• Title/Summary/Keyword: discharge rating curve

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Improvement of Rating-curve by HEC-RAS (HEC-RAS를 이용한 수위-유량곡선의 개선방안)

  • Lee, Yeong Hwa;Lee, Chang Su;Park, Gi Beom
    • Journal of Environmental Science International
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    • v.13 no.9
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    • pp.759-765
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    • 2004
  • HEC-RAS model is used for estimation of rating-curve of Musung in Wi stream. Discharge is computed from stage estimated by HEC-RAS model, is compared with the discharge of water surface slope method. The relative deviation of observed and computed discharge is 5.37%, and shows as a good results. A rating-curve by HEC-RAS model shows better results than by water surface slope method.

A Study on Derivation of Rating Curve for Yangsan River (양산천 수위-유량 관계곡선의 유도에 관한 연구)

  • Lee, Y.H.;Lee, S.B.
    • Journal of Korean Port Research
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    • v.12 no.1
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    • pp.131-143
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    • 1998
  • This paper presents derivation of stage-discharge curve for Yangsan river. To derivate of stage-discharge lationship is one of the essential research areas in the water resource field. It provides reliable data a long term planning and hydrologic quantity on water resource development by quantitative analysis. The rating curve derivated through 15 discharge-observation on Yangsan river basin in 1997 has been estimated Q=1283.0262-1553.3158H+477.2702H2. According to the rating curve, the highest water level 2.6m, the limited water-level should be bound to the maximum of 2.6m. Before this research, stage-discharge curve of Yangsan river has not been developed, and only 15 discharge observation(hydrometry) has been carried out though this research. Therefore it seems necessary to collect observation data through a long term process to obtain a reliable rating curve equation.

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Analysis of Field Observations on Characteristics of Stage-Discharge Relationshiup for Yangsan River (양산천 수위-유량관계 특성에 관한 현장관측 분석)

  • 이용희;이상배
    • Journal of Korean Port Research
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    • v.14 no.1
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    • pp.107-114
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    • 2000
  • Derivation of stage-discharge relationship and characteristics for Yangsan river is presented in this paper. This research has been conducted as the second one after the first trial in 1997. The determination of discharge at a Yangsan river gauging was best made by measuring the flow velocities with a current meter and rod float. The rating curve obtained through 52 stage-discharge measurements on Yangsan river basin in 1999 is represented by Q=15.3540-140.6076H+182.44372H$^2$, which is discovered to be most excellent among other curves in reliability analysis. The observed stage-discharge data for Yangsan river was tested by HEC-RAS program, and reproduction of discharge by the induced curve was investigated and compared with the computational results. The rating curve of Yangsan river shows characteristics of Yangsan river more accurately compared with those separated in terms of water levels.

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A Study on Characteristics of Stage-discharge Relationship for Yangsan River (양산천 수위-유량관계 특성에 관한 연구)

  • 이용희;이상배
    • Proceedings of the Korean Institute of Navigation and Port Research Conference
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    • 2000.04a
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    • pp.91-98
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    • 2000
  • Derivation of stage-discharge relationship and characteristics for Yangsan river is presented in this paper. This research has been conducted as the second one after the first trial of 1997. The determination of discharge at a Yangsan river gauging was best made by measuring the flow velocities with a current meter and rod float. The rating curve obtained through 52 stage-discharge measurements on Yangsan river basin in 1999 is represented by Q=15.3540-140.6076H+182.44372$H^2$, which is discovered to be most excellent among other curves in reliability analysis. The capability of the observed stage-discharge data for Yangsan river was tested by HEC-RAS program, and its capability to reproduce discharge was investigated and compared with the computational results. Rating curve stability is determined on the basis of deviations in the stage-discharge relationship, utilization of specific gauge, and absolute differences between sequential stream flow measurements and an analysis residuals. Therefore it seems necessary to research method to obtain rating curve in a rigorous and accurate manner.

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Development of Rating Curves Using a Maximum Likelihood Model (최우도 모형을 이용한 수위-유량곡선식 개발)

  • Kim, Gyeong-Hoon;Park, Jun-Il;Shin, Chan-Ki
    • Journal of environmental and Sanitary engineering
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    • v.23 no.4
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    • pp.83-93
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    • 2008
  • The non-linear least squares model(NLSM) has long been the standard technique used by hydrologists for constructing rating curves. The reasons for its adaptation are vague, and its appropriateness as a method of describing discharge measurement uncertainty has not been well investigated. It is shown in this paper that the classical method of NLSM can model only a very limited class of variance heterogeneity. Furthermore, this lack of flexibility often leads to unaccounted heteroscedasticity, resulting in dubious values for the rating curve parameters and estimated discharge. By introducing a heteroscedastic maximum likelihood model(HMLM), the variance heterogeneity is treated more generally. The maximum likelihood model stabilises the variance better than the NLSM approach, and thus is a more robust and appropriate way to fit a rating curve to a set of discharge measurements.

