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Pradhananga, N.S., Kayastha, R.B., Bhattarai, B.C., Adhikari, T.R., Pradhan, S.C., Devkota, L.P., Shrestha, A.B. and Mool, P.K. (2014) Estimation of Discharge from Langtang River Basin, Rasuwa, Nepal, Using a Glacio-Hydrological Model. Annals of Glaciology, 55, 223-230.
http://dx.doi.org/10.3189/2014AoG66A123

has been cited by the following article:

• TITLE: Assessment of Sediment Load of Langtang River in Rasuwa District, Nepal

  AUTHORS: Aastha Chhetri, Rijan B. Kayastha, Ahuti Shrestha

  KEYWORDS: Sediment Load, SSC, Discharge, Depth Integration Technique, Langtang River

  JOURNAL NAME: Journal of Water Resource and Protection, Vol.8 No.1, January 25, 2016

  ABSTRACT: This paper assesses the sediment load of the glacier fed Langtang River, Nepal from April 2014 to March 2015. Water samples were collected from the centre of the river with a frequency of two samples per each sampling day using the Depth Integration Technique (DIT) on daily basis in the monsoon season, weekly in the pre- and post-monsoon seasons and bi-monthly in the winter season. Suspended sediment concentration (SSC) is calculated from the water samples using filtration followed by oven-drying, and a rating curve is used to calculate daily discharge of the Langtang River. The annual sediment yield is 109,276.75 tons and 37.69, 11.52 and 5.54 tons of sediment is transported per day in the pre-monsoon, post-monsoon and winter seasons, respectively. There is a very high value of 872.86 tons per day in the monsoon season, which contributes the highest sediment load among all of the seasons comprising 83% of the total sediment transport. Diurnal cycle of sediment discharge is clearly seen with higher sediment discharge during the evening than the morning and reaching maximum values of 41.1 kg·s-1 and 61.5 kg·s-1, respectively. A clock-wise hysteresis loop has been obtained for discharge and sediment discharge where sediment flux is higher in the early monsoon than in the late monsoon for a corresponding discharge.