The quantitative reconstruction of the length of the rainy season and precipitation on the Tibetan Plateau (TP) is crucial for revealing the spatiotemporal evolution of the Westerlies and South Asian monsoon, as well as its ecological and environmental effects.
The quantitative reconstruction of the length of the rainy season and precipitation on the Tibetan Plateau (TP) is crucial for revealing the spatiotemporal evolution of the Westerlies and South Asian monsoon, as well as its ecological and environmental effects.
Accurately determining the start and end times of the rainy season on the Plateau remains challenging. A recent study, published in the journal Science China Earth Sciences, quantitatively reconstructed the spatiotemporal variations of rainy season precipitation from northern TP (Kusai Lake) and central TP (Jiang Co) during the past two millennia.
