Chin J Plant Ecol ›› 2014, Vol. 38 ›› Issue (1): 1-16.DOI: 10.3724/SP.J.1258.2014.00001
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MU Shao-Jie1, ZHOU Ke-Xin1,*(), QI Yang2, CHEN Yi-Zhao3, FANG Ying1, ZHU Chao1
Received:
2013-09-09
Accepted:
2013-11-04
Online:
2014-09-09
Published:
2014-01-15
Contact:
ZHOU Ke-Xin
MU Shao-Jie, ZHOU Ke-Xin, QI Yang, CHEN Yi-Zhao, FANG Ying, ZHU Chao. Spatio-temporal patterns of precipitation-use efficiency of vegetation and their controlling factors in Inner Mongolia[J]. Chin J Plant Ecol, 2014, 38(1): 1-16.
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URL: https://www.plant-ecology.com/EN/10.3724/SP.J.1258.2014.00001
Fig. 1 Maps of land cover types in Inner Mongolia (A) and the spatial distribution of meteorological stations and sampling sites (B). C, cropland; D, desert; DBF, deciduous broad-leaved forest; DNF, deciduous needle-leaf forest; DS, desert steppe; ENF, evergreen needle-leaf forest; MF, mixed needle-leaf and broad-leaved forest; MS, meadow steppe; S, shrub; TS, typical steppe; U, urban land; W, water body.
Fig. 3 Spatial patterns of annual precipitation (A), annual mean air temperature (B), net primary productivity (NPP) (C) and precipitation-use efficiency (PUE) (D) of the vegetation in Inner Mongolia during 2001-2010.
Fig. 5 Precipitation-use efficiency (PUE) in Inner Mongolia during 2001-2010 for different vegetation types (mean ± SE). C, cropland; D, desert; DBF, deciduous broad-leaved forest; DNF, deciduous needle-leaf forest; DS, desert steppe; ENF, evergreen needle-leaf forest; MF, mixed needle-leaf and broad-leaved forest; MS, meadow steppe; S, shrub; TS, typical steppe. The numbers above the error bars are the PUE for different vegetation types, and the numbers in the brackets are the mean PUE for forest and grassland, respectively. The letters above the error bars indicate significant difference (p < 0.05).
Fig. 6 Pattern of changes in precipitation-use efficiency (PUE) with precipitation (A) and the spatial distribution of areas with different precipitation ranges (B) in Inner Mongolia.
Fig. 7 Patterns of changes in precipitation-use efficiency (PUE) with precipitation by areas with different temperatures in Inner Mongolia. A, Low temperature area. B, Moderate temperature area. C, High temperature area.
Fig. 9 Responses of precipitation-use efficiency (PUE) of vegetation to annual precipitation (A) and annual mean air temperature change (B) in Inner Mongolia during 2001-2010.
Fig. 10 Patterns of changes with precipitation in the correlation coefficient between inter-annual variations of precipitation-use efficiency (PUE) and precipitation (rPUE-P) and the correlation coefficient between inter-annual variations of PUE and air temperature (rPUE-T) in Inner Mongolia during 2001-2010.
Fig. 11 A conceptual model describing the relationship between spatial distribution of precipitation-use efficiency (PUE) and precipitation of vegetation in Inner Mongolia.
气温 Air temperature | 植被覆盖度 FVC | 叶面积指数 LAI | |
---|---|---|---|
降水量 Precipitation | -0.594 | 0.875 | 0.725 |
气温 Air temperature | -0.664 | -0.834 | |
植被覆盖度 FVC | 0.853 |
Table 1 Correlations among climatic factors and biological indices
气温 Air temperature | 植被覆盖度 FVC | 叶面积指数 LAI | |
---|---|---|---|
降水量 Precipitation | -0.594 | 0.875 | 0.725 |
气温 Air temperature | -0.664 | -0.834 | |
植被覆盖度 FVC | 0.853 |
Fig. 12 Correlations of spatial distribution of precipitation-use efficiency (PUE) with fraction of vegetation cover (FVC) (A) and leaf area index (LAI) (B) (mean ± SD).
Fig. 13 Correlations of inter-annual variations in precipitation-use efficiency (PUE) with fraction of vegetation cover (FVC) (A) and leaf area index (LAI) (B) (mean ± SD).
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