Articles | Volume 19, issue 3
https://doi.org/10.5194/os-19-603-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-19-603-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Extension of the general unit hydrograph theory for the spread of salinity in estuaries
Huayang Cai
Institute of Estuarine and Coastal Research/State and Local Joint
Engineering Laboratory of Estuarine Hydraulic Technology, School of Ocean
Engineering and Technology, Sun Yat-sen University, Guangzhou, 510275, China
Guangdong Provincial Engineering Research Center of Coasts, Islands
and Reefs/Southern Marine Science and Engineering Guangdong Laboratory
(Zhuhai), Zhuhai, 519082, China
Guangdong Provincial Key Laboratory of Marine Resources and Coastal
Engineering, Zhuhai, 519082, China
Bo Li
Institute of Estuarine and Coastal Research/State and Local Joint
Engineering Laboratory of Estuarine Hydraulic Technology, School of Ocean
Engineering and Technology, Sun Yat-sen University, Guangzhou, 510275, China
Guangdong Provincial Engineering Research Center of Coasts, Islands
and Reefs/Southern Marine Science and Engineering Guangdong Laboratory
(Zhuhai), Zhuhai, 519082, China
Guangdong Provincial Key Laboratory of Marine Resources and Coastal
Engineering, Zhuhai, 519082, China
Junhao Gu
Institute of Estuarine and Coastal Research/State and Local Joint
Engineering Laboratory of Estuarine Hydraulic Technology, School of Ocean
Engineering and Technology, Sun Yat-sen University, Guangzhou, 510275, China
Guangdong Provincial Engineering Research Center of Coasts, Islands
and Reefs/Southern Marine Science and Engineering Guangdong Laboratory
(Zhuhai), Zhuhai, 519082, China
Guangdong Provincial Key Laboratory of Marine Resources and Coastal
Engineering, Zhuhai, 519082, China
Tongtiegang Zhao
School of Civil Engineering, Sun Yat-sen University, Zhuhai, 519082,
China
Centre for Marine and Environmental Research (CIMA), University of
Algarve, Faro, Portugal
Related authors
Huayang Cai, Hao Yang, Pascal Matte, Haidong Pan, Zhan Hu, Tongtiegang Zhao, and Guangliang Liu
Ocean Sci., 18, 1691–1702, https://doi.org/10.5194/os-18-1691-2022, https://doi.org/10.5194/os-18-1691-2022, 2022
Short summary
Short summary
Quantifying spatial–temporal water level dynamics is essential for water resources management in estuaries. In this study, we propose a simple yet powerful regression model to examine the influence of the world’s largest dam, the Three Gorges Dam (TGD), on the spatial–temporal water level dynamics within the Yangtze River estuary. The presented method is particularly useful for determining scientific strategies for sustainable water resources management in dam-controlled estuaries worldwide.
Tongtiegang Zhao, Haoling Chen, Yu Tian, Denghua Yan, Weixin Xu, Huayang Cai, Jiabiao Wang, and Xiaohong Chen
Hydrol. Earth Syst. Sci., 26, 4233–4249, https://doi.org/10.5194/hess-26-4233-2022, https://doi.org/10.5194/hess-26-4233-2022, 2022
Short summary
Short summary
This paper develops a novel set operations of coefficients of determination (SOCD) method to explicitly quantify the overlapping and differing information for GCM forecasts and ENSO teleconnection. Specifically, the intersection operation of the coefficient of determination derives the overlapping information for GCM forecasts and the Niño3.4 index, and then the difference operation determines the differing information in GCM forecasts (Niño3.4 index) from the Niño3.4 index (GCM forecasts).
Erwan Garel, Ping Zhang, and Huayang Cai
Ocean Sci., 17, 1605–1621, https://doi.org/10.5194/os-17-1605-2021, https://doi.org/10.5194/os-17-1605-2021, 2021
Short summary
Short summary
Understanding tidal hydrodynamics is essential for water resources management in estuarine environments. In this study, we propose an analytical model to examine the fortnightly water level variations due to tidal motions alone in tide-dominated estuaries. Details of the analytical model show that changes in the mean depth or length of semi-arid estuaries affect the fortnightly tide amplitude, which has significant potential impacts on the estuarine ecosystem management.
Leicheng Guo, Chunyan Zhu, Huayang Cai, Zheng Bing Wang, Ian Townend, and Qing He
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2021-75, https://doi.org/10.5194/hess-2021-75, 2021
Revised manuscript not accepted
Short summary
Short summary
Overtide is a shallow water tidal component and its interaction with astronomical tides induces tidal wave deformation, which is an important process that controls sediment transport. We use a numerical tidal model to examine overtide changes in estuaries under varying river discharges and find spatially nonlinear changes and the threshold of an intermediate river that benefits maximal overtide generation. The findings inform management of sediment transport and flooding risk in estuaries.
