干旱区研究 ›› 2024, Vol. 41 ›› Issue (12): 2083-2093.doi: 10.13866/j.azr.2024.12.10 cstr: 32277.14.AZR.20241210

• 植物生态 • 上一篇    下一篇

环境条件对黄河流域植被干旱状态的影响特征分析

杨晓娟1,2(), 韩立新1,2(), 吕超1,2   

  1. 1.水发规划设计有限公司,山东 济南 250000
    2.山东省湖泊流域管理信息化工程技术研究中心,山东 济南 250000
  • 收稿日期:2024-06-03 修回日期:2024-10-16 出版日期:2024-12-15 发布日期:2024-12-20
  • 通讯作者: 韩立新. E-mail: 308372367@qq.com
  • 作者简介:杨晓娟(1987-),女,硕士,高级工程师,主要从事水土保持方面的研究. E-mail: sxwncc@126.com
  • 基金资助:
    山东省省级水利科研项目(SDSLKY201808);水发设计集团科研项目(SFSJKY201913)

Analysis of the influence of environmental conditions on the vegetation drought index in the Yellow River Basin

YANG Xiaojuan1,2(), HAN Lixin1,2(), LYU Chao1,2   

  1. 1. Shuifa Plannning & Design Limited Company, Jinan 250000, Shandong, China
    2. Shandong Lake Basin Management & Informationize Engineering Technology Research Center, Jinan 250000, Shandong, China
  • Received:2024-06-03 Revised:2024-10-16 Published:2024-12-15 Online:2024-12-20

摘要:

为明晰黄河流域不同植被干旱指数对气候变化的空间响应特征,选取2003—2022年的植被状态指数(VCI)、植被健康指数(VHI)、温度植被干旱指数(TVDI)与降水、温度、蒸散发数据,结合趋势分析、空间通径分析及多层感知机(MLP)回归分析,探究黄河流域3种植被干旱指数的时空变化特征,揭示气候因子对黄河流域植被干旱状态的直接影响、间接影响和综合影响。结果表明:(1) 20 a内VCI、VHI呈波动上升趋势,TVDI增减趋势不明显;空间上以温带-暖温带界限为分割,东南方向TVDI与西北方向VHI降低趋势明显。(2) 降水对VCI、温度对TVDI的直接促进作用最强,降水对TVDI、温度对VHI的间接作用最强;TVDI主要受降水的抑制作用,VCI、VHI主要受温度的促进作用。(3) 3种植被干旱指数均与降水、温度呈负相关关系,与潜在蒸散发量呈正相关关系;影响TVDI的主要影响特征为潜在蒸散发量,影响VCI、VHI的最主要影响因素为温度;VHI最适用于黄河流域的植被干旱状态判定。研究结果可为黄河流域干旱状况评估及治理提供理论依据。

关键词: 黄河流域, 干旱, 通径分析, MLP回归分析, 植被干旱指数

Abstract:

In this study, we aimed to clarify the spatial response of different vegetation drought indices to climate change in the Yellow River Basin. We selected the vegetation condition index (VCI), vegetation health index (VHI), and temperature vegetation drought index (TVDI), along with precipitation, temperature, and evapotranspiration data from 2003 to 2022. Using trend analysis, spatial path analysis, and multi-layer perceptron regression analysis, we examined the spatial and temporal variation characteristics of the three drought vegetation indices in the Yellow River Basin. Our findings reveal the direct, indirect, and overall effects of climatic factors on drought in the Yellow River Basin. The results show the following: (1) During the 20 years under study, VCI and VHI showed a fluctuating upward trend, while TVDI remained stable without significant increases or decreases. Spatially, the temperate-warm temperate boundary is delineated, revealing significant reductions in TVDI in the southeast and VHI in the northwest. (2) Precipitation has the strongest direct effect on VCI, while temperature exerts the most significant direct influence on TVDI. Additionally, the indirect effects of precipitation on TVDI and temperature on VHI are also substantial. TVDI is primarily inhibited by precipitation, while temperature predominantly enhances VCI and VHI. (3) The four drought indices exhibited a negative correlation with precipitation and temperature and a positive correlation with potential evapotranspiration. Potential evapotranspiration is the primary influencing factor for TVDI, while temperature is the main influencing factor for both VCI and VHI. Among these indices, the VHI is the most suitable for drought assessment in the Yellow River Basin. Our study offers a theoretical basis for vegetation drought assessment and management in the Yellow River Basin.

Key words: Yellow River Basin, drought, path analysis, Multi-Layer Perceptron (MLP) regression analysis, vegetation condition index