Chin J Plant Ecol ›› 2025, Vol. 49 ›› Issue (3): 415-431.DOI: 10.17521/cjpe.2023.0265 cstr: 32100.14.cjpe.2023.0265
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LIU Ke-Yan1, HAN Lu1, SONG Wu-Ye1, ZHANG Chu-Rui1, HU Xu1, XU Hang1, CHEN Li-Xin1,2,*()
Received:
2023-09-14
Accepted:
2024-04-08
Online:
2025-03-20
Published:
2024-04-09
Contact:
CHEN Li-Xin
Supported by:
LIU Ke-Yan, HAN Lu, SONG Wu-Ye, ZHANG Chu-Rui, HU Xu, XU Hang, CHEN Li-Xin. Detection of drought effects on photosynthetic stability of vegetation on the Loess Plateau based on solar-induced chlorophyll fluorescence[J]. Chin J Plant Ecol, 2025, 49(3): 415-431.
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URL: https://www.plant-ecology.com/EN/10.17521/cjpe.2023.0265
干旱等级 Drought classification | SPEI值 SPEI value |
---|---|
轻度干旱 Mild drought | -1.0 < SPEI ≤ -0.5 |
中度干旱 Moderate drought | -1.5 < SPEI ≤ -1.0 |
重度干旱 Severe drought | SPEI ≤ -1.5 |
Table 1 Drought classification based on standardized precipitation evapotranspiration index (SPEI)
干旱等级 Drought classification | SPEI值 SPEI value |
---|---|
轻度干旱 Mild drought | -1.0 < SPEI ≤ -0.5 |
中度干旱 Moderate drought | -1.5 < SPEI ≤ -1.0 |
重度干旱 Severe drought | SPEI ≤ -1.5 |
系数 Coefficient | 变化幅度的解释 Explanation of the magnitude of change | 正负符号的解释 Interpretation of positive and negative signs |
---|---|---|
α (Yt-1的系数) α (coefficients for Yt-1) | 绝对值在0到1之间代表植被恢复平衡, 绝对值越大表明复原力越低。绝对值大于1, 植被将以振荡的方式恢复平衡 Absolute values between 0 and 1 represent systems returning to equilibrium, with large absolute values indicating a low resilience. Absolute values are larger than 1, the system returns to equilibrium in an oscillating way | 正异常与之前的异常相似; 负异常与之前的异常相似, 但符号相反 Positive anomalies are similar to the previous anomaly. Negative anomalies are similar to the previous anomaly, but with the opposite sign |
β (SPEIt的系数)和σ (Tt的系数) β (coefficients for SPEIt) and σ (coefficients for Tt) | 绝对值越大表明植被对干旱/温度异常越敏感, 即植被对短期干旱/温度反常的抵抗力越小 Large absolute values indicate a low resistance to droughts/ temperature anomalies | 正值表示更湿润条件下或更高的温度下植被光合作用增加; 负值表示更润湿条件下或更高的温度下植被光合作用下降 Positive values indicate wetter conditions or higher temperatures induce the increase of solar-induced chlorophyll fluorescence (SIF). Negative values indicate wetter conditions or higher temperatures induce the decrease of SIF |
Table 2 Interpretation of autoregressive model coefficients for assessing vegetation photosynthetic stability
系数 Coefficient | 变化幅度的解释 Explanation of the magnitude of change | 正负符号的解释 Interpretation of positive and negative signs |
---|---|---|
α (Yt-1的系数) α (coefficients for Yt-1) | 绝对值在0到1之间代表植被恢复平衡, 绝对值越大表明复原力越低。绝对值大于1, 植被将以振荡的方式恢复平衡 Absolute values between 0 and 1 represent systems returning to equilibrium, with large absolute values indicating a low resilience. Absolute values are larger than 1, the system returns to equilibrium in an oscillating way | 正异常与之前的异常相似; 负异常与之前的异常相似, 但符号相反 Positive anomalies are similar to the previous anomaly. Negative anomalies are similar to the previous anomaly, but with the opposite sign |
β (SPEIt的系数)和σ (Tt的系数) β (coefficients for SPEIt) and σ (coefficients for Tt) | 绝对值越大表明植被对干旱/温度异常越敏感, 即植被对短期干旱/温度反常的抵抗力越小 Large absolute values indicate a low resistance to droughts/ temperature anomalies | 正值表示更湿润条件下或更高的温度下植被光合作用增加; 负值表示更润湿条件下或更高的温度下植被光合作用下降 Positive values indicate wetter conditions or higher temperatures induce the increase of solar-induced chlorophyll fluorescence (SIF). Negative values indicate wetter conditions or higher temperatures induce the decrease of SIF |
Fig. 3 Spatial distribution of drought severity on the Loess Plateau. A, 2001. B, 2005. C, 2009. D, 2015. SPEI, standardized precipitation evapotranspiration index.
Fig. 4 Spatial distribution of solar-induced chlorophyll fluorescence (SIF) anomalies on the Loess Plateau. A, 2001. B, 2005. C, 2009. D, 2015. The black portion of the pie chart represents a very small percentage.
Fig. 6 Changes in photosynthetic stability of vegetation on the Loess Plateau under different degrees of drought. SPEI, standardized precipitation evapotranspiration index.
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