Corrigendum to “Diurnal dynamics of minor and trace elements in stream water draining Dongkemadi Glacier on the Tibetan Plateau and its environmental implications” [J. Hydrol. 541 (2016) 1104–1118](S0022169416305121)(10.1016/j.jhydrol.2016.08.021)

The authors regret: At the Dongkemadi Glacier (DG) basin, daily and annual meltwater discharge at gauging section S1 should be corrected. Namely, annual discharge should be 2.74 × 10⁷ m³ throughout 1 June to 30 September of 2013. Thus, variation in solute exports is controlled by changes in discharge and specific solute concentration (Fig. 9), and the estimated solute export, cation denudation rates (CDR) and discharge-normalized CDR are 417 tons, 185 Σ^∗meq⁺m⁻² and 189 Σ^∗meq⁺m⁻³ (with annual specific discharge of 0.98 m) respectively in 2013 (Table 4). In comparison, the CDR at the DG basin is within the scope of previously published CDR (94–4200 Σ^∗meq⁺m^–2) from glacial catchments (Hodson et al., 2010). The discharge-normalized CDR is lower than the rates from most glacial catchments, but is higher than those from Mittivakkat (Greenland), S Cascade (N American) and Lewis River (Arctic) (Yde et al., 2004, 2014; Hodson et al., 2000, 2010). The authors would like to apologise for any inconvenience caused.