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  2. AI winter - Wikipedia

    en.wikipedia.org/wiki/AI_winter

    In the history of artificial intelligence, an AI winter is a period of reduced funding and interest in artificial intelligence research. [1] The field has experienced several hype cycles , followed by disappointment and criticism, followed by funding cuts, followed by renewed interest years or even decades later.

  3. Extreme cold - Wikipedia

    en.wikipedia.org/wiki/Extreme_cold

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  4. Winterization - Wikipedia

    en.wikipedia.org/wiki/Winterization

    Equipment designed for use in particularly extreme cold conditions (such as the polar regions) also undergoes a "winterization" process.Many complex devices (automobiles, electronics and radios) as well as common materials (metals, rubbers, petroleum lubricants) are not designed to operate at extremely low temperatures and must be winterized to operate without severe damage from the elements ...

  5. Wintermute - Wikipedia

    en.wikipedia.org/wiki/Wintermute

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  6. Category:Winter - Wikipedia

    en.wikipedia.org/wiki/Category:Winter

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  7. Volcanic winter - Wikipedia

    en.wikipedia.org/wiki/Volcanic_winter

    The conversion of sulfur dioxide to sulfuric acid, which condenses rapidly in the stratosphere to form fine sulfate aerosols. A volcanic winter is a reduction in global temperatures caused by droplets of sulfuric acid obscuring the Sun and raising Earth's albedo (increasing the reflection of solar radiation) after a large, sulfur-rich, particularly explosive volcanic eruption.

  8. Winter City - Wikipedia

    en.wikipedia.org/wiki/Winter_City

    Livable Winter Cities, published in 1986 in Edmonton, provides a solid context and background of the city's relationship with winter. The book emphasizes the lack of literature on the design of winter cities, and attempts to provide a comprehensive resource for winter cities, at a time when it was a relatively newer topic.

  9. Nuclear winter - Wikipedia

    en.wikipedia.org/wiki/Nuclear_winter

    Nuclear winter is a severe and prolonged global climatic cooling effect that is hypothesized [1] [2] to occur after widespread firestorms following a large-scale nuclear war. [3] The hypothesis is based on the fact that such fires can inject soot into the stratosphere, where it can block some direct sunlight from reaching the surface of the Earth.