The discovery in ice core records that atmospheric concentrations of two potent greenhouse gases, carbon dioxide and methane, have decreased during past glacial periods and
peaked during interglacials indicates important feedback processes in the Earth system.
Not exact matches
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.
Other studies indicate that the
peak sea level
during the latest
interglacial was a few metres higher than today, implying that
peak temperatures were higher.
During this period, global temperatures were 1.5 - 2.0 °C warmer than the
peak warmth of the present
interglacial, or Holocene, in which we are now living.
Once a temperature threshold is breached, abrupt events follow due to amplifying feedbacks, even within a few years, examples being (1) freeze events which followed temperature
peaks during past
interglacial peaks due to influx of cold ice - melt water into the north Atlantic Ocean; (2) the Dansgaard — Oeschger warming events
during the last glacial period; (3) the Younger dryas stadial freeze and the Laurentian stadial freeze.
Sea level in the Eemian
interglacial peaked some 6 — 9 meters higher than it's ever been
during the Holocene.
The observation that led to his conclusion was that in the ice core records
during interglacials methane rises to a
peak and then decreases as temperature rises and falls.
During this
interglacial, methane rose,
peaked, started to decrease and then stopped decreasing and began increasing again starting about 5,000 years ago.
During the Last
Interglacial Period (about 129,000 to 116,000 years ago) when
peak global warmth was not more than 2 °C above pre-industrial temperatures, and
peak global annual sea surface temperatures were 0.7 [0.1 to 1.3] °C warmer (medium confidence), maximum GMSL was at least 5 m higher than at present (very high confidence), but did not exceed 10 m (high confidence).
The Earth must be in radiative (energy) balance within a very small fraction of 1 W / m2 averaged over the current
interglacial period as well as
during the
peak of the last ice age 20,000 years ago.