The beginning and
end of a glacial period are clearly times of global climate change, but there are also periods of abrupt change in climate patterns within those periods.
At
the end of the glacial periods, CO2 increases about 80 ppm over ~ 10,000 years.
The «stuff on the bottom» of a coal seam is the tail
end of a glacial period, she said.
I've understood that he also predicted the ~ 1000 year time lag between temperature rise and CO2 at
the end of a glacial period, before it was observed in the ice cores thanks to better dating techniques.
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.
A prehistoric human skeleton found on the Yucatán Peninsula is at least 13,000 years old and most likely dates from a
glacial period at the
end of the most recent ice age, the late Pleistocene.
Understanding the complex interplay between climate and biotic interactions is thus essential for fully anticipating how ecosystems will respond to the fast rates
of current warming, which are unprecedented since the
end of the last
glacial period.
However, some species
of animals survived the
end of the last
glacial period somewhat longer than others.
They compared the carbon - 13 and nitrogen - 15 values in the giant deer bones from the Swabian Alb caves with those
of red deer, other giant deer and reindeer, which were living at the beginning and the
end of the last
glacial period.
Woolly mammoths disappeared from Siberia and North America about 10,000 years ago, along with other giant mammals that went extinct at the
end of the last
glacial period.
«Conversely, there is more and better evidence across Iceland that when the ice sheet underwent major reduction at the
end of the last
glacial period, there was a large increase in both the frequency and volume
of basalt erupted — with some estimates being 30 times higher than the present day.
However, it's quite a different matter melting a long - lived massive ice sheet up to 1.5 km thick that covers over 70 %
of the land surface (as happened at the
end of the last
glacial period), from melting isolated and much thinner ice caps / sheets that only cover about 11 %
of the land surface (i.e. present - day).»
Just 200 years before the young girls» short lifetimes, the last
glacial period of the Pleistocene Epoch (2.6 million — 11,700 years ago)
ended.
It is very unlikely that the Milankovitch cycles can start or
end an ice age (series
of glacial periods):
The history
of Scotland is known to have begun by the
end of the last
glacial period (in the paleolithic), roughly 10,000 years ago.
Interesting study out on the outgassing
of CO2 from the northern Pacific to
end the last
glacial period:
It is therefore estimated that about 500 billion tons
of carbon were emitted into the atmosphere at the
end of the last
glacial period.
In the mid-latitudes and the tropics, the
end of the last
glacial period was marked by a tremendous increase in rainfall.
[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.
During the Earth's ice ages the Pacific Ocean stored large amounts
of carbon, which for some reason it released again close to the last
glacial period's
end, warming the world and melting most
of the icecaps.
Few people have read paleo - climatology text books, are aware
of the
glacial / interglacial cycle, are aware that the paleoclimatic record has unequivocal evidence
of cyclic gradual changes and cyclic abrupt climate events, are aware that the abrupt climate change events such as the abrupt termination
of the last 22 interglacial
periods lacks an explanation, are aware that all
of the past interglacial
periods are short (roughly 12,000 years) and that they have
ended abruptly, and so on.
Kent points out that according to the Milankovitch theory, we should be at the peak
of a 20,000 - some year warming trend that
ended the last
glacial period; the Earth may eventually start cooling again over thousands
of years, and possibly head for another glaciation.
Suess reported that the last
glacial period had
ended with a «relatively rapid» rise
of temperature — about 1C (roughly 2F) per thousand years.
A new study documents evidence
of a massive release
of carbon from permafrost as temperatures rose at the
end of the last
glacial period.
In addition, the rate
of warming over the 21st century is projected to be far faster than has occurred over such
periods since the
end of the last
glacial period, again long before societal development.
A new study is shedding light on what that could mean for the future by providing the first direct physical evidence
of a massive release
of carbon from permafrost during a warming spike at the
end of the last
glacial period.
Rhetorically speaking, was
glacial melt and SLR from warming «equally measured» in 150 year increments from 20k years ago at the
end of the LIA to 10k years ago when the last glacier receded from New York; or did the velocity
of SLR increase over this
period as factors, like the before mentioned, accelerated the velocity
of melt through the
period?
For the last three thousand years, Since 1000 BC, the
end of the Minoan Warm
Period, the global temperature trend has been -0.5 to -0.7 dgC per 1000 yrs, projecting full
glacial of 8 dgC in another 7,000 yrs.
1998 was near the tail
end of a decade that jumped well above the mean average longer term rate
of increase (there is a thing called climate variability, it didn't disappear with climate change, and if anything probably only intensified;, and ocean warming and
glacial melt both accelerated during this
period, taking more energy out
of the air — see below).
------- * Not to mention that there is an event similar to the Younger Dryas at the
end of at least one other
glacial period, «termination III» (see e.g. Carlson et al., 2008).
The problem was the Pleistocene extinction, the disappearance
of most species
of large mammals across most
of the world at the
end of the last
glacial period some 12,000 years ago.