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Covering 14.2% of Earth's land area, hot deserts are the second most common type of climate on Earth after the polar climate. There are two variations of a desert climate according to the Köppen climate classification: a hot desert climate (BWh), and a cold desert climate (BWk).
- Semi-arid climate
A semi-arid climate, semi-desert climate, or steppe climate...
- Desert
In hot deserts, the temperature during daytime can exceed 45...
- Semi-arid climate
Das BWh-Klima – Heißes Wüstenklima, von Köppen auch „Saharaklima“ genannt, englisch ebenso Hot desert climate – grenzt die Klimate der heißen Wüsten ein. h = Ganzjährig heiß; die Jahresmitteltemperatur liegt über 18 °C. Beispiele. Phoenix, Arizona, USA; Lima, Peru; Águilas, Spanien
There are three types of desert climates in the Köppen climate classification: a hot desert climate (BWh), a cold desert climate (BWk) and a mild desert climate (BWh/BWn). Hot deserts have very hot summers that have temperatures that can even reach 45 °C (113 °F).
effect on. These are the hot desert, semiarid, tropical wet-and-dry, equatorial (tropical wet), Mediterranean, humid subtropical marine, warm temperate upland, and mountain regions. …larger and more prominent in arid and semiarid regions, however, and generally are regarded as characteristic desert landforms.
Desert climate (in the Köppen climate classification BWh and BWk, sometimes also BWn), also known as an arid climate, is a climate that does not meet the criteria to be classified as a polar climate, and in which precipitation is too low to sustain any vegetation at all, or at most a very scanty shrub.
