Stable isotopes in precipitation are important indicators for studying changes in the Earth’s water cycle and reconstructing the paleoclimate history. Previous studies have shown that the precipitation stable isotopes in Asia recorded in stalagmites and other sediments have prominent periodic change patterns on the 10,000-year scale (orbital scale) in geological periods, but in the scientific community there are still controversies about the climatological significance indicated by the precipitation isotope changes in different parts of Asia.
Click here for original story, Climate simulation reveals precipitation isotope changes in Asian monsoon and arid regions for the past 300,000 years
Source: Phys.org