Research Article

Complexity to Forecast Flood: Problem Definition and Spatiotemporal Attention LSTM Solution

Table 2

Comparison experiments on Lech dataset to show sensibility of different input hydrological features, where Wo- refers to operation of eliminating one specifical hydrological feature, ST-Water is short for hydrological feature of soil tension water, subscripts A and σ represent mean value and bias value respectively, R, M and D represents measurements of RMSE, MAPE, and DC, respectively. Note that bold texts indicate best performance among comparative methods. We define unit for M as %.

MethodsRT+3RT+6RT+9RARσMT+3MT+6MT+9MAMσDT+3DT+6DT+9DADσ

Wo-precipitation117.0121.3145.3127.961.8829.6131.9636.3132.6316.120.350.330.280.320.49
Wo-evaporation65.8274.0885.1675.029.0016.4918.5322.3919.142.630.800.760.640.730.08
Wo-ST-water80.4474.7477.9277.7011.6819.9118.9219.6419.492.980.710.800.730.750.06
Wo-temperature63.3868.5175.5069.133.1115.9417.1819.0417.390.880.820.790.740.780.03
Wo-wind63.8168.1275.9169.283.2615.9817.0618.3217.120.610.820.780.760.790.02
STA-LSTM60.9465.5671.5666.0215.2416.3917.8916.510.840.810.770.81