Response of Hydrological Drought to Meteorological Drought under the Influence of Large Reservoir

<div>Monthly correlation coefficients between SSI-1 and SPI at different time scales (from SPI-1 to SPI-12) in Shilong hydrological station; (a) the period without reservoir effect (1960–1982); (b) the period with reservoir effect (1983–2010).</div>

Advances in Meteorology

fig5

Figure 5

Figure 5: Response of Hydrological Drought to Meteorological Drought under the Influence of Large Reservoir 