Except for MIS 14, the temperature anomalies (relative to the mean temperature of the last millennium) of the coldest
levels of all glacial periods range from around -9 to -9.5 °C with CO2 concentrations generally in the range 180 — 190 p.p.m.v..
Not exact matches
These may be submerged ancient shorelines cut during times
of lower sea
level, «the most recent
of which occurred during the last
glacial period, which ended about 19,000 years ago,» Chaytor said.
Glacial Isostatic Adjustment (GIA) occurs in response to retreating ice from the last glacial period, where around most of the world, land is subsiding at a fraction of a millimetre per year, compounding the problem of sea - leve
Glacial Isostatic Adjustment (GIA) occurs in response to retreating ice from the last
glacial period, where around most of the world, land is subsiding at a fraction of a millimetre per year, compounding the problem of sea - leve
glacial period, where around most
of the world, land is subsiding at a fraction
of a millimetre per year, compounding the problem
of sea -
level rise.
Glacial Isostatic Adjustment (GIA) occurs in response to retreating ice from the last glacial period, where around most of the world, land is subsiding at a fraction of a millimetre per year, compounding the problem of sea - leve
Glacial Isostatic Adjustment (GIA) occurs in response to retreating ice from the last
glacial period, where around most of the world, land is subsiding at a fraction of a millimetre per year, compounding the problem of sea - leve
glacial period, where around most
of the world, land is subsiding at a fraction
of a millimetre per year, compounding the problem
of sea -
level rise.
If the oceans had been losing energy over the same
period the troposphere was seeing the «pause» or the sea
level declining, or the net
glacial mass
of Greenland and Antarctica increasing rather than declining, then the «pause» would be confirmatory evidence that maybe the climate is not as sensitive to increasing GH gases.
I have also seen your comments on WUWT where I read about your ideas on the termination
of the
glacial periods from a low vegetation / high dust environment as a result
of low CO2
levels at the
glacial peaks, which seems very plausible to me.
[1] It began with the end
of the cold
period known as the Oldest Dryas, and ended abruptly with the onset
of the Younger Dryas, a cold
period that reduced temperatures back to near -
glacial levels within a decade.
Carbon starvation, which apparently sometimes occurs during
glacial periods due to the low
levels of CO2 that are reached, has the same effect on C3 plants * trees, shrubs, and such) as do warm, dry conditions when the warm is excesaive.
In addition to running climate models, the researchers compared modern warming to similar temperature increases that happened approximately 120,000 years ago in a
period known as the Eemian, when global sea
level was 5 to 9 meters (between 16 and 30 feet) higher than it is today due to the release
of glacial water.
During the last
glacial period, sea
level dropped 400 feet as water was tied up in ice, and as we have moved out
of the cold
glacial period, sea
level has recovered.
Yes, marked by but evidently not maintained by, as the climate invariably plunges into an extended
glacial period ahead
of any drop in CO2
levels.
As glaciers melted and retreated since the peak
of the last
glacial period about 18,000 years ago (Figure 4 - 6, p. 89), the earth's average sea
level has risen about 125 meters (410 feet).
The coming and going
of glacial periods (ice ages) largely determine the rise and fall
of sea
level.
However I have found another with a CO2
level in the range we have experienced since the 1940's http://www.pnas.org/content/99/20/12567.full At 379 ppm within 35 ppm, the start
of the Namurian
period, 330 million years ago, should be deep in an
glacial period if CO2 was the answer to the faint sun paradox.
Andre Droxler, a professor at Rice University and one
of the scientists analyzing the ancient coral, said that during the last
glacial period, sea
levels were almost 400 feet (120 meters) lower than what they are today.
Since then, atmospheric CO2 declined as the Indian and Atlantic Oceans have been major depocentres for carbonate and organic sediments while subduction
of carbonate - rich crust has been limited mainly to small regions near Indonesia and Central America [10], thus allowing CO2 to decline to
levels as low as 170 ppm during recent
glacial periods [11].