Global temperature declined after the Holocene Climatic Optimum, causing a sea level lowering of between 4000 and 2500 years before present.
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It is a well studied ice cap, and is important to understanding the last Climactic Optimum . ( Holocene climatic optimum)
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Another event during the middle Eocene that was a sudden and temporary reversal of the cooling conditions was the Middle Eocene Climatic Optimum.
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During the Eemian the climatic optimum took place during pollen zone E4 in the type area ( city of Amersfoort, Netherlands ).
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During the Holocene Climatic Optimum the monsoonal rains that reached the Loess Plateau in the modern era pushed the desert back to the Yellow River.
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Points of correlation indicate that in these two locations the Holocene climatic optimum ( post glacial climatic optimum ) probably occurred at the same time.
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Points of correlation indicate that in these two locations the Holocene climatic optimum ( post glacial climatic optimum ) probably occurred at the same time.
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And, here again as with Dye 3, steady state in grain growth was reached and continued through the post-glacial climatic optimum.
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:: : See Holocene, Anthropocene, Holocene Climatic Optimum, Little Ice Age, Climate change and agriculture and current sea level rise.
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These two periods occurred during the Holocene Climatic Optimum ( between 4000 BC and 2000 BC ), when the local climate became more humid.
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