Climate flickering ended last ice age

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SUMMARY

The discussion centers on the Younger Dryas event, which commenced around 12,900 years ago, characterized by significant cooling in the Northern Hemisphere due to atmospheric and oceanic circulation changes. Recent findings suggest that climate oscillated between cold and wet conditions before stabilizing into interglacial periods. The debate highlights discrepancies in dating methods, particularly regarding varve counts in the Meerfelder maar, and raises questions about the influence of external factors, such as micrometeorite bombardments, on these climatic shifts. Participants express skepticism about speculative theories without peer-reviewed backing.

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  • Understanding of the Younger Dryas event and its climatic implications
  • Familiarity with varve dating techniques and sediment archives
  • Knowledge of atmospheric and oceanic circulation patterns
  • Awareness of micrometeorite bombardment theories in climate science
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  • Research the Younger Dryas event and its climatic impacts on the Northern Hemisphere
  • Study varve chronology and its application in paleoclimatology
  • Explore the role of micrometeorite impacts in historical climate fluctuations
  • Investigate peer-reviewed literature on the mechanisms of climate oscillations during the Younger Dryas
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Climate scientists, geologists, and researchers interested in paleoclimatology and the mechanisms behind historical climate changes.

wolram
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http://www.sciencedaily.com/releases/2009/02/090216092824.htm

Quote.
The Younger Dryas event, which began approximately 12,900 years ago, was a period of rapid cooling in the Northern Hemisphere, driven by large-scale reorganizations of patterns of atmospheric and oceanic circulation. Environmental changes during this period have been documented by both proxy-based reconstructions from sediment archives and model simulations, but there is currently no consensus on the exact mechanisms of onset, stabilization, or termination of the Younger Dryas. In contrast to existing knowledge, the Nature article shows that the climate shifted repeatedly from cold and dry to wet and less cold, from decade to decade, before interglacial conditions were finally reached and the climate system became more stable.
 
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Yeah, great article Wolram.

Very interesting argument Andre. Very enlightening. Sorry to go on, but the 'large body close encounter' of a giant comet like near-miss with the Earth around 40,000 years ago we discussed earlier fits the bill. The tilt would have increased and then oscillated before settling into the Earth's obliquity cycle we are now familiar with. I'm surprised myself to see how it seems to fit all the criteria so effortlessly.
 
Does it with 30,000 years in between?

Moreover there is something fishy with that article. It suggests that the transition to the YD in the Meerfelder maar varves was around 12,870 varve count years ago. However here it is 12,700 years, which is quite robust, as being 200 varve years before the mega eruption of the Laacher see maar around 12,920 years ago.
 
Andre said:
Does it with 30,000 years in between?
It could take 30,000 years to reach it's maximum increase in obliquity, and then oscillate on a smaller scale until stabilization.
 
Mammo, overly speculative posts are not allowed here. Do you have any peer reviewed papers on such an incident? I have found nothing in my searches that even suggests such a thing.
 
I do seem to have got a bit carried away with myself Evo. I doubt whether there's a paper on the idea, I admit. I'm interested in other people's explanations of the fluctuations, it's a fascinating topic.
 
You guys will have to bicker amongst yourselves, i find there is is no truths in these things, may be we will never know, but i hope for enlightenment, but now i am fizzled out.
 
wolram said:
http://www.sciencedaily.com/releases/2009/02/090216092824.htm
The Younger Dryas event, which began approximately 12,900 years ago, was a period of rapid cooling in the Northern Hemisphere, driven by large-scale reorganizations of patterns of atmospheric and oceanic circulation.
The evidence of a micrometeorite bombardment (Firestone et al) around 12.9 ka is presumably a candidate for this fluctuating climate change.
 

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