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东北地区夏季骤旱下植被响应与恢复特征及其影响因素

Characteristics of Vegetation Response and Recovery and Their Influencing Factors Under Summer Flash Drought in Northeast China

  • 摘要: 基于ERA5-Land土壤湿度数据筛选骤旱事件,对2000~2022年东北地区夏季骤旱事件进行了识别,分析了其发展与恢复阶段的空间分布特征。在此基础上,结合MODIS叶面积指数(Leaf Area Index, LAI)分析了不同植被类型对骤旱响应与恢复阶段的差异,进一步采用随机森林与偏相关分析方法,探讨了其主导因素的空间格局。结果表明,东北地区不同植被类型对骤旱的响应与恢复存在明显差异。具体而言,森林对骤旱的响应时间最长(28 d),恢复时间最短(12 d)。相较之下,草地的响应时间最短(10 d),恢复时间最长(30 d)。此外,森林的下降速率和恢复速率均较快,分别为0.99/候和1.02/候,而草地则表现为较慢的下降和恢复速率,为0.28/候和0.41/候。主导因素分析结果表明,土壤湿度和饱和水汽压差(Vapor Pressure Deficit, VPD)是影响植被响应时间的主要因素,骤旱发展速率和气温对植被的下降速率起主要作用,植被恢复时间主要受土壤湿度和降水影响,而恢复速率主要受土壤湿度和VPD影响。气温和VPD分别决定了50%以上森林的下降速率和恢复速率,且均高于草地和农田,土壤湿度主导了超过73%的森林、草地、农田的响应时间和恢复时间。研究结果可在一定程度上为骤旱对不同生态系统的可能影响提供一定的参考,同时加深对骤旱发生后生态系统的响应与恢复的理解。

     

    Abstract: Soil moisture data derived from the ERA5-Land reanalysis dataset are used to select flash drought events and identify summer flash drought events in Northeast China during 2000-2022. The spatial distribution characteristics during the onset and recovery stages are analyzed. On this basis, the characteristics of the response and recovery of different vegetation types to a flash drought are analyzed by combining them with the MODIS Leaf Area Index, and the spatial pattern of dominant factors is further discussed using the random forest model and partial correlation analysis. The results show significant differences in the response and recovery of different vegetation types to a flash drought in Northeast China. Specifically, forests have the longest response time (28 d) but the shortest recovery time (12 d), whereas grasslands have the shortest response time (10 d) but the longest recovery time (30 d). In addition, the decrease and recovery rates of forests are both faster (0.99/pentad and 1.02/pentad, respectively), whereas those of grasslands are slower (0.28/pentad and 0.41/pentad, respectively). The results of dominant factor analysis suggest that soil moisture and vapor pressure deficit (VPD) are the main factors affecting the response time of vegetation, the onset rate of flash drought and temperature play a major role in the decrease rate, the recovery time of vegetation is mainly impacted by soil moisture and precipitation, and the recovery rate is primarily influenced by soil moisture and VPD. Moreover, temperature and VPD determine the decrease and recovery rates of more than 50% of forests. In addition, the temperature and VPD of forests are higher than those of grasslands and croplands. Furthermore, soil moisture dominates the response and recovery times of more than 73% of forests, grasslands, and croplands. The results of this study can provide some reference for the possible effects of flash droughts on different ecosystems and deepen the understanding of ecosystem response and recovery after flash droughts.

     

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