Abstract

Suspended sediment rating-curves are low cost and reliable tools used all around the world to estimate river suspended sediment concentrations (SSC) based on either linear or non-linear regression with a second variable, such as the river discharge. The aim of this paper is to undertake an evaluation of four different suspended sediment rating-curves for three turbid large river tributaries flowing into the largest choked coastal lagoon of the world, a very turbid system. Statistical parameters such as Nash–Sutcliffe efficiency coefficient (NSE), percent of bias (PBIAS) and a standardized root-mean-square error (RMSE), referred to as RSR (RMSE-observations standard deviation ratio) were used to calibrate and validate the suspended sediment rating-curves. Results indicated that for all tributaries, the non-linear approach yielded the best correlations and proved to be an effective tool to estimate the SSC from river flow data. The tested curves show low bias and high accuracy for monthly resolution. However, for higher temporal resolution, and therefore variability, an ad hoc data acquisition to capture extreme rating-curve values is required to reliably fill gaps of information for both performing modeling approaches and setting monitoring efforts for long-term variability studies.

Highlights

  • The coastal export of fine terrigenous continental material from turbid to marine systems consists of a source-to-sink process, which includes erosion and resuspension mechanisms within watersheds, fluvial transport and discharge throughout river-estuaries, and deposition on the inner continental shelf [1]

  • São Goncalo Channel (SGC) is not characterized as a hydraulic channel, its discharge is governed by wind and water level difference between Mirim

  • The SGC discharge data used for the rating-curves approach were obtained through a slope-type analytical model proposed by [41] using wind and water level time series

Read more

Summary

Introduction

The coastal export of fine terrigenous continental material from turbid to marine systems consists of a source-to-sink process, which includes erosion and resuspension mechanisms within watersheds, fluvial transport and discharge throughout river-estuaries, and deposition on the inner continental shelf [1]. Such a process depends on geological, geomorphological, sedimentological, and oceanographic features of the region, but its original magnitude is modulated by rainfall, wind and geological attributes such as catchment grain size composition [1,2]. One of the main shortcomings in studying the riverine capacity/load of suspended sediment transport is the lack of long-term series of suspended sediment concentrations (SSC) due to the difficulties in installing and maintaining continuous monitoring

Objectives
Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call