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  2. Desert climate - Wikipedia

    en.wikipedia.org/wiki/Desert_climate

    The desert climate or arid climate (in the Köppen climate classification BWh and BWk) is a dry climate sub-type in which there is a severe excess of evaporation over precipitation. The typically bald, rocky, or sandy surfaces in desert climates are dry and hold little moisture, quickly evaporating the already little rainfall they receive.

  3. Köppen climate classification - Wikipedia

    en.wikipedia.org/wiki/Köppen_climate_classification

    If the annual precipitation is less than 50% of this threshold, the classification is BW (arid: desert climate); if it is in the range of 50%–100% of the threshold, the classification is BS (semi-arid: steppe climate). [9] [11] A third letter can be included to indicate temperature.

  4. Climate classification - Wikipedia

    en.wikipedia.org/wiki/Climate_classification

    Climate classifications are systems that categorize the world's climates. A climate classification may correlate closely with a biome classification, as climate is a major influence on life in a region. The most used is the Köppen climate classification scheme first developed in 1884. [1] [2]

  5. Geographical zone - Wikipedia

    en.wikipedia.org/wiki/Geographical_zone

    Today, the most commonly used climate map is the Köppen climate classification, developed by Russian climatologist of German descent and amateur botanist Wladimir Köppen (1846–1940), which divides the world into five major climate regions, based on average annual precipitation, average monthly precipitation, and average monthly temperature.

  6. Desert - Wikipedia

    en.wikipedia.org/wiki/Desert

    A semi-arid desert or a steppe is a version of the arid desert with much more rainfall, vegetation and higher humidity. These regions feature a semi-arid climate and are less extreme than regular deserts. [34] Like arid deserts, temperatures can vary greatly in semi deserts.

  7. Climatic geomorphology - Wikipedia

    en.wikipedia.org/wiki/Climatic_geomorphology

    Atolls like Atafu in Tokelau in the Pacific Ocean are landforms associated to tropical climate. No atoll exists outside the tropics. Climatic geomorphology is the study of the role of climate in shaping landforms and the earth-surface processes. [1] An approach used in climatic geomorphology is to study relict landforms to infer ancient ...

  8. Aridity - Wikipedia

    en.wikipedia.org/wiki/Aridity

    The latter does change significantly over time through climate change. For example, temperature increase by 1.5–2.1 percent across the Nile Basin over the next 30–40 years could change the region from semi-arid to arid, significantly reducing the land usable for agriculture. In addition, changes in land use can increase demands on soil ...

  9. List of deserts by area - Wikipedia

    en.wikipedia.org/wiki/List_of_deserts_by_area

    This is a list of the largest deserts in the world by area. It includes all deserts above 50,000 km 2 (19,300 sq mi). ... 6: Gobi Desert: Cold winter: 1,295,000 [1]

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