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  2. Retreat of glaciers since 1850 - Wikipedia

    en.wikipedia.org/wiki/Retreat_of_glaciers_since_1850

    The glacier retreated 1.9 kilometres (1.2 mi) in 33 years. The retreat of glaciers since 1850 is well documented and is one of the effects of climate change. The retreat of mountain glaciers provide evidence for the rise in global temperatures since the late 19th century. Examples include mountain glaciers in western North America, Asia, the ...

  3. Climate change - Wikipedia

    en.wikipedia.org/wiki/Climate_change

    The World Meteorological Organization estimates a 66% chance of global temperatures exceeding 1.5 °C warming from the preindustrial baseline for at least one year between 2023 and 2027. [ 94 ] [ 95 ] Because the IPCC uses a 20-year average to define global temperature changes, a single year exceeding 1.5 °C does not break the limit.

  4. Climate change in the Arctic - Wikipedia

    en.wikipedia.org/wiki/Climate_change_in_the_Arctic

    Due to climate change in the Arctic, this polar region is expected to become "profoundly different" by 2050. [1]: 2321 The speed of change is "among the highest in the world", [1]: 2321 with the rate of warming being 3-4 times faster than the global average. [2][3][4][5] This warming has already resulted in the profound Arctic sea ice decline ...

  5. Glacier - Wikipedia

    en.wikipedia.org/wiki/Glacier

    Glacier. Glacier of the Geikie Plateau in Greenland. The Taschachferner in the Ötztal Alps in Austria. The mountain to the left is the Wildspitze (3.768 m), second highest in Austria. With 7,253 known glaciers, Pakistan contains more glacial ice than any other country on earth outside the polar regions. [1]

  6. Post-glacial rebound - Wikipedia

    en.wikipedia.org/wiki/Post-glacial_rebound

    Post-glacial rebound (also called isostatic rebound or crustal rebound) is the rise of land masses after the removal of the huge weight of ice sheets during the last glacial period, which had caused isostatic depression. Post-glacial rebound and isostatic depression are phases of glacial isostasy (glacial isostatic adjustment, glacioisostasy ...

  7. Tipping points in the climate system - Wikipedia

    en.wikipedia.org/wiki/Tipping_points_in_the...

    Altogether, it was estimated in 2023 that 49% of the world's glaciers would be lost by 2100 at 1.5 °C (2.7 °F) of global warming, and 83% of glaciers would be lost at 4 °C (7.2 °F). This would amount to one quarter and nearly half of mountain glacier *mass* loss, respectively, as only the largest, most resilient glaciers would survive the ...

  8. Climate change in Europe - Wikipedia

    en.wikipedia.org/wiki/Climate_change_in_Europe

    Increase of average yearly temperature (2000-2017) above the 20th century average in selected cities in Europe [ 1 ] Climate change has resulted in an increase in temperature of 2.3 °C (4.14 °F) (2022) in Europe compared to pre-industrial levels. Europe is the fastest warming continent in the world. [ 2 ] Europe's climate is getting warmer ...

  9. Climate change in Asia - Wikipedia

    en.wikipedia.org/wiki/Climate_change_in_Asia

    Climate change in Asia. The 2022 South Asian floods, including in Pakistan (pictured) are an example of a climate change impact. [1][2] Climate change occurs all over the world, and it is particularly important in Asia, as it accounts for the majority of the human population. Warming since the 20th century is increasing the threat of heatwaves ...