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For Ridgwell, it's a better analog for the future: This is why I like the PETM, at least it's a warming event.
It is believed that a sudden increase in the concentration of methane in the atmosphere was responsible for a warming event that raised average global temperatures by 4 8 °C (7.2 14.4 °F) over a few thousand years during the so-called Paleocene-Eocene Thermal Maximum, or PETM.
And the answer every time appears to be, if you do this, if you keep on doing what we're doing now, we will repeat, in all essential details, the past warming event — at which stage geologists can take a really lofty view – which unless you've got grandchildren you tend to do – and you say, well, we don't care.
The Middle Eocene Climatic Optimum (MECO) was a warming event that interrupted the long-term Eocene cooling trend.
The warming event of the three protocols was monitored during slow warming of the samples in air at room temperature.
A smaller prototype device was in place during the 1998 warming event and more than 80% of its corals survived, compared to just 2% elsewhere on the reef.
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In the case of weaker warming events with 1 1.5 SDs, the warming-blocking relationship also holds with three exceptions 23 July 2003, 7 8 July 2011, and 13 15 July 2011.
Ridgwell has also investigated global warming events going back deeper in geological time, including the big mass extinction events like the end-Permian and the end-Triassic, as well as so-called "Ocean Anoxic Events" in the Cretaceous.
Yes, global warming events have occurred naturally in the past, and sea level rose as a consequence, but that doesn't tell us anything about the causes of the current global warming.
Large negative zonal winds were observed during stratospheric sudden warming events.
The 2009 SSW has been one of the strongest warming events that has been recorded.
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CEO of Professional Science Editing for Scientists @ prosciediting.com