lead to strong upwelling. This interpretation appears to largely reconcile the so-called “sea-land precession-phase paradox”, as the monsoon wind strength over the oceans is not necessarily coupled with monsoon precipitation over the Asian continent1,2. However, in light of these recent discussion...
During the period of 5.2~3.0 cal ka BP, the interaction between downdraft air flow and direct monsoon precipitation reduction in low-altitude areas was the main reason for the climate change of the desert in this period. After 3.0 cal ka BP of the late Holocene, due to the continuous ...