Yantai Geological Survey Center of Coastal Zone, China Geological Survey, Yantai 264000, Shandong, China.
Jiangxi Academy of Forestry/Jiangxi Nanchang Urban Ecosystem Research Station, Nanchang 330013, China.
Ying Yong Sheng Tai Xue Bao. 2024 Jul 18;35(7):1866-1876. doi: 10.13287/j.1001-9332.202407.025.
The lower limit temperature in the crop water stress index (CWSI) model refers to the canopy temperature () or the canopy-air temperature differences () under well-watered conditions, which has significant impacts on the accuracy of the model in quantifying plant water status. At present, the direct estimation of lower limit temperature based on data-driven method has been successfully used in crops, but its applicability has not been tes-ted in forest ecosystems. We collected continuously and synchronously and meteorological data in a plantation at the southern foot of Taihang Mountain to evaluate the feasibility of multiple linear regression model and BP neural network model for estimating the lower limit temperature and the accuracy of the CWSI indicating water status of the plantation. The results showed that, in the forest ecosystem without irrigation conditions, the lower limit temperature could be obtained by setting soil moisture as saturation in the multiple linear regression mo-del and the BP neural network model with soil water content, wind speed, net radiation, vapor pressure deficit and air temperature as input parameters. Combining the lower limit temperature and the upper limit temperature determined by the theoretical equation to normalize the measured and could realize the non-destructive, rapid, and automatic diagnosis of the water status of plantation. Among them, the CWSI obtained by combining the lower limit temperature determined by the under well-watered condition calculated by the BP neural network model and the upper limit temperature was the most suitable for accurate monitoring water status of the plantation. The coefficient of determination, root mean square error, and index of agreement between the calculated CWSI and measured CWSI were 0.81, 0.08, and 0.90, respectively. This study could provide a reference method for efficient and accurate monitoring of forest ecosystem water status.
作物水分胁迫指数(CWSI)模型中的下限温度是指在充分供水条件下的冠层温度()或冠层-空气温度差(),这对模型定量描述植物水分状况的准确性有重要影响。目前,基于数据驱动的方法直接估算下限温度已成功应用于作物,但尚未在森林生态系统中进行测试。本研究在太行山东南麓的人工林连续同步采集和气象数据,以评估多元线性回归模型和 BP 神经网络模型估算下限温度的可行性,及其在指示林分水分状况方面的 CWSI 精度。结果表明,在无灌溉条件的森林生态系统中,可通过在多元线性回归模型中设定土壤湿度为饱和,以及在以土壤水分含量、风速、净辐射、水汽压亏缺和空气温度为输入参数的 BP 神经网络模型中设定土壤水分含量为饱和,来获取下限温度。结合由理论方程确定的下限温度和上限温度,对实测和归一化,可实现对林分水分状况的非破坏性、快速、自动诊断。其中,由结合了通过 BP 神经网络模型计算的充分供水条件下理论方程确定的下限温度和上限温度的 CWSI 估算值与实测 CWSI 之间的决定系数、均方根误差和吻合指数分别为 0.81、0.08 和 0.90,最适合准确监测林分的水分状况。本研究可为高效、准确监测森林生态系统水分状况提供参考方法。