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Teleconnection analysis of runoff and soil moisture over the Pearl River basin in southern China

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Academic year: 2020

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Figure

Fig. 1. The Pearl River basin in southern China, gauge stations, and 10 sub-basins (after Niu, 2013).Fig
Table 1. Runoff simulation results at a monthly time step for 10 gauging stations over the Pearl River basin (in Fig
Table 2. Statistical properties of the observed precipitation and the simulated monthly time series (1952–2000) of 10 sub-basins over thePearl River basin.∗
Fig. 2. (a) wavelet, normalized by 1/ (i) Monthly runoff anomaly time series at Boluo station in the East River and (ii) its local wavelet power spectrum using the Morlet 2 ( 2 = 3668.94 mm2)
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