然后以时间步长为日，运行新安江模型，用模拟的月径流过程验证了解集方法的合理性。
The two methods are validated by running the Xin'anjiang model at a daily time step from the monthly data, and the model outputs are more accurate than the monthly hydrological model.
模型能合理反演地表温度的空间格局和河道日径流量，多年年径流的模拟误差小于10%。
The modelled spatial patterns of surface temperature and daily runoff are in well agreement with the observatio with the mean relative error less than 10%.
模型能合理反演地表温度的空间格局和河道日径流量，多年年径流的模拟误差小于10%。
The modelled spatial patterns of surface temperature and daily runoff are in well agreement with the observatio with the mean relative error less than 10%.
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