What Counts as Geologically Rapid Warming?
I frequently hear people downplay the claim that the 1.3°C warming above the 1850-1900 mean is geologically significant. I hear words like "slight" or "modest" or "insignificant" thrown around a lot. And certainly global temperatures have increased by a lot more than 1.3°C on geologic time scales. My first response is typically to point out that on geologic time scales, global temperatures do change a lot, but at much slower rates. Current warming rates are exceptional, even on geologic time scales. And I think this point can be relatively easily demonstrated with the evidence we have, even taking into consideration the fact that proxies do not preserve a high degree of temporal resolution, and actual warming rates may exceed what we can detect with proxy evidence. I think we need a two part response to this.
Defining Geologically "Rapid" Warming
Since terms like "rapid" are relative terms, I think we need to come up with a standard for what should count as "rapid" on geologic time scales. I think most everyone agrees that warming rates coming out of glacial maxima count as rapid, so I propose we use that as a definition of what counts as rapid. That is, at the very least, if global temperatures warm more rapidly than deglaciation warming rates, it's safe to say that warming rate counts as rapid. So we need a metric for warming rates of global temperatures coming out of glacial maxima. For this I'm going to use Friedrich et al 2016.[1]
- Locally, sudden climate changes can and do happen that can produce much more rapid warming. But these events typically involve a sudden redistribution of heat around the globe, and rapid warming in one area is compensated by cooling in another. An example of this would be the Younger Dryas event, where local Greenland temperatures suddenly cooled by perhaps as much as 10°C on decadal time scales, but Antarctica warmed, and the global mean temperature change wasn't nearly that rapid.
- Global temperatures fluctuate by much more than 0.01°C annually; annual variability can range by 0.25°C or more. But here we aren't interested in annual variability; even when stationarity can be assumed internal variability happens. We're interested in sustained changes in global temperatures on decadal time scales or longer.
How Exceptional is Recent Warming?
Taking into account timespan-dependent scaling, warming rates through intervals such as the Permian–Triassic boundary and the PETM likely exceeded current rates on decadal timescales, at least intermittently. Warming across the Permian–Triassic boundary stands out as the most significant temperature change of the past ∼0.5 billion years.In other words, there are just a few events in geologic history where warming happened rapidly enough that, on decadal time scales undetectable by proxy evidence, warming occurred more rapidly than current warming. So it's true that proxy evidence can't preserve evidence of the maximum rates of climate change, and we can infer that warming on decadal time scales occurred more rapidly than proxies detect. However, the two candidates that likely exceeded current warming are found in exceedingly extreme events like the end-Permian extinction and PETM, which were associated with mass extinctions of nearly all life (end-Permian) and benthic foraminifera (PETM). So if current warming rates are not geologically unprecedented (yet), current warming is still exceptionally rapid geologically peaking and ranks among the most rapid warming events in the last half billion years, events also associated with mass extinctions. We also know that the warming during both of these extinction events were linked to long-term increases in GHG concentrations from persistent eruptions of large igneous provinces, which is not currently occurring. So we can rule out the possibility that recent warming has the same natural cause as the end Permian warming or the PETM. The cause of recent warming is due to human emissions of greenhouse gases.
https://www.researchgate.net/publication/309791338_Nonlinear_climate_sensitivity_and_its_implications_for_future_greenhouse_warming
[2] Kemp, D., Eichenseer, K. & Kiessling, W. Maximum rates of climate change are systematically underestimated in the geological record. Nat Commun 6, 8890 (2015). https://doi.org/10.1038/ncomms9890
[3] Geological Society of London. "What the Geological Record Tells Us About Our Present and Future Climate." Journal of the Geological Society, vol. 178, no. 1, 2021, https://doi.org/10.1144/jgs2020-239. https://www.lyellcollection.org/doi/pdf/10.1144/jgs2020-239
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