Abstract
As the largest hydroelectric project worldwide, previous studies indicate that the Three Gorges Dam (TGD) affects the local climate because of the changes of hydrological cycle caused by the impounding and draining of the TGD. However, previous studies do not analyze the long-term precipitation changes before and after the impoundment, and the variation characteristics of local precipitation remain elusive. In this study, we use precipitation anomaly data derived from the CN05.1 precipitation dataset between 1988 and 2017 to trace the changes of precipitation before and after the construction of the TGD (i.e., 1988–2002 and 2003–2017), in the Three Gorges Reservoir Area (TGRA). Results showed that the annual and dry season precipitation anomaly in the TGRA presented an increasing trend, and the precipitation anomaly showed a slight decrease during the flood season. After the impoundment of TGD, the precipitation concentration degree in the TGRA decreased, indicating that the precipitation became increasingly uniform, and the precipitation concentration period insignificantly increased. A resonance phenomenon between the monthly average water level and precipitation anomaly occurred in the TGRA after 2011 and showed a positive correlation. Our findings revealed the change of local precipitation characteristics before and after the impoundment of TGD and showed strong evidence that this change had a close relationship with the water level.
Highlights
Before we studied the changes of precipitation, the Precipitation Concentration Degree (PCD), and the Precipitation Concentration Period (PCP) before and after the impoundment in the Three Gorges Reservoir Area (TGRA)
This study explores the possible relationship between the precipitation anomaly and monthly average water level by Cross-Wavelet Transform (CWT) analysis
After theofimpoundment spatial pattern changedin obvithe decrease precipitation of in the the Three Gorges Dam (TGD), flood the season andprecipitation the increase of precipitation dry ously, and the precipitation in the west of the with season, the proportion of precipitation in dry season in the TGRA increased, which means the of precipitation flood season theuniform
Summary
Dams provide numerous conveniences for people’s lives and production and contribute considerably to economic development [1]. In addition to their enormous societal benefits, more land is converted to surface water with the construction of a dam. This change can lead to the increased availability of local moisture and significantly affect mesoscale circulation [2,3]. The mesoscale circulation is basically a “local” ranging from 10 km to 100 km, and one of the local effects on this change can be the modification of precipitation [4]
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