Global response of terrestrial gross primary productivity to climate extremes

被引:36
|
作者
Yuan, Minshu [1 ]
Zhu, Qiuan [1 ,2 ,10 ]
Zhang, Jiang [1 ]
Liu, Jinxun [3 ]
Chen, Huai [4 ]
Peng, Changhui [5 ]
Li, Peng [6 ]
Li, Mingxu [7 ]
Wang, Meng [8 ]
Zhao, Pengxiang [9 ]
机构
[1] Northwest A&F Univ, Coll Forestry, Ctr Ecol Forecasting & Global Change, Yangling 712100, Shaanxi, Peoples R China
[2] Hohai Univ, Coll Hydrol & Water Resources, Nanjing 210098, Peoples R China
[3] US Geol Survey, Western Geog Sci Ctr, Moffett Field, CA 94035 USA
[4] Chinese Acad Sci, Chengdu Inst Biol, Chengdu 610041, Peoples R China
[5] Univ Quebec Montreal, Inst Environm Sci, Dept Biol Sci, Case Postale 8888,Succursale Ctr Ville, Montreal, PQ H3C 3P8, Canada
[6] Hunan Normal Univ, Coll Resources & Environm Sci, Changsha 410081, Peoples R China
[7] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Beijing 100101, Peoples R China
[8] Northeast Normal Univ, Inst Peat & Mire Res, State Environm Protect Key Lab Wetland Ecol & Veg, Changchun 130024, Peoples R China
[9] Northwest A&F Univ, Coll Forestry, Yangling 712100, Shaanxi, Peoples R China
[10] Natl Sci & Technol Infrastruct China, Natl Earth Syst Sci Data Ctr, Beijing 100101, Peoples R China
基金
中国国家自然科学基金; 国家重点研发计划;
关键词
Carbon cycle; Climate extremes; Gross primary productivity; Precipitation-related indices; Temperature-related indices; NET PRIMARY PRODUCTION; MINIMUM TEMPERATURES; CARBON-DIOXIDE; CHANGE IMPACTS; SOIL-MOISTURE; PRECIPITATION; DROUGHT; LAND; HEAT; VARIABILITY;
D O I
10.1016/j.scitotenv.2020.142337
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Extreme climate events undoubtedly have essential impacts on ecosystem gross primary productivity (GPP), but the global spatio-temporal patterns of GPP responses to climate extremes are unclear. In this study, we analyzed the responses of GPP to temperature and precipitation extremes during historical (1901-2016) and future (2006-2100) periods using climate extreme indices (CEIs) developed by the Expert Team on Climate Change Detection and Indices. Eight temperature-related CEIs and eight precipitation-related CEIs were used for this analysis, along with three future greenhouse gas concentration trajectory scenarios generated by the IPCC: RCP 2.6, RCP 4.5, and RCP 8.5. Our results show that under RCP 4.5 and RCP 8.5, most climate extremes are increasing from the historical period into the future, indicating a warming globe with more frequent and more intense extreme climate events. But the increasing rate is only persistently enhanced with time under scenario RCP 8.5. GPP shows a continuous negative relationship with cold CEIs and positive relationship with wet CEIs from the historical period into the future. In all zonal scales, the changed magnitude of GPP responds strongly to extreme value-related temperature extremes under different scenarios. However, the precipitation-related extremes with the strongest GPP response are various in different regions. In the future, GPP is most sensitive to temperature extremes in upper northern latitudes and in high-altitude regions (e.g., Qinghai-Tibet Plateau) and to precipitation extremes in the tropical zone. This study may provide a basis for predicting how GPP responds to climate extremes and explaining the underlying changes in the carbon cycle. (C) 2020 Elsevier B.V. All rights reserved.
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页数:14
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