The release of carbon dioxide and methane from the Arctic will provide a positive feedback to climate change which will be more
important over longer timescales — millennia and longer.
Not exact matches
It would require a much stronger relationship of temperature driving CO2 than occurred during the ice age — interglacial oscillations (and it is also
important to remember that those changes occurred
over much
longer timescales too... which is the presumed reason why there is a several hundred year lag time between temperatures starting to rise or fall and CO2 starting to rise or fall).
Components of the Earth's climate system that vary
over long timescales, such as ice sheets and vegetation, could have an
important effect on this temperature sensitivity, but have often been neglected.