Multi-scale streamflow variability responses to precipitation over the headwater catchments in southern China

• Published in: Journal of hydrology (Amsterdam) Vol. 551; pp. 14 - 28
• Main Authors: Niu, Jun, Chen, Ji, Wang, Keyi, Sivakumar, Bellie
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.08.2017
• Subjects: Coherent mode; Haar wavelet; Principal component analysis; South China; Streamflow variability; VIC model; Coherent mode; VIC model; Streamflow variability; South China; Haar wavelet; Principal component analysis
• ISSN: 0022-1694; 1879-2707
• DOI: 10.1016/j.jhydrol.2017.05.052

•Coherent modes of multi-scale streamflow variability in 16 catchments are examined.•Daily streamflow time series are simulated by the VIC model and a routing scheme.•Three modes of multi-scale streamflow variability explain almost 95% of variability.•High variability at distinct scales is associated with tendency of flood or drought. This paper examines the multi-scale streamflow variability responses to precipitation over 16 headwater catchments in the Pearl River basin, South China. The long-term daily streamflow data (1952–2000), obtained using a macro-scale hydrological model, the Variable Infiltration Capacity (VIC) model, and a routing scheme, are studied. Temporal features of streamflow variability at 10 different timescales, ranging from 6days to 8.4years, are revealed with the Haar wavelet transform. The principal component analysis (PCA) is performed to categorize the headwater catchments with the coherent modes of multi-scale wavelet spectra. The results indicate that three distinct modes, with different variability distributions at small timescales and seasonal scales, can explain 95% of the streamflow variability. A large majority of the catchments (i.e. 12 out of 16) exhibit consistent mode feature on multi-scale variability throughout three sub-periods (1952–1968, 1969–1984, and 1985–2000). The multi-scale streamflow variability responses to precipitation are identified to be associated with the regional flood and drought tendency over the headwater catchments in southern China.