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  2. Desert greening - Wikipedia

    en.wikipedia.org/wiki/Desert_greening

    Deserts span all seven continents of the Earth [1] and make up nearly a fifth of the Earth's landmass, [2] areas that recently have been increasing in size. [3] As some of the deserts expand [4] and global temperatures increase, [5] the different methods of desert greening may provide a possible response. [6]

  3. Desert ecology - Wikipedia

    en.wikipedia.org/wiki/Desert_ecology

    Semiarid deserts experience similar conditions to hot deserts, however, the maximum and minimum temperatures tend to be less extreme, and generally range from 10 to 38 °C. Coastal deserts are cooler than hot and semiarid deserts, with average summer temperatures ranging between 13 and 24 °C.

  4. Desert climate - Wikipedia

    en.wikipedia.org/wiki/Desert_climate

    The world's absolute heat records, over 50 °C (122 °F), are generally in the hot deserts, where the heat potential can be the highest on the planet. This includes the record of 56.7 °C (134.1 °F) in Death Valley , which is currently considered the highest temperature recorded on Earth . [ 4 ]

  5. The world is on track for a “catastrophic” 3.1 degrees Celsius (5.6 degrees Fahrenheit) of global warming over preindustrial levels, according to the United Nations.. The international ...

  6. 2 Degrees Will Change The World - The Huffington Post

    data.huffingtonpost.com/2015/11/two-degrees-will...

    The green, orange and yellow lines indicate how surface temperatures will likely respond if leading carbon emitters begin to reduce reliance on fossil fuels. Without immediate curbs, temperatures are set to follow the red track, and increase between 3.2 and 5.4 degrees Celsius by 2100. The green line shows how we can minimize warming if ...

  7. Desert - Wikipedia

    en.wikipedia.org/wiki/Desert

    Like arid deserts, temperatures can vary greatly in semi deserts. They share some characteristics of a true desert and are usually located at the edge of deserts and continental dry areas. They usually receive precipitation from 250 to 500 mm (9.8 to 19.7 in) but this can vary due to evapotranspiration and soil nutrition.

  8. Land surface effects on climate - Wikipedia

    en.wikipedia.org/wiki/Land_surface_effects_on...

    As a consequence of the different adiabatic lapse rates of moist and dry air, the air on the leeward slopes becomes warmer than equivalent elevations on the windward slopes. Föhn winds can raise temperatures by as much as 14 °C (25 °F) [ 20 ] in just a matter of minutes.

  9. Deserts and xeric shrublands - Wikipedia

    en.wikipedia.org/wiki/Deserts_and_xeric_shrublands

    Many deserts, such as the Sahara, are hot year-round, but others, such as East Asia's Gobi Desert, become quite cold during the winter. [1] Temperature extremes are a characteristic of most deserts. High daytime temperatures give way to cold nights because there is no insulation provided by humidity and cloud cover. The diversity of climatic ...