Temperateness
Temperateness is a term used in climatology to describe a climate which is neither extremely hot nor extremely cold. It is often associated with the Köppen climate classification system, where it is used to describe climates that fall into the C (temperate) category.
Temperate climates are typically found in the middle latitudes, between the tropics and the polar regions. They are characterized by moderate temperatures, with a relatively small range between the hottest and coldest months. Precipitation is often evenly distributed throughout the year, although some temperate climates may have a distinct wet and dry season.
Characteristics[edit | edit source]
Temperate climates are characterized by four distinct seasons: spring, summer, autumn, and winter. The length and severity of these seasons can vary depending on the specific location.
In general, summers in temperate climates are warm to hot, with temperatures typically ranging from 20 to 30 degrees Celsius. Winters are cool to cold, with temperatures often falling below freezing.
Precipitation in temperate climates is often evenly distributed throughout the year, although some regions may have a distinct wet and dry season. The average annual precipitation in temperate climates typically ranges from 500 to 1,500 millimeters.
Types of Temperate Climates[edit | edit source]
The Köppen climate classification system recognizes several subtypes of temperate climates, including:
- Mediterranean climate (Csa, Csb): Characterized by hot, dry summers and mild, wet winters.
- Humid subtropical climate (Cfa, Cwa): Characterized by hot, humid summers and mild to cool winters.
- Oceanic climate (Cfb, Cfc): Characterized by mild summers and cool winters, with precipitation evenly distributed throughout the year.
- Subtropical highland climate (Cwb, Cwc): Characterized by mild summers and cool winters, with a distinct wet season.
See Also[edit | edit source]
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