annual flood
1.The regional flood frequency analysis based on L?moment proposed by Hosking in 1997 was applied to the flood frequency analysis of annual maximum flood volume for five hydrological stations, including Yichang, Shashi, Luoshan, Hankou, and Datong on the middle and lower reaches of the Yangtze River.
3.Abstract: The sea-surface temperature change in October along the eastern Pacific equator is obviously counter-correlation to the western Pacific ridge line of the subtropical high of the coming early summer (June); The sea-surface temperature annual change has a sensitively instructive meaning on the precipitation of the coming flood season in Qingdao area.
7.By using the 1960—2004 flood season (from May to September) daily precipitation data of 87 stations in six provinces and one city in the mid-lower reaches of theYangtze River, with EOF, REOF, tendency analysis and Morlet wavelet analysis, it is analyzed that the annual extreme precipitation of various stations and its spatial distribution for the recent 45 years.
8.Through the statistics and analysis of runoff and amount of sand lost in the downstream of Weihe in recent years, it is discovered that in the downstream of Weihe the magnitude sand season was ahead of the main flood season relatively within the year; Variation tendency of annual runoff and amount of sand lost was identical basically , and the quantity of water and sand at Huaxian gauging station was tailing-off continuously from the 1960 to 2005; There was direct relation between the situation of rushing or silting deposits and rainfall at this section of the river: The river depositing in the year which is rich rainfall, the eroding in the poor rainfall.

