Semi-quantitative reconstruction of paleoclimate of Serbia and the Chinese Loess Plateau
The semi quantitative reconstruction of paleoclimate parameters such as Paleoprecipitation and paleotemperature in the Loess Plateau of Serbia and China in the past 1 million years is completed based on the magnetic susceptibility climate conversion function of loess established on the topsoil through the comprehensive magnetic susceptibility data of tiel stari slankamen loess profile in Serbia and Xifeng loess profile in the Loess Plateau of China in the past 1 million years. It is of great significance to study the difference and relationship of climate behavior characteristics (duration, amplitude, variability, etc.) between East Asian monsoon area and westerly affected area at different time scales during interglacial period with different temperature increase amplitude.
Semi-quantitative reconstruction of paleoclimate of Serbia and the Chinese Loess Plateau
Hao, Q. (2021). Semi-quantitative reconstruction of paleoclimate of Serbia and the Chinese Loess Plateau. A Big Earth Data Platform for Three Poles, DOI: 10.11888/Paleoenv.tpdc.271692. CSTR: 18406.11.Paleoenv.tpdc.271692. (Download the reference： RIS | Bibtex )
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Comparative study of past climate changes at multi-timescale in East Asian monsoon region and Westerly zone (No:2017YFE0112800)
NSFC Basic Research Center Program: Continental Evolution and Earth’s monsoon System (No:41888101)
NSFC National Science Fund for Distinguished Young Scholars: Quaternary Geology (No:41625010)
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