The Nature article “Climate and atmospheric history of the past 420,000 years from the Vostok
ice core, Antarctica.” (see https://www.nature.com/articles/20859)
provides a wealth of perspectives on climate variations over the last 400,000
years along with some insights into future climate response. The analysis reveals
interrelationships between many measurable quantities including CO2, CH4,
temperature variations from deuterium (hydrogen atom with a neutron),
precipitation rate and more.
The authors illustrate the frequency of variations of measurable quantities (CO2, CH4,...) over the period of observation and their results
reveal a persistent 100,000 year (orbital eccentricity) spectral peak. The 41,000 year (axial tilt) peak is often present but of lower amplitude and less consistent.
The variations associated with eccentricity,
obliquity and precession have periods of roughly 100,000 years, 41,000 years
and 21,000 years respectively (above). Astronomical forcing with
100,000 and 41,000 year periods is evident for most of the variables, while
21,000 precession seems less persistent. Eccentricity, obliquity and precession orbital features are visually illustrated below (taken from http://deschutes.gso.uri.edu/~rutherfo/milankovitch.html).
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