2013
DOI: 10.1016/j.jhydrol.2013.03.049
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Large-scale hydrodynamic modeling of the middle Yangtze River Basin with complex river–lake interactions

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Cited by 107 publications
(61 citation statements)
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References 36 publications
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“…Long et al (2015) [21] adopted a global hydrological model (PCR-GLOBWB) for simulating total water storage changes in the Yangtze River basin. Lai et al (2013) [22] developed a new Coupled Hydrodynamic Analysis Model aiming to simulate the water system in the middle reaches of the Yangtze River. Long et al (2015) adopted a global hydrological model to simulate water storage changes for the Yangtze River basin.…”
Section: Rainfall Discharge Modeling Over the Jinsha River Basinmentioning
confidence: 99%
“…Long et al (2015) [21] adopted a global hydrological model (PCR-GLOBWB) for simulating total water storage changes in the Yangtze River basin. Lai et al (2013) [22] developed a new Coupled Hydrodynamic Analysis Model aiming to simulate the water system in the middle reaches of the Yangtze River. Long et al (2015) adopted a global hydrological model to simulate water storage changes for the Yangtze River basin.…”
Section: Rainfall Discharge Modeling Over the Jinsha River Basinmentioning
confidence: 99%
“…Regional evapotranspiration estimates were extracted from the latest satellite products (MOD16) of the Moderate resolution Imaging Spectroradiometer (MODIS) (http://www.ntsg.umt.edu/project/mod16) for the lake region and the gauged basin in 2000-2010. In addition, the lake stage at Hukou is available for the case without the TGD for the period 2006-2010, which is the output of the CHAM-Yangtze model (Lai et al, 2013).…”
Section: Y Liu and G Wu: Hydroclimatological Influences On Droughtsmentioning
confidence: 99%
“…Water impoundments of the TGD incurred water level drops with an average estimate of 2 m at the outlet of Poyang Lake in mid-September to November for the period 2003-2008(Guo et al, 2012Zhang et al, 2012). Alternatively, Lai et al (2013) developed a hydrodynamic model for the middle Yangtze River region (CHAM-Yangtze), in which they coupled both Poyang Lake and the Yangtze River to account for the lake-river interactions explicitly. They demonstrated that the lake stage was more sensitive to the alternation in lake inflow compared to the same discharge modification in the Yangtze River (Lai et al, 2014a).…”
Section: Introductionmentioning
confidence: 99%
“…Previous attempts to simulate the hydrodynamics of Poyang Lake have been limited. A coupled 1-D and 2-D model has been created to simulate the interaction between the Yangtze River and its linked lakes, including Poyang Lake [16]. However, the model is not concentrated on the hydrodynamics of Poyang Lake and the simulated current velocities were not calibrated and validated by field measurements.…”
Section: Introductionmentioning
confidence: 99%