Comprehensive analysis of the impact of climatic changes on Chinese terrestrial net primary productivity

Recent climatic changes have affected terrestrial net primary productivity (NPP). This paper presents an investigation of the impact of climatic changes on Chinese terrestrial vegetation NPP by analyzing 18 years’ (1982 to 1999) climatic data and satellite observations of vegetation activity. Results indicate that climatic changes in China have eased some critical climatic constraint on plant growth. (1) From 1982 to 1999, modeled NPP increased by 1.42%·a-1 in water-limited regions of Northwest China, 1.46%·a-1 in temperature-limited regions of Northeast China and Tibet Plateau, and 0.99%·a-1 in radia- tion-limited regions of South China and East China. (2) NPP increased by 24.2%, i.e. 0.76 petagram of carbon (Pg C) over 18 years in China. Changes in climate (with constant vegetation) directly contrib- uted nearly 11.5% (0.36 Pg C). Changes in vegetation (with constant climate) contributed 12.4% (0.40 Pg C), possibly as a result of climate-vegetation feedbacks, changes in land use, and growth stimula- tion from other mechanisms. (3) Globally, NPP declined during all three major El Ni-o events (1982 to 1983, 1987 to 1988, and 1997 to 1998) between 1982 and 2000, but Chinese vegetation productivity re- sponded differently to them because of the monsoon dynamics. In the first three events (1982 to 1983, 1987 to 1988, and 1992), Chinese vegetation NPP declined, while in the later two events (1993, 1997 to 1998) increasing obviously.

Recent climatic changes have affected terrestrial net primary productivity （NPP）. This paper presents an investigation of the impact of climatic changes on Chinese terrestrial vegetation NPP by analyzing 18 years＇ （1982 to 1999） climatic data and satellite observations of vegetation activity. Results indicate that climatic changes in China have eased some critical climatic constraint on plant growth. （1） From 1982 to 1999, modeled NPP increased by 1.42%·a^-1 in water-limited regions of Northwest China, 1.46%·a^-1in temperature-limited regions of Northeast China and Tibet Plateau, and 0.99%·a^-1 in radiation-limited regions of South China and East China. （2） NPP increased by 24.2%, i.e. 0.76 petagram of carbon （Pg C） over 18 years in China. Changes in climate （with constant vegetation） directly contributed nearly 11.5% （0.36 Pg C）. Changes in vegetation （with constant climate） contributed 12.4% （0.40 Pg C）, possibly as a result of climate-vegetation feedbacks, changes in land use, and growth stimulation from other mechanisms. （3） Globally, NPP declined during all three major El Nino events （1982 to 1983, 1987 to 1988, and 1997 to 1998） between 1982 and 2000, but Chinese vegetation productivity responded differently to them because of the monsoon dynamics. In the first three events （1982 to 1983, 1987 to 1988, and 1992）, Chinese vegetation NPP declined, while in the later two events （1993, 1997 to 1998） increasing obviously.