Analysis of Stream Discharge Characteristic at Control Point for Runoff Model Application (유출모의를 위한 주요제어지점 유량특성 분석)

  • Lee, Sang-Jin;Lee, Bae-Sung;Ryoo, Kyong-Sik;Hwang, Man-Ha
    • Journal of Korea Water Resources Association
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    • v.39 no.11 s.172
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    • pp.905-914
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    • 2006
  • For an accurate rainfall-runoff simulation in the river basin, not evaluation of runoff model but accurate runoff data are very important. In this study, SSARR model was applied to the Geum River basin and these results are compared with runoff data observed at the Gongju gauging station. The model results didn't good fit the discharge data determined from the rating curve at Gongju gauging station during normal and dry season, especially. For the reliability analysis for the existing rating curve, we observed new stream discharge set from 2003 to 2005. We also estimated long term runoff data from the base flow separation method and defined the hydraulic characteristics. The results show that the new observed stream discharge is similar to the rainfall-runoff model results but existing rating curve seems to be overestimated about 10-20% during normal and dry season. We found that the continuous monitoring and update for the existing rating curve at the gaging station are needed for accurate estimation of runoff data.

A Basic Study of Stage-discharge Rating Stabilization at the Ssang-chi Gauging Station (쌍치 수위관측소의 수위-유량관계곡선 안정화를 위한 기초 연구)

  • Lee, Jeong-Ju;Kwon, Hyun-Han
    • KSCE Journal of Civil and Environmental Engineering Research
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    • v.30 no.1B
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    • pp.81-87
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    • 2010
  • On the SSang-chi gauging station, the discharge had been measured by the rod float method for the past twelve years. However the shifts of the rating curves are too big to be accepted. The major factors of rating curve variation were reviewed for shift analysis. To estimate the discharge measured by rod float method, two cross sections and their stages are generally required. But, the rating curves had been derived only with the observed depth of gauging station since the cross sections were not available. To correct the errors, the reference rating curve was developed. In this study, the water surface slopes of the curve were simulated by RMA2 model. The historical rating curves were re-developed by the calculated discharges on the base of the water surfaces. The results show that the range of fluctuation decreased and rating curves in recent years are physically reasonable.

Development of Looped Rating Curve at Hwawon Station (화원 수위관측소 지점의 고리모양 수위-유량 관계곡선 작성)

  • Kang Shin-Uk;Lee Sang-Ho;Hwang Man-Ha
    • Journal of Korea Water Resources Association
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    • v.39 no.6 s.167
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    • pp.487-494
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    • 2006
  • The flood discharge on the rising limb of a hydrograph at Hwawon station greatly differs from the flood discharge on the falling limb for the same stage. When there is such a big hysteresis, there can be a significant amount of errors in the rated discharge obtained from a simple rating curve. To reduce errors in rated discharges, a looped rating curve was established for Hwawon station in the Nakdong River. In order to compute the deviation between real discharges and simply rated discharges, a simple rating curve was established using the stage and discharge data from the results of a hydraulic channel routing. The relationship between the discharge deviation ${\Delta}Q$ and a product of B and ${\Delta}h/{\Delta}t$ was analysed, where B is the channel topwidth; ${\Delta}h$ is the stage increment; At is the time increment. Strong relation between ${\Delta}Q$ and $B{\Delta}h/{\Delta}t$ was found. The discharges calculated from the relationship show differences by 10 % or less for the 7 observations out of 11 observations in 1997 whose stages exceeds 7 m. The observed discharges for the stages over 9 m in 1998 also show small difference with the discharges estimated from the loop rating curve. Looped rating curve is recommended, instead of the simple rating curve to reduce the errors of rated discharges for gauging stations like Hwawon, which has relatively large loop width.

Estimating the rating curve of irrigation canals in the Cheongju Sindae area

  • Mikyoung Choi;Inhyeok Song;Heesung Lim;Hansol Kang;Hyunuk An
    • Korean Journal of Agricultural Science
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    • v.51 no.1
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    • pp.79-86
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    • 2024
  • As the frequency and intensity of heavy rains increase, the vulnerability of agriculture to disasters also increases. Consequently, there is a need to improve flood and inundation predictions. To enhance the accuracy of inundation predictions, it is essential to monitor water level and discharge data within agricultural areas. This study was conducted to monitor water levels and rainfall in the Cheongju Sindae area from 2022 to 2023, and the data was utilized as input and validation data for agricultural inundation modeling. Four irrigation drainage canals were installed to a square-shaped concrete structure where the water level gauge is. It was then confirmed that the water level rises with rainfall. The flow velocities were monitored during periods of heavy rainfall. The rating curve, which estimates water level and flow velocity based on observations, was estimated using the software K-HQ. The resulting curve was presented with the Coefficient of Determination (R2). K-HQ was also used to calculate the equation for the rating curve, taking outliers into account at each data point. Outliers were extracted and the rating curve was recalculated. As the coefficient of determination of three out of four stations exceeded 0.95, the estimated rating curve may be considered reliable for discharge estimation. This study provides critical data for enhancing agricultural inundation modeling accuracy and drainage improvement projects.

Improvement of Low Water Level Rating Curve in Tidal River Taehwa (태화강 갑조부의 저수위 수위-유량곡선 개선)

  • Jo, Hong-Je;Hwang, Jae-Ho;Mun, Seong-Jun
    • Journal of Korea Water Resources Association
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    • v.33 no.5
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    • pp.635-645
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    • 2000
  • In tidal rivers, the river level, discharge and tide are interrelated. Therefore, the stage-discharge relation that takes no account of tidal effects is inaccurate. For the calculation of river discharge in low water level, this paper attempts to formulate a multiple regression equation of stage-discharge curve to calculate the river discharge in low water level with variables as river level and differences between sea level and river level. Numerical application were perfonned on Ulsan gaging station in Taehwa river, and the comparison with existing rating curve equation showed good applicability of this multiple regression equation.uation.

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