Evaluating the responses of net primary productivity and carbon use efficiency of global grassland to climate variability along an aridity gradient

被引:103
作者
Liu, Yangyang [1 ]
Yang, Yue [2 ]
Wang, Qian [1 ]
Du, Xiaolong [1 ]
Li, Jianlong [1 ]
Gang, Chengcheng [3 ]
Zhou, Wei [4 ]
Wang, Zhaoqi [5 ]
机构
[1] Nanjing Univ, Sch Life Sci, Dept Ecol, Xianlin Rd 163, Nanjing 210046, Jiangsu, Peoples R China
[2] Nanjing Inst Environm Sci, Minist Environm Protect Peoples Republ China, Nanjing 210042, Jiangsu, Peoples R China
[3] Northwest A&F Univ, Inst Soil & Water Conservat, Yangling 712100, Shaanxi, Peoples R China
[4] Chongqing Jiaotong Univ, Coll Architecture & Urban Planning, Chongqing 400074, Peoples R China
[5] Peking Univ, Coll Urban & Environm Sci, Beijing 100871, Peoples R China
基金
中国国家自然科学基金;
关键词
Aridity index; Net primary productivity (NPP); Carbon use efficiency (CUE); Climate variability; Grassland ecosystems; WATER-USE EFFICIENCY; TIBETAN PLATEAU; DRIVING FORCES; PINUS-RADIATA; RESPIRATION; DROUGHT; CHINA; VEGETATION; ECOSYSTEM; SEQUESTRATION;
D O I
10.1016/j.scitotenv.2018.10.295
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Net primary productivity (NPP) and carbon use efficiency (CUE) are common ecological indicators for assessing the terrestrial carbon cycle. However, despite their widespread use, considerable uncertainties exist toward the response patterns of NPP and CUE to climate variability along an aridity gradient, especially for grassland ecosystems. The aridity index (AI) was calculated in this study to specify arid-humid zones across the global grassland ecosystem. The dynamics of grassland NPP, CUE, and their dependence on climate under different AI levels from 2000 to 2013 were investigated. Results showed that the NPP and CUE of grasslands demonstrated a slightly increasing trend with regional increasing precipitation in most AI zones, except for arid regions (AR) from 2000 to 2013. The NPP and CUE of grasslands exhibited a remarkable spatial heterogeneity in different AI zones. High NPP values mainly occurred in the dry and sub-humid (DSH) and humid (HU) regions of Southern Hemisphere with warm and wet climate. High CUE values were mostly found in the HU of the Northern Hemisphere with cold and wet climate. In addition, low NPP and CUE values were observed in most parts of AR and semi-AR (SAR) with hot and dry climate. Overall, the NPP and CUE of grasslands were significantly affected by precipitation at the global scale. Specifically, grassland NPP was positively correlated with the mean annual precipitation (MAP) in SAR and AR, but negatively related with the MAP in the HU region. The positive correlation between NPP and mean annual temperature (MAT) was found only for HU regions. Grassland CUE indicated a positive relation with MAP, but a negative relation was observed with MAT in all AI zones. The correlation coefficients between CUE and MAP decreased from AR to HU regions. This finding indicated that grassland CUE was highly sensitive to precipitation in dry areas, but this relationship weakened in HU ecosystems. (C) 2018 Elsevier B.V. All rights reserved.
引用
收藏
页码:671 / 682
页数:12
相关论文
共 44 条
[21]  
Noy-Meir I., 1973, Annual Review of Ecology and Systematics, V4, P25, DOI 10.1146/annurev.es.04.110173.000325
[22]   Tundra CO2 fluxes in response to experimental warming across latitudinal and moisture gradients [J].
Oberbauer, Steven F. ;
Tweedie, Craig E. ;
Welker, Jeff M. ;
Fahnestock, Jace T. ;
Henry, Greg H. R. ;
Webber, Patrick J. ;
Hollister, Robert D. ;
Walker, Marilyn D. ;
Kuchy, Andrea ;
Elmore, Elizabeth ;
Starr, Gregory .
ECOLOGICAL MONOGRAPHS, 2007, 77 (02) :221-238
[23]   Country-level net primary production distribution and response to drought and land cover change [J].
Peng, Dailiang ;
Zhang, Bing ;
Wu, Chaoyang ;
Huete, Alfredo R. ;
Gonsamo, Alemu ;
Lei, Liping ;
Ponce-Campos, Guillermo E. ;
Liu, Xinjie ;
Wu, Yanhong .
SCIENCE OF THE TOTAL ENVIRONMENT, 2017, 574 :65-77
[24]  
Running SW, 2004, BIOSCIENCE, V54, P547, DOI 10.1641/0006-3568(2004)054[0547:ACSMOG]2.0.CO
[25]  
2
[26]  
Ryan MG, 1996, TREE PHYSIOL, V16, P333
[27]  
Schuur EAG, 2003, ECOLOGY, V84, P1165, DOI 10.1890/0012-9658(2003)084[1165:PAGCRT]2.0.CO
[28]  
2
[29]  
Schuur EAG, 2001, ECOLOGY, V82, P3182, DOI 10.1890/0012-9658(2001)082[3182:CCASCS]2.0.CO
[30]  
2