This is because warmer
conditions during interglacials encouraged the collapse of ice shelves.
Not exact matches
Instead, the fossil record indicates they vanished
during the Earth's glacial -
interglacial transition, which occurred about 12,000 years ago and led to much warmer
conditions and the start of the current Holocene period.
The sequence of climatic forcings and responses
during deglaciations (transitions from full glacial
conditions to warm
interglacials) are well documented.
The current secondary contact is thought to result from a range expansion associated with the amelioration of climatic
conditions after the last glacial maximum (∼ 18000 ya)[20], although previous glacial /
interglacial cycles
during the Pleistocene may have provided multiple opportunities for vicariant and past hybridization events.
In any event, there is unequivocal geologic evidence for parts of the GIS still in tact
during the last
interglacial, and Northern Hemisphere ice core records (see NEEM) now go back that far, which rules out ice - free
conditions at the time in the NH.
That is all I meant except to point out that
conditions during the Eemian
interglacial in East Africa were not conducive to human habitation; many groups left for more hospitable locations.
[Response: If this reservoir existed and was so poised to release methane as you speculate, then it would have done something
during warmer
conditions early in the Holocene, or in the last
interglacial.
You said: «If this reservoir existed and was so poised to release methane as you speculate, then it would have done something
during warmer
conditions early in the Holocene, or in the last
interglacial.
It is also clear that
conditions during the last
interglacial (LIG, 125 kya BP) that temperature changes were close to what is anticipated by the end of the century.
During subsequent
interglacials, when humid
conditions returned to the tropics, the forests expanded and were repopulated by plants and animals from the species - rich refuges.»
However, a major sudden cold event did probably occur under global climate
conditions similar to those of the present,
during the Eemian
interglacial, around 122,000 years ago.
Müller, C. Reconstruction of the paleontological
conditions at the Laptev Sea continental margin
during the last two glacial /
interglacial cycles based on sedimentological and mineralogical investigations.
Matthiessen, J. & Knies, J. Dinoflagellate cyst evidence for warm
interglacial conditions at the northern Barents Sea margin
during marine oxygen isotope stage 5.
This type of behavior is especially evident
during transitions from glacial to
interglacial conditions, when climate is affected by a wide variety of time - varying influences and is relatively unstable.
but this occurred under significantly different orbital forcing
conditions» This is to make us believe that a global mean temperature could drive the melting or calving of the Greenland; but the Eemian diminution of the Greenland ice cap is by no means related to an average global temperature but to the local summer insolation that
during the last
interglacial was up to 30 W / m ² to 60 W / m ² stronger than today's.
each period of warming
during the descent to the next glacial stage should be more intense than the previous ones, as climatic variability increases outside the warm
conditions of an
interglacial climatic optimum.
Other processes must be responsible for the 40 - to 50 - ppm pCO2 drawdown
during the initial transition from
interglacial to glacial
conditions as well as for a comparable pCO2 increase
during the latter part of glacial terminatins.
In the first post, we described the
conditions that exisited
during the Last
Interglacial.
Climate change models predict that the Middle East will get warmer and drier, similar to the
conditions during the last
interglacial period when the Dead Sea dried up.