Tian Lan, Kairong Lin, Chong-Yu Xu, Zhiyong Liu, and Huayang Cai
Hydrol. Earth Syst. Sci., 24, 5859–5874, https://doi.org/10.5194/hess-24-5859-2020, https://doi.org/10.5194/hess-24-5859-2020, 2020
Tongtiegang Zhao, Qiang Li, Tongbi Tu, and Xiaohong Chen
Geosci. Model Dev., 18, 5781–5799, https://doi.org/10.5194/gmd-18-5781-2025, https://doi.org/10.5194/gmd-18-5781-2025, 2025
Short summary
Short summary
The recent WeatherBench 2 provides a versatile framework for the verification of deterministic and ensemble forecasts. In this paper, we present an explicit extension to binary forecasts of hydroclimatic extremes. Seventeen verification metrics for binary forecasts are employed, and scorecards are generated to showcase the predictive performance. The extension facilitates more comprehensive comparisons of hydroclimatic forecasts and provides useful information for forecast applications.
Tongtiegang Zhao, Zecong Chen, Yongyong Zhang, Bingyao Zhang, and Yu Li
Hydrol. Earth Syst. Sci., 29, 2429–2443, https://doi.org/10.5194/hess-29-2429-2025, https://doi.org/10.5194/hess-29-2429-2025, 2025
Short summary
Short summary
The classic logistic function characterizes the stationary relationship between drought loss and intensity. This paper accounts for time in the magnitude, shape and location parameters of the logistic function and derives nonstationary intensity loss functions. A case study is designed to test the functions for drought-affected populations by province in mainland China from 2006 to 2023. Overall, the nonstationary intensity loss functions are shown to be a useful tool for drought management.
Tongtiegang Zhao, Zexin Chen, Yu Tian, Bingyao Zhang, Yu Li, and Xiaohong Chen
Hydrol. Earth Syst. Sci., 28, 3597–3611, https://doi.org/10.5194/hess-28-3597-2024, https://doi.org/10.5194/hess-28-3597-2024, 2024
Short summary
Short summary
The local performance plays a critical part in practical applications of global streamflow reanalysis. This paper develops a decomposition approach to evaluating streamflow analysis at different timescales. The reanalysis is observed to be more effective in characterizing seasonal, annual and multi-annual features than daily, weekly and monthly features. Also, the local performance is shown to be primarily influenced by precipitation seasonality, longitude, mean precipitation and mean slope.
Qiang Li and Tongtiegang Zhao
EGUsphere, https://doi.org/10.5194/egusphere-2024-1449, https://doi.org/10.5194/egusphere-2024-1449, 2024
Preprint withdrawn
Short summary
Short summary
This paper focuses on the effect of the water balance constraint on the robustness of the long short-term memory (LSTM) network in learning rainfall-runoff relationships. Through large-sample tests, it is found that incorporating this constraint into the LSTM improves the robustness, while the improvement tends to decrease as the amount of training data increases. The results point to the compensation effects between training data and process knowledge on the LSTM’s performance.
Qiang Li and Tongtiegang Zhao
EGUsphere, https://doi.org/10.5194/egusphere-2023-2841, https://doi.org/10.5194/egusphere-2023-2841, 2024
Preprint archived
Short summary
Short summary
The lack of physical mechanism is a critical issue for the use of popular deep learning models. This paper presents an in-depth investigation of the fundamental mass balance constraint for deep learning-based rainfall-runoff prediction. The robustness against data sparsity, random parameters initialization and contrasting climate conditions are detailed. The results highlight that the water balance constraint evidently improves the robustness in particular when there is limited training data.
Huayang Cai, Hao Yang, Pascal Matte, Haidong Pan, Zhan Hu, Tongtiegang Zhao, and Guangliang Liu
Ocean Sci., 18, 1691–1702, https://doi.org/10.5194/os-18-1691-2022, https://doi.org/10.5194/os-18-1691-2022, 2022
Short summary
Short summary
Quantifying spatial–temporal water level dynamics is essential for water resources management in estuaries. In this study, we propose a simple yet powerful regression model to examine the influence of the world’s largest dam, the Three Gorges Dam (TGD), on the spatial–temporal water level dynamics within the Yangtze River estuary. The presented method is particularly useful for determining scientific strategies for sustainable water resources management in dam-controlled estuaries worldwide.
Tongtiegang Zhao, Haoling Chen, Yu Tian, Denghua Yan, Weixin Xu, Huayang Cai, Jiabiao Wang, and Xiaohong Chen
Hydrol. Earth Syst. Sci., 26, 4233–4249, https://doi.org/10.5194/hess-26-4233-2022, https://doi.org/10.5194/hess-26-4233-2022, 2022
Short summary
Short summary
This paper develops a novel set operations of coefficients of determination (SOCD) method to explicitly quantify the overlapping and differing information for GCM forecasts and ENSO teleconnection. Specifically, the intersection operation of the coefficient of determination derives the overlapping information for GCM forecasts and the Niño3.4 index, and then the difference operation determines the differing information in GCM forecasts (Niño3.4 index) from the Niño3.4 index (GCM forecasts).
Luciano de Oliveira Júnior, Paulo Relvas, and Erwan Garel
Ocean Sci., 18, 1183–1202, https://doi.org/10.5194/os-18-1183-2022, https://doi.org/10.5194/os-18-1183-2022, 2022
Short summary
Short summary
The circulation patterns of surface water over the northern Gulf of Cádiz are described based on hourly high-frequency radar data from 2016 to 2020. A persistent current follows the continental shelf slope eastward while near the coast, and currents generally have a balanced (eastward–westward) direction. In summer cross-shelf transport is promoted when westward coastal countercurrents recirculate offshore in