• Acta Geographica Sinica
  • Vol. 75, Issue 7, 1432 (2020)
Jingyun ZHENG1、2, Xuezhen ZHANG1、2, Yang LIU1, and Zhixin HAO1、2、*
Author Affiliations
  • 1Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographical Sciences and Natural Resources Research, CAS, Beijing 100101, China
  • 2University of Chinese Academy of Sciences, Beijing 100049, China
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    DOI: 10.11821/dlxb202007008 Cite this Article
    Jingyun ZHENG, Xuezhen ZHANG, Yang LIU, Zhixin HAO. The assessment on hydroclimatic changes of different regions in China at multi-scale during the past millennium[J]. Acta Geographica Sinica, 2020, 75(7): 1432 Copy Citation Text show less
    Map of cited proxies that used for reconstruction on hydroclimate in China
    Fig. 1. Map of cited proxies that used for reconstruction on hydroclimate in China
    The dry/wet index series (left) and power spectrum (right) for the past 2000 years in central-eastern China (a) and its sub-regions of North China Plain (b), Jiang-Huai Area (b), and Jiangnan Area(d)
    Fig. 2. The dry/wet index series (left) and power spectrum (right) for the past 2000 years in central-eastern China (a) and its sub-regions of North China Plain (b), Jiang-Huai Area (b), and Jiangnan Area(d)
    Hydroclimate reconstructions based on multi-proxies in Northeast China and semi-arid region in North China
    Fig. 3. Hydroclimate reconstructions based on multi-proxies in Northeast China and semi-arid region in North China
    Precipitation reconstructions based on tree rings in Northwest China
    Fig. 4. Precipitation reconstructions based on tree rings in Northwest China
    Dry/wet changes in the north of Tibetan Plateau based on tree rings over the past 3000 years
    Fig. 5. Dry/wet changes in the north of Tibetan Plateau based on tree rings over the past 3000 years
    Dry/wet changes reconstructed from tree rings in the south of Tibetan Plateau over the past 1000 years
    Fig. 6. Dry/wet changes reconstructed from tree rings in the south of Tibetan Plateau over the past 1000 years
    Comparison on the changes of precipitations from previous July to current June in the northeast (a) and south (b) of Tibetan Plateau, and the bar chart between (a) and (b) shows their correlation coefficient in the 50-year running windows
    Fig. 7. Comparison on the changes of precipitations from previous July to current June in the northeast (a) and south (b) of Tibetan Plateau, and the bar chart between (a) and (b) shows their correlation coefficient in the 50-year running windows
    Jingyun ZHENG, Xuezhen ZHANG, Yang LIU, Zhixin HAO. The assessment on hydroclimatic changes of different regions in China at multi-scale during the past millennium[J]. Acta Geographica Sinica, 2020, 75(7): 1432
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