In a study published in Nature Communications, researchers have documented that persistent millennial-scale Asian winter monsoon (AWM) intensity fluctuations were superimposed on 41-kyr and ~100-kyr orbital variability during both the warmer (higher CO2) late Pliocene and colder (lower CO2) early Pleistocene, in response to both external astronomical forcing and internal climate dynamics.
Researchers find Northern Hemisphere glaciation enhances orbital- and millennial-scale Asian winter monsoon variability
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