Synchronized slowdown of climate warming and carbon sink enhancement over deciduous broadleaf forests based on FLUXNET analysis

被引:3
作者
Xu, Tingting [1 ,2 ]
Zhang, Anzhi [1 ]
Xu, Xiyan [1 ]
Jia, Gensuo [1 ,3 ]
机构
[1] Chinese Acad Sci, Key Lab Reg Climate Environm East Asia, Inst Atmospher Phys, Beijing 100029, Peoples R China
[2] Univ Chinese Acad Sci, Beijing 101408, Peoples R China
[3] Chinese Acad Sci, Inst Atmospher Phys, POB 9804, Beijing 100029, Peoples R China
关键词
Deciduous broadleaf forests; Carbon sink enhancement; Climate warming; Slowdown; INTERANNUAL VARIABILITY; SOIL RESPIRATION; NET; HIATUS; TEMPERATURE; FLUXES; PHOTOSYNTHESIS; PRODUCTIVITY; EXCHANGE;
D O I
10.1016/j.ecolind.2023.111042
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
The temperate deciduous broadleaf forests (DBFs) are widely distributed in middle and high latitudes and play vital role in providing ecosystem services and mitigating human induced climate change, however, the responses of the carbon sink of DBFs to recent warming slowdown were not well known at regional scale. Here, we investigated the temporal pattern of carbon sink in DBFs and its drivers based on the eddy covariance carbon flux observations at 15 FLUXNET sites from 1997 to 2014. The annual mean net ecosystem production (NEP) was 272 +/- 43 g C m(-2) yr(-1) during 1997-2005 and it increased to 445 +/- 13 g C m(-2) yr(-1) during 2006-2014, as a result of boosted gross primary production (GPP) and weakened ecosystem respiration, respectively. We found slowdown in trends of temperature and carbon sink enhancement during 2006-2014. The NEP decreased at the rate of -11.9 g C m(-2) yr(-1) during the warming slowdown period (2006-2014, p < 0.05) compared to a prior strong increased trend during the warming period (1997-2005, 47.6 g C m(-2) yr(-1), p < 0.05). The mean annual temperature dominated the inter-annual variation of NEP (46.9 %), and it worked together with seasonal water availability to control the NEP changes. The slowdown of peak photosynthesis growth rate and carbon uptake period (CUP) extension may contribute to the NEP reversal during the later period. Our results demonstrated that the carbon uptake potential of temperate DBFs may highly depend on warming trends.
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页数:7
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