Integrated river flow modelling: A case study

2012 ◽  
Vol 9 (4) ◽  
pp. 259-276 ◽  
Author(s):  
N.T. Lan-Anh ◽  
J. Boxall ◽  
A. Saul ◽  
P. Willems
Keyword(s):  
2017 ◽  
Vol 11 ◽  
pp. S902-S915 ◽  
Author(s):  
A. Quintela-del-Río ◽  
M. Francisco-Fernández

1999 ◽  
Vol 10 (2) ◽  
pp. 402-409 ◽  
Author(s):  
A.F. Atiya ◽  
S.M. El-Shoura ◽  
S.I. Shaheen ◽  
M.S. El-Sherif

Author(s):  
Adam Łajczak

Abstract Changes in flood risk impacted by river training - case study of piedmont section of the Vistula river. Main problems concerning the flood risk in piedmont section of the Vistula, Southern Poland, are discussed. This stretch of the river is channelized since the middle of the 19th century. It is part of the mainstream discussion of the effectiveness of existing river channelization methods. The following problems are analysed: (1) current state of flood risk, (2) the rate of river flow, (3) changes in flood risk since the start of channelization efforts with respect to changing channel geometry and changing rates of river flow reflecting the effects of channelization work. Substantially increased bankfull discharge in a channelized river may be considered as a stable hydrologic feature of the river stretch analysed. This means that the river is effectively reducing the quantity of water available for flooding the inter-embankment zone. This statement is the basis for analysis of changes in flood risk in the river studied. An assessment of changes in flood risk for the piedmont section of the Vistula cannot be categorical. Some changes in discharge help reduce flood risk, while others increase it. The paper is based mainly on the State Hydrological Survey data over more than the last 100 years, a large-scale maps over the last 230 years, and fieldwork conducted by the author.


2018 ◽  
Vol 7 (1) ◽  
pp. 22 ◽  
Author(s):  
Petrus Subardjo ◽  
Agus Anugroho Dwi Suryo ◽  
Ibnu Pratikno ◽  
Gentur Handoyo ◽  
Karlina Putri Diani

Muara Sungai Sambas merupakan gerbang bagi kapal-kapal yang akan melakukan aktivitas bongkar muat hasil tangkapan ikan di PPN Pemangkat. Besarnya konsentrasi material padatan tersuspensi berkaitan dengan tingkat sedimentasi di muara Sungai Sambas yang dapat menyebabkan pendangkalan sehingga aliran sungai ke laut terhambat dan alur pelayaran terganggu. Tujuan penelitian ini adalah untuk mengetahui konsentrasi dan pola sebaran material padatan tersuspensi di muara Sungai Sambas Provinsi Kalimantan Barat. Metode yang digunakan dalam penelitian ini adalah metode studi kasus. Analisis material padatan tersuspensi menggunakan metode Gravimetri. Data utama yang digunakan dalam penelitian ini meliputi data material padatan tersuspensi, arus,  dan pasang surut serta data pendukung berupa peta batimetri, dan peta RBI. Hasil penelitian menunjukkan bahwa konsentrasi material padatan tersuspensi terbesar berada di muara sungai dan semakin mengecil kearah laut lepas dengan konsentrasi material padatan tersuspensi saat pasang berkisar antara 67-600 mg/l serta konsentrasi material padatan tersuspensi saat surut berkisar antara 11-321 mg/l. Jenis arus yang mendominasi di muara Sungai Sambas adalah arus pasang surut. Tipe pasang surut yaitu campuran condong ke harian ganda. Kurangnya informasi mengenai arah pergerakan dan besaran konsentrasi material padatan tersuspensi di muara Sungai Sambas menjadikan penelitian untuk mengetahui konsentrasi dan pola sebaran material padatan tersuspensi di perairan tersebut diperlukan. Sambas Estuaries is the entrance for every fisherman boats which will do loading and unloading activity for their fishing at PPN Pemangkat. The amount of total suspended matter concentration is related to the sedimentation at the Sambas estuaries which can cause sedimentation so the river flow hampered and the shipping line disrupted. The purpose of this research is to know the concentration and the distribution of total suspended solid at Sambas Estuaries, West Kalimantan. The method which is used in this research is case study method. Data processing is using gravimetric analysis. The main data used in this research are data of total suspended solid, current, tidal and supporting data such as bathymetri map, RBI map. Based on data processing, known that the highest value of total suspended solid was at estuary and decreased toward the sea with the conscentration at tides ranged between 67-600 mg/l whereas concentration at low tide ranged between 11-321 mg/l. The type tidal which is belong mixed dominant semidiurnal type. Lack of information on the direction of movement and the concentration of total suspended solid at Sambas Estuaries makes research to find out the concentration and distribution of total suspended solid is held at the waters. 


Water ◽  
2020 ◽  
Vol 12 (11) ◽  
pp. 3049
Author(s):  
Chiara Belvederesi ◽  
John Albino Dominic ◽  
Quazi K. Hassan ◽  
Anil Gupta ◽  
Gopal Achari

Catchments located in cold weather regions are highly influenced by the natural seasonality that dictates all hydrological processes. This represents a challenge in the development of river flow forecasting models, which often require complex software that use multiple explanatory variables and a large amount of data to forecast such seasonality. The Athabasca River Basin (ARB) in Alberta, Canada, receives no or very little rainfall and snowmelt during the winter and an abundant rainfall–runoff and snowmelt during the spring/summer. Using the ARB as a case study, this paper proposes a novel simplistic method for short-term (i.e., 6 days) river flow forecasting in cold regions and compares existing hydrological modelling techniques to demonstrate that it is possible to achieve a good level of accuracy using simple modelling. In particular, the performance of a regression model (RM), base difference model (BDM), and the newly developed flow difference model (FDM) were evaluated and compared. The results showed that the FDM could accurately forecast river flow (ENS = 0.95) using limited data inputs and calibration parameters. Moreover, the newly proposed FDM had similar performance to artificial intelligence (AI) techniques, demonstrating the capability of simplistic methods to forecast river flow while bypassing the fundamental processes that govern the natural annual river cycle.


2016 ◽  
Vol 17 (7) ◽  
pp. 2013-2039 ◽  
Author(s):  
Bruce Davison ◽  
Alain Pietroniro ◽  
Vincent Fortin ◽  
Robert Leconte ◽  
Moges Mamo ◽  
...  

Abstract Land surface schemes (LSSs) are of potential interest both to hydrologists looking for innovative ways to simulate river flow and the land surface water balance and to atmospheric scientists looking to improve weather and climate predictions. This paper discusses three ideas, which are grounded in hydrological science, to improve LSS predictions of streamflow and latent heat fluxes. These three possibilities are 1) improved representation of lateral flow processes, 2) the appropriate representation of surface heterogeneity, and 3) calibration to streamflow as a way to account for parameter uncertainty. The current understanding of lateral hydrological processes is described along with their representation of a selected group of LSSs. Issues around spatial heterogeneity are discussed, and calibration in hydrologic models and LSSs is examined. A case study of an evapotranspiration-dominated basin with over 10 years of extensive observations in central Canada is presented. The results indicate that in this particular basin, calibration of streamflow presents atmospheric modelers with a unique opportunity to improve upon the current practice of using lookup tables to define parameter values. More studies are needed to determine if model calibration to streamflow is an appropriate method for generally improving LSS-modeled heat fluxes around the globe.


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