We still do not know what processes
triggered hyperthermals, the source (s) of carbon released, and their wider Earth system impacts.
Not exact matches
Starting 50 million years ago, these
hyperthermal events seem to have been
triggered every 400,000 years, and involved temperature rises of 3 F to 5 F (2 C to 3 C) that lasted up to 40,000 years.
This presentation will show evidence that the non-PETM
hyperthermals were
triggered by orbital pacing of the regular processes that readily redistribute carbon between reservoirs at Earth's surface.
The
triggering mechanism for early Cenozoic
hyperthermals, however, is poorly understood.
He has a particular interest in the relationship between volcanism and past climate change, including the possible
trigger mechanisms for the enigmatic warming events known as
hyperthermals, such as the PETM.
Her main research interest is in exploring the links between extinction, carbon emission, global warming and the
triggers of
hyperthermals.
It's not clear boreal feedbacks are even necessary to lighting off tropical biomass (fire once again), but they'll certainly speed the process way up; if that does happen in turn we're on our way to a
hyperthermal (with some lag since the oceans have to warm enough to
trigger a self - sustaining loss of shallow methane hydrates).