Climate sensitivity: Difference between revisions
From Climate State Wiki
mNo edit summary |
mNo edit summary |
||
Line 4: | Line 4: | ||
==References== | ==References== | ||
{{Reflist|2}} | {{Reflist|2}} | ||
[[Category:Climate change]] | [[Category:Climate change]] | ||
[[Category:Climate change feedbacks]] |
Revision as of 10:07, 6 May 2023
Climate sensitivity is a measure of how much Earth's surface will cool or warm after a specified factor causes a change in its climate system, such as how much it will warm for a doubling in the atmospheric carbon dioxide (CO2) concentration.[1] In technical terms, climate sensitivity is the average change in global mean surface temperature in response to a radiative forcing, which drives a difference between Earth's incoming and outgoing energy.[2] Climate sensitivity is a key measure in climate science,[3] and a focus area for climate scientists, who want to understand the ultimate consequences of anthropogenic global warming.
References
- ↑ What is ‘climate sensitivity’? MetOffice
- ↑ PALAEOSENS Project Members (2012) Making sense of palaeoclimate sensitivity - DOINature
- ↑ Alan Buis (2020) Making Sense of ‘Climate Sensitivity' NASA