1) Continuous streamflow is measured at about 150 locations.

2) The observation data of rainfall, evapotranspiration and streamflow from 1979 to 1984 and 1985 to 1987 were used to calibrate and validate the modal, respectively.

3) Study on mechanism of runoff and streamflow has great foreground to build hydrological model coupled with GIS and RS, and hydrological scale problems should always be paid attention to.

4) Mid-term and long-term streamflow prediction is of vital importance in flood control, reservoir operation and water resources management.

5) In view of the differences of the monthly streamflow variation between during the flood season and non-flood season, ensemble prediction model by stages is developed.

6) First the relationship between streamflow and local climate change is reviewed.

7) Spring and winter streamflow increased while summer and autumn streamflow decreased, especially, the low flow in spring exhibited significant augmented.

8) With the combination of prediction and non-prediction streamflow, runoff description based on Markov model is developed for Ertan hydropower station.

9) Overall the land use changes in the Yangtze River basin may intensify the hydrological cycle of the basin, which should increase summer precipitation and streamflow.

10) Due to the lack of reliable meteorological inputs, statistical method is commonly used to mid-term and long-term streamflow prediction.

11) After forest fire, the ability to regulate the water circulation of forest was reduced, and the changes in streamflow depended on the precipitation even more.

12) For many elements, the most substantial pathway of loss is in streamflow.

13) Generally, although most of parameters can be deduced from geographic information, some sensitive parameters in VIC have to be calibrated based on observed streamflow data.

14) Based on the data obtained by single watershed experiment,[http:///streamflow.html] the changes in streamflow by forest fire were studied.

15) The grid technique of Box-counting methods is applied to fractal dimension of daily streamflow hydrograph in the upper reaches of Minjiang River.

16) The periodic change of the precipitation led to a same change trend with the streamflow abundant or dry up in Qingshui River, but only with time lag slightly.

17) According to the variation of the components in the ground water of Streamflow within a year, the nonpoint pollutant load in a basin can be computed.