At the end of these 100,000 year cycles of temperature, what causes

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The discussion centers on the factors influencing the end of 100,000-year temperature cycles, primarily driven by changes in Earth's orbit and amplified by greenhouse gas fluctuations and albedo effects from snow and ice coverage. It highlights that the cycle's duration has varied historically, with periods of 41,000 years, raising questions about the consistency of the 100,000-year cycle and suggesting the possibility of averaging different cycle lengths. Additionally, the 413,000-year eccentricity cycle's impact on insolation is noted, though it does not align with oceanic and ice core proxies. The relationship between solar forcing and glaciation stages is complex, with significant glaciation events occurring despite minimal summer forcing variation, indicating that other factors may also play a role in climate changes.
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at the end of these 100,000 year cycles of temperature, what causes the peak temperature to fall?
 
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http://en.wikipedia.org/wiki/Milankovitch_cycles"
 
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Changes in Earth's orbit normally drive long term climate changes (warming and cooling) and are amplified by changes in greenhouse gases (CO2 and CH4) along with changes in snow and ice coverage (albedo).

http://stephenschneider.stanford.edu/Publications/PDF_Papers/Ruddiman2003.pdf

BTW, it wasn't always a 100,000 year cycle. For a significant period of time, the temperature cycle was 41,000 years. It's not entirely clear what caused that shift or if there really is a 100,000 year cycle as opposed to a series of 82,000 and 123,000 year cycles that happen to average out at 100,000 years.
 


thanks.
 
Not done yet,

Another problem is that the 413,000 years eccentricity cycle clearly shows up in the insolation cycles as amplitude modulation here, but it does not show up in the oceanic benthic foraminifera isotope proxies as well as the ice cores.

chuky-milankovitch.png


The graph shows that the total resulting solar forcing at 65 degrees north in the summer does not resemble the stages of glaciation a lot. Note especially that 400,000 years ago we see one of the biggest spikes in the glaciation together with the one of the least variation in summer forcing compared to 200,000 years ago when one of the strangest variation in summer forcing is seen together with only a small spike.

Apparantly there is some more to it, although this wasn't even the reason why Karner and Muller challenged the Milankovitch idea http://sciencemag.org/cgi/content/summary/288/5474/2143.

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