How fast to turn around: preventing tipping after a system has crossed a climate tipping threshold
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<p>A classical scenario for tipping is that a dynamical system experiences a slow parameter drift across a fold tipping point, caused by a run-away positive<br>feedback loop. We study what happens if one turns around after one has crossed the threshold. We derive a simple criterion that relates how far the parameter exceeds the tipping threshold maximally and how long the parameter stays above the threshold to avoid tipping in an inverse-square law to observable properties of the dynamical system near the fold. We demonstrate the inverse-square law relationship using simple models of recognised potential future tipping points in the climate system.&#160;</p>
2019 ◽
Vol 475
(2222)
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pp. 20180504
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2012 ◽
Vol 8
(5)
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pp. 4269-4294
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2019 ◽
Vol 16
(158)
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pp. 20190345
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2017 ◽
Vol 04
(01)
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pp. 1750004
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2012 ◽
Vol 2012
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pp. 1-15
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