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Chinese Journal of Applied Ecology ›› 2018, Vol. 29 ›› Issue (2): 412-420.doi: 10.13287/j.1001-9332.201802.006

• Original Articles • Previous Articles     Next Articles

Dynamic change of Pinus tabuliformis forest productivity and its response to future climate change in Shaanxi Province, China.

HUO Xiao-ying1, PENG Shou-zhang2,3, REN Jing-yu1, CAO Yang2,3, CHEN Yun-ming2,3*   

  1. 1Institute of Soil and Water Conservation, Northwest A&F University, Yangling 712100, Shaanxi, China;
    2Stake Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau, Northwest A&F University, Yangling 712100, Shaanxi, China;
    3Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling 712100, Shaanxi, China
  • Received:2017-07-10 Online:2018-02-18 Published:2018-02-18
  • Contact: E-mail: ymchen@ms.iswc.ac.cn
  • Supported by:

    This work was supported by the Fundamental Research Funds for the Central Universities (2452017183), the National Natural Science Foundation of China (41601058), the China Special Fund for Meteorological Research in the Public Interest (Major Project) (GYHY201506001-3), and the ‘Light of West China’ Program of Chinese Academy of Sciences (XAB2015B07).

Abstract: This study analyzed the dynamics of net primary productivity (NPP) of Pinus tabuliformis forest under future climate scenarios in Shaanxi Province during 2015-2100, using a dynamic vegetation model (LPJ-GUESS). The results showed that in the 2015-2100 period, annual mean temperature of this region would significantly increase by 0.12, 0.23 and 0.54 ℃·10 a-1 under RCP2.6, RCP4.5 and RCP8.5 scenarios, respectively, while the annual precipitation would have no significant change under climate scenarios except RCP4.5, under which it would significantly increase by 14.36 mm·10 a-1. Compared with the NPP of P. tabuliformis forest in the historical period (1961-1990), it would increase by 1.6%-29.6% in the future period, and the enhancement could reach 45.4% at the end of this century (2071-2100) under RCP8.5 scenario. The NPP under the RCP8.5 scenario was the highest, followed by the RCP4.5 and RCP2.6 scenarios. During 2015-2100, the NPP in the northern Shaanxi region would significantly decrease with the rate of 41.00 and 21.00 g C·m-2·10 a-1 under the RCP2.6 and RCP4.5 scenarios, respectively, implying that this area has the potentiality to be carbon source.

Key words: Pinus tabuliformis, LPJ-GUESS model, climate change., net primary productivity