青藏高原多年冻土区不同海拔土壤含水量对气候变化的响应
张方园, 常娟, 刘健, 孙文军

Response of soil water content at different altitudes to climate change in the permafrost region of the Qinghai-Tibet Plateau: an ELM model analysis
Fangyuan ZHANG, Juan CHANG, Jian LIU, Wenjun SUN
表5 二输入变量ELM模型对土壤含水量的模拟效率参数
Table 5 Simulation efficiency parameters of ELM model with two input variables for soil water content
统计参数坡上20 cm坡上40 cm坡上65 cm
训练期SM+1SM+7SM+14训练期SM+1SM+7SM+14训练期SM+1SM+7SM+14
MAE/%3.413.633.203.004.043.302.912.654.814.834.204.00
RMSE/%5.455.945.185.005.544.824.003.576.696.345.565.66
R0.910.910.940.940.850.890.930.950.770.850.900.89
NSE0.830.820.860.870.720.790.860.890.600.690.760.75
统计参数坡下20 cm坡下40 cm坡下65 cm
训练期SM+1SM+7SM+14训练期SM+1SM+7SM+14训练期SM+1SM+7SM+14
MAE/%3.222.151.921.983.294.504.163.902.502.522.202.02
RMSE/%3.153.532.712.604.686.705.705.503.404.133.533.09
R0.940.940.970.980.930.920.950.960.920.880.930.94
NSE0.880.870.920.930.860.790.840.850.840.770.840.87