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)

Xiangying Li, Xiaobo He, Shichang Kang, Sillanpää Mika, Yongjian Ding, Tianding Han, Qingbai Wu, Zhongbo Yu

Research output: Contribution to journalComment/debate

2 Citations (Scopus)

Abstract

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 Σmeq+m−2 and 189 Σmeq+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 Σmeq+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.

Original languageEnglish
Pages (from-to)995
Number of pages1
JournalJournal of Hydrology
Volume555
DOIs
Publication statusPublished - Dec 2017
Externally publishedYes

ASJC Scopus subject areas

  • Water Science and Technology

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