The National Key Laboratory of Water Disaster Prevention, Hohai University, Nanjing 210098, China; College of Hydrology and Water Resources, Hohai University, Nanjing 210098, China.
The National Key Laboratory of Water Disaster Prevention, Hohai University, Nanjing 210098, China; College of Hydrology and Water Resources, Hohai University, Nanjing 210098, China; Yinshanbeilu Grassland Eco-hydrology National Observation and Research Station, China Institute of Water Resources and Hydropower Research, Beijing 100038, China.
Sci Total Environ. 2024 Nov 15;951:175423. doi: 10.1016/j.scitotenv.2024.175423. Epub 2024 Aug 10.
Ecological drought is a complex process in terrestrial ecosystems where vegetation's eco-physiological functions are impaired due to water stress. However, there is currently a lack of long-term assessment of ecological drought from an eco-physiological perspective. In this study, the standardized ecological drought index (SESNDI) was developed using actual evaporation, root soil moisture, and kernel normalized difference vegetation index via the Euclidean distance method, reflecting ecosystem physiology, water supply capacity, and vegetation status. Solar-induced chlorophyll fluorescence validated SESNDI by reflecting vegetation photosynthesis. Using China as an example, severely impacted by climate change and ecological restoration, ecological drought's spatio-temporal variation and propagation characteristics was evaluated using clustering algorithms. The results demonstrated that (1) SESNDI showed superior performance over several other drought indices. (2) During 1982-2020, ecological drought was prevalent from 1990 to 2010, especially in the central and northeastern regions. (3) Compared to 1982-2000, the median duration and affected area of ecological drought events during 2001-2020 reduced by four months and 1.51 × 10 km, respectively, while the median intensity increased by 0.06. (4) Decreased precipitation and increased temperature were the primary factors contributing to the frequent occurrence of ecological drought in China from 1990 to 2010. This study offers a crucial methodology for evaluating ecological drought, serving as a reference for developing effective terrestrial restoration strategies.
生态干旱是陆地生态系统中一个复杂的过程,由于水分胁迫,植被的生态生理功能受到损害。然而,目前缺乏从生态生理角度对生态干旱进行长期评估。本研究利用实际蒸散量、根区土壤水分和核标准化植被指数,通过欧几里得距离法,开发了标准化生态干旱指数(SESNDI),反映了生态系统的生理、供水能力和植被状况。太阳诱导叶绿素荧光通过反映植被光合作用来验证 SESNDI。以中国为例,中国受气候变化和生态恢复的严重影响,本研究采用聚类算法评估了生态干旱的时空变化和传播特征。结果表明:(1)SESNDI 优于其他几种干旱指数;(2)1982-2020 年期间,1990-2010 年生态干旱较为普遍,尤其是在中部和东北地区;(3)与 1982-2000 年相比,2001-2020 年生态干旱事件的中值持续时间和受影响面积分别减少了 4 个月和 1.51×10^4km^2,而中值强度增加了 0.06;(4)降水减少和温度升高是导致 1990-2010 年中国生态干旱频发的主要因素。本研究为评估生态干旱提供了重要的方法,为制定有效的陆地恢复策略提供了参考。