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Linear and Nonlinear Aspects of Climate Response to External Forcings
The main role in the current climate change is played by anthropogenic forcings, primarily anthropogenic emissions of greenhouse gases and aerosols. On the global scale, the response of the Earth system to these forcings is close to linear. In particular, it depends mostly on the magnitude of such f...
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Published in: | Radiophysics and quantum electronics 2023-07, Vol.66 (2-3), p.79-92 |
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description | The main role in the current climate change is played by anthropogenic forcings, primarily anthropogenic emissions of greenhouse gases and aerosols. On the global scale, the response of the Earth system to these forcings is close to linear. In particular, it depends mostly on the magnitude of such forcings and only weakly on their nature and spatial localization. However, even with relatively small (in absolute value) external forcings, the response of the characteristics of the Earth system can be essentially nonlinear with the manifestation of tipping points, upon transition through which the behavior of the Earth’s climate changes qualitatively. Examples are given for linear and nonlinear mechanisms of the climate response to external forcings. |
doi_str_mv | 10.1007/s11141-023-10277-5 |
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subjects | Air pollution Astronomy Astrophysics and Astroparticles Climate change Earth Global temperature changes Greenhouse gases Hadrons Heavy Ions Lasers Mathematical and Computational Physics Nuclear Physics Observations and Techniques Optical Devices Optics Photonics Physics Physics and Astronomy Quantum Optics Theoretical |
title | Linear and Nonlinear Aspects of Climate Response to External Forcings |
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