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En-en adult card 15 radiative forcing: Difference between revisions
En-en adult card 15 radiative forcing (view source)
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|title=Radiative forcing | |title=Radiative forcing | ||
}}<ref>[https://www.ipcc.ch/site/assets/uploads/2018/02/WG1AR5_all_final.pdf#page=715 Figure 8.18, Report 5 Working Group 1]</ref> | }}<ref>[https://www.ipcc.ch/site/assets/uploads/2018/02/WG1AR5_all_final.pdf#page=715 Figure 8.18, Report 5 Working Group 1]</ref> | ||
== Correction== | |||
===Causes=== | |||
* [[En-en_adult_card_13_additional_greenhouse_effect|Additional Greenhouse Effect]] | |||
* [[En-en_adult_card_10_aerosols|Aerosols]] | |||
=== Consequences === | |||
* [[En-en_adult_card_14_energy_budget|Energy Budget]] | |||
== Explanation == | == Explanation == | ||
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== Other possible links == | == Other possible links == | ||
=== | === Other consequences === | ||
* [[En-en adult card 18 melting of sea ice|Melting of Sea Ice]] pack and [[En-en adult card 6 deforestation|Deforestation]] When sea ice melts, a white surface is replaced by a navy blue surface, which has a lower [https://simple.wikipedia.org/wiki/Albedo albedo] and therefore absorbs more energy. When the forest is cut down and replaced by a meadow, it is the opposite, a dark surface (the foliage) is replaced by a light surface (the meadow). All in all, the artificialization of the soil has a cooling effect on the climate. | * [[En-en adult card 18 melting of sea ice|Melting of Sea Ice]] pack and [[En-en adult card 6 deforestation|Deforestation]] When sea ice melts, a white surface is replaced by a navy blue surface, which has a lower [https://simple.wikipedia.org/wiki/Albedo albedo] and therefore absorbs more energy. When the forest is cut down and replaced by a meadow, it is the opposite, a dark surface (the foliage) is replaced by a light surface (the meadow). All in all, the artificialization of the soil has a cooling effect on the climate. | ||