But an ice core collected in nearby Greenland suggests that the planet experienced continuous cold from 40,000 to about 115,000 years ago, when the
last warm interglacial period ended, Miller said.
The sediment cores used in this study cover a period when the planet went through many climate cycles driven by variations in Earth's orbit, from extreme glacial periods such as the Last Glacial Maximum about 20,000 years ago, when massive ice sheets covered the northern parts of Europe and North America, to
relatively warm interglacial periods with climates more like today's.
Many of the glaciers that jut out into the ocean are thinning, but whether the ice sheet itself has remained stable and intact, even
during warm interglacial periods, is a matter of considerable debate.
«We have analyzed the transition from the last glacial period until our
present warm interglacial period, and the climate shifts are happening suddenly, as if someone had pushed a button,» said Dahl - Jenson.
Researchers from the Niels Bohr Institute have analysed the natural climate variations over the last 12,000 years, during which we have had
a warm interglacial period and they have looked back 5 million years to see the major features of the Earth's climate.
The climate during
the warm interglacial periods is more stable than the climate of ice age climate.
For example, the polar bear specimen from roughly 120,000 years ago survived in Svalbard during
a warm interglacial period because that Arctic archipelago remained more frozen than other areas.
Previous estimates suggested that peak temperatures during
the warmest interglacial periods — which occurred at around 125,000, 240,000 and 340,000 years ago — were about three degrees higher than they are today.
Ice sheet models can be run through many glacial cycles (i.e. cold glacial periods and
warm interglacial periods).
Historically, methane concentrations in the world's atmosphere have ranged between 300 and 400 nmol / mol during glacial periods commonly known as ice ages, and between 600 to 700 nmol / mol during
the warm interglacial periods.
They also found that there were long periods when the speleothems didn't grow at all — certainly not during ice ages, when permafrost locked the soil across most of Siberia, but not even, in the northernmost caves, during
warmer interglacial periods, like the one we're in now when glaciers went into retreat.
Substantial and correlated changes in marine carbonate (CaCO3) content of oceanic sediments commonly accompany the transitions from cold glacial periods to
warm interglacial periods.
Over that time, the globally averaged temperature difference between the depth of an ice age and
a warm interglacial period was 4 to 6 °C — comparable to that predicted for the coming century due to anthropogenic global warming under the fossil - fuel - intensive, business - as - usual scenario.
For the past million years, atmospheric CO2 has ranged from around 280 ppm during
warm interglacial periods to as low as 180 ppm during cold ice ages.
If we look to roughly 325,000 years ago, based on the Vostok data above, we see that Earth was at the peak of
a warm interglacial period.
Then during
each warm interglacial period, when both land and marine productivity increased, pH fell to ~ 8.1 (Honisch 2005).
No doubt the present
warm interglacial period would end eventually, but that might be thousands of years away.
But
warm interglacial periods had certainly been subject to big swings of temperature lasting for centuries.
With the onset of
the warmer interglacial period CO2 rebounded to 280 ppm.
Over that time, the globally averaged temperature difference between the depth of an ice age and
a warm interglacial period was 4 to 6 °C — comparable to that predicted for the coming century due to anthropogenic global warming under the fossil - fuel - intensive, business - as - usual scenario.
Loutre and Berger (2002) suggest that Marine Isotope Stage 11 (MIS 11) from 405 to 340 ka would make a better analogue for future climate than the Last Interglacial, due to it being
a warmer interglacial period, but with an orbital insolation signal that correlates closely with the recent past and future, giving a much better comparison of orbital forcing.
In each hundred - thousand year period, there is an ice - age that lasts about ninety thousand years and
a warm interglacial period that lasts about ten thousand years.
It is obtained by comparing the current
warm interglacial period, called the Holocene, which has existed on planet Earth for the past ten thousand years, with...»