,
temperate latitudes of the globe lie between the
tropics and the
polar circles. The changes in these regions between summer and winter are generally mild, rather than extreme hot or cold. However, a temperate climate can have very unpredictable weather. In regions traditionally considered tropical, localities at high altitudes (for example parts of the
Andes) may have a temperate climate.
The
north temperate zone extends from the
Tropic of Cancer (at about 23.5 degrees north latitude) to the
Arctic Circle (at approximately 66.6 degrees north latitude). The
south temperate zone extends from the
Tropic of Capricorn (at approximately 23.5 degrees south latitude,) to the
Antarctic Circle (at approximately 66.5 degrees south latitude.)
Within these borders there are many climate types, which are generally grouped into two categories:
maritime and
continental.
The maritime climate is affected by the oceans, which help to sustain somewhat stable temperatures throughout the year. In temperate zones the prevailing winds are from the west, thus the western edge of temperate continents most commonly experience this maritime climate. Such regions include
Western Europe, and western
North America at latitudes between 40° and 60° north (65°N in Europe).
The continental climate is usually situated inland, with warmer summers and colder winters. Heat loss and reception are aided by extensive land mass. In
North America, the
Rocky Mountains act as a climate barrier to the maritime air blowing from the west, creating a continental climate to the east. In Europe, the maritime climate is able to stabilize inland temperature, because the major mountain range - the
Alps - is oriented east-west (the area east of the long
Scandinavian mountain range is an exception).
The majority of the world's human population resides in temperate zones, especially in the northern hemisphere because of the mass of land.
For the history of the term, see geographical zone
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