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.
Spatiotemporal variations of rainy season precipitation in the Tibetan Plateau during the past two millennia retrieved 27 March 2024 from https://phys.org/news/2024-03-spatiotemporal-variations-rainy-season-precipitation.html
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