Response of the water use efficiency of natural vegetation to drought in Northeast China

被引:25
作者
Liu, Dan [1 ,2 ,3 ]
Yu, Chenglong [1 ,2 ,3 ]
Zhao, Fang [4 ]
机构
[1] China Meteorol Adm, Northeast China Ecol & Meteorol Open Innovat Lab, Harbin 150030, Heilongjiang, Peoples R China
[2] Meteorol Acad Workstat Heilongjiang Prov, Harbin 150030, Heilongjiang, Peoples R China
[3] Heilongjiang Prov Inst Meteorol Sci, Harbin 150030, Heilongjiang, Peoples R China
[4] Ningxia Univ, Coll Agron, Yinchuan 750021, Peoples R China
基金
中国国家自然科学基金;
关键词
natural vegetation; drought; water use efficiency (WUE); TERRESTRIAL ECOSYSTEMS; PRIMARY PRODUCTIVITY; CARBON; EVAPOTRANSPIRATION; MODIS; LEAF; DYNAMICS; CLIMATE; FOREST; CO2;
D O I
10.1007/s11442-018-1494-9
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Drought has become a problem that is universally faced by global terrestrial ecosystems. Northeast China is located in a region sensitive to global climate changes, and one of the main impacts of climate changes in Northeast China is manifested as drought in growing seasons. This study analyzes the spatio-temporal evolution law of the water use efficiency (WUE) of the main natural vegetation (i.e., cold-temperate coniferous forests, temperate pine-broad-leaved mixed forests, warm-temperate deciduous broad-leaved forests, and grasslands) in Northeast China based on public MODIS data products, including MCD12Q1, MOD15A2H, MOD16A2, and MOD17A3H, and meteorological data from 2002 to 2013. The influence of drought events on the WUE of different vegetation types and their response to drought events are also investigated. The study findings are as follows: (1) drought in Northeast China frequently occurs in the regions stretching from 114.55A degrees E to 120.90A degrees E, and the percentage of drought area among the forests is lower than that among the grasslands during these years; (2) the annual average WUE of the natural vegetation ranges from 0.82 to 1.08 C/kg(-1)H(2)O, and the WUE of forests (0.82 to 1.08 C/kg(-1)H(2)O) is universally higher than that of grasslands (0.84 to 0.99 C/kg(-1)H(2)O; (3) in 2008, the regions where the WUE in drought conditions is higher than that in normal water conditions account for 86.11% of the study area, and a significant linear positive correlation is found between the WUE in drought conditions and the WUE in normal water conditions, whereas the degree of drought does not influence the WUE of the natural vegetation in an obviously linear manner; and (4) the WUE for the cold-temperate coniferous forests and temperate pine-broad-leaved mixed forests with a high ET or low NPP is more likely to rise in drought conditions; the WUE for the grasslands with a low Evapotranspiration (ET), Net Primary Production (NPP), and Leaf Area Index (LAI) is more likely to rise in drought conditions; and the ET, NPP, and LAI have no significant influence on the WUE for the warm-temperate deciduous broad-leaved forests in drought conditions. This study contributes to improving the evaluation of the influence of drought on natural ecosystems.
引用
收藏
页码:611 / 628
页数:18
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