基于BMA多模型组合的疏勒河径流预测研究
|
周婷, 温小虎, 冯起, 尹振良, 杨林山
|
Study on runoff prediction of Shule River based on BMA multi-model combination
|
Ting ZHOU, Xiaohu WEN, Qi FENG, Zhenliang YIN, Linshan YANG
|
|
表6 BMA和组成它的3个模型的预测值在3个不同流量等级的统计结果
|
Table 6 Statistical results of BMA and the forecast values of the three models that comprised it at three different flow levels
|
|
时间 | 指标 | 模型 | 训练期 | 测试期 |
---|
高水 | 中水 | 低水 | 高水 | 中水 | 低水 |
---|
t+1 | R | ELM | 0.741 | 0.930 | 0.779 | 0.781 | 0.952 | 0.842 | SVM | 0.830 | 0.935 | 0.764 | 0.781 | 0.946 | 0.838 | MARS | 0.750 | 0.924 | 0.766 | 0.689 | 0.944 | 0.817 | BMA | 0.835 | 0.940 | 0.765 | 0.949 | 0.958 | 0.962 | NSE | ELM | 0.425 | 0.857 | 0.561 | 0.506 | 0.894 | 0.671 | SVM | 0.625 | 0.874 | 0.584 | 0.645 | 0.874 | 0.694 | MARS | 0.412 | 0.851 | 0.411 | 0.033 | 0.887 | 0.667 | BMA | 0.835 | 0.941 | 0.769 | 0.523 | 0.891 | 0.832 | RMSE/(m3·s-1) | ELM | 36.657 | 9.659 | 1.971 | 40.675 | 9.319 | 2.126 | SVM | 30.624 | 8.796 | 2.228 | 1.964 | 18.664 | 21.803 | MARS | 34.611 | 9.897 | 2.021 | 46.892 | 9.368 | 2.210 | BMA | 28.506 | 8.312 | 1.987 | 38.659 | 9.021 | 2.012 | t+3 | R | ELM | 0.359 | 0.856 | 0.632 | 0.501 | 0.879 | 0.701 | SVM | 0.944 | 0.843 | 0.800 | 0.811 | 0.870 | 0.899 | MARS | 0.465 | 0.856 | 0.626 | 0.236 | 0.887 | 0.701 | BMA | 0.459 | 0.891 | 0.834 | 0.478 | 0.871 | 0.676 | NSE | ELM | 0.109 | 0.637 | 0.122 | 0.234 | 0.729 | 0.357 | SVM | 0.718 | 0.615 | 0.335 | 0.656 | 0.446 | 0.647 | MARS | 0.171 | 0.644 | 0.345 | 0.036 | 0.693 | 0.443 | BMA | 0.172 | 0.670 | 0.405 | 0.228 | 0.729 | 0.375 | RMSE/(m3·s-1) | ELM | 64.431 | 18.944 | 3.381 | 65.412 | 17.287 | 3.966 | SVM | 20.648 | 25.508 | 23.309 | 3.955 | 31.584 | 24.800 | MARS | 59.235 | 18.651 | 3.231 | 82.461 | 18.015 | 4.012 | BMA | 58.375 | 17.998 | 3.114 | 62.357 | 16.986 | 3.554 | t+5 | R | ELM | 0.321 | 0.798 | 0.556 | 0.367 | 0.848 | 0.642 | SVM | 0.285 | 0.786 | 0.513 | 0.321 | 0.855 | 0.577 | MARS | 0.315 | 0.801 | 0.549 | 0.235 | 0.850 | 0.642 | BMA | 0.326 | 0.812 | 0.561 | 0.392 | 0.862 | 0.621 | NSE | ELM | 0.101 | 0.534 | 0.288 | 0.152 | 0.656 | 0.161 | SVM | 0.081 | 0.554 | 0.263 | 0.103 | 0.652 | 0.163 | MARS | 0.111 | 0.532 | 0.279 | 0.059 | 0.641 | 0.375 | BMA | 0.126 | 0.611 | 0.306 | 0.158 | 0.734 | 0.191 | RMSE/(m3·s-1) | ELM | 70.603 | 22.687 | 4.302 | 76.542 | 21.015 | 4.736 | SVM | 80.281 | 22.225 | 1.146 | 98.263 | 21.808 | 5.121 | MARS | 69.375 | 22.325 | 4.261 | 92.162 | 19.663 | 5.012 | BMA | 70.501 | 17.865 | 3.996 | 75.826 | 15.568 | 4.346 | t+7 | R | ELM | 0.271 | 0.752 | 0.365 | 0.278 | 0.823 | 0.601 | SVM | 0.310 | 0.733 | 0.528 | 0.237 | 0.812 | 0.599 | MARS | 0.315 | 0.755 | 0.532 | 0.316 | 0.757 | 0.534 | BMA | 0.331 | 0.864 | 0.641 | 0.290 | 0.827 | 0.610 | NSE | ELM | -2.312 | 0.494 | 0.012 | -1.013 | 0.819 | 0.606 | SVM | -3.894 | 0.470 | -1.436 | -2.060 | 0.655 | -0.084 | MARS | -2.892 | 0.452 | 0.286 | -0.401 | 0.581 | 0.305 | BMA | -2.007 | 0.534 | 0.108 | -1.397 | 0.581 | 0.320 | RMSE/(m3·s-1) | ELM | 74.316 | 22.732 | 4.301 | 85.671 | 22.125 | 5.046 | SVM | 82.903 | 24.524 | 4.071 | 106.930 | 24.187 | 4.855 | MARS | 73.015 | 23.752 | 4.406 | 95.587 | 20.989 | 5.405 | BMA | 72.309 | 20.067 | 4.112 | 84.032 | 18.032 | 5.062 |
|
|
|