Past and future changes of streamflow in Poyang Lake Basin, Southeastern China

Abstract

Abstract.To understand the causes of the past water cycle variations and the influence of climate variability on the streamflow, lake storage, and flood potential, we analyze the changes in streamflow and the underlying drivers in four typical watersheds (Gaosha, Meigang, Saitang, and Xiashan) within the Poyang Lake Basin, based on the meteorological observations at 79 weather stations, and datasets of streamflow and river level at four hydrological stations for the period of 1961-2000. The contribution of different climate factors to the change in streamflow in each watershed is estimated quantitatively using the water balance equations. Results show that in each watershed, the annual streamflow exhibits an increasing trend from 1961-2000. The increases in streamflow by 4.80 m 3 s −1 yr −1 and 1.29 m 3 s −1 yr −1 at Meigang and Gaosha, respectively, are statistically significant at the 5 % level. The increase in precipitation is the biggest contributor to the streamflow increment in Meigang (3.79 m 3 s −1 yr −1 ), Gaosha (1.12 m 3 s −1 yr −1 ), and Xiashan (1.34 m 3 s −1 yr −1 ), while the decrease in evapotranspiration is the major factor controlling the streamflow increment in Saitang (0.19 m 3 s −1 yr −1 ). In addition, radiation and wind contribute more than actual vapor pressure and mean temperature to the changes in evapotranspiration and streamflow for the four watersheds.For revealing the possible change of streamflow due to the future climate change, we also investigate the projected precipitation and evapotranspiration from of the Coupled Model Intercomparison Project phase 3 (CMIP3) under three greenhouse gases emission scenarios (SRESA1B, SRESA2 and SRESB1) for the period of 2061-2100. When the future changes in the soil water storage changes are assumed ignorable, the streamflow shows an uptrend with the projected increases in both precipitation and evapotranspiration (except for the SRESB1 scenario in Xiashan watershed) relative to the observed mean during 1961-2000. Furthermore, the largest increase in the streamflow is found at Meigang (+4.31 %) and Xiashan (+3.84 %) under the SRESA1B scenario, while the increases will occur at Saitang (+6.87 %) and Gaosha (+5.15 %) under the SRESB1 scenario.

Effects of climatic variation on pan-evaporation in the Poyang Lake Basin, China

“…It is also the largest natural reservoir of the Yangtze River, which is important to the flood and drought control of the Yangtze River (Shankman et al 2006). The lake and its surrounding catchments have suffered from frequent droughts and floods since the 1980s (Sun et al 2012, Ye et al 2013. Evapotranspiration in the Poyang Lake Basin influences the streamflow into Poyang Lake.…”

Role of reservoir regulation and groundwater feedback in a simulated ground‐soil‐vegetation continuum: A long‐term regional scale analysis

“…The Poyang Lake basin is located in the centre of Southeast China (Figure 1(b)) and covers in total an area of approximately 160 000 km 2 (Sun et al, 2012). The Poyang Lake basin encompasses five sub-basins of the Xiushui River (the sub-basin size: 3548 km 2 ), the Ganjiang River (80 948 km 2 ), the Fuhe River (15 811 km 2 ), the Xinjiang River (15 535 km 2 ) and the Raohe River (6374 km 2 ) shown in Figure 1 (b), and the five tributaries drain off into the largest freshwater lake in China, that is, Poyang Lake (an area of 3500 km 2 in a hydrologically normal year).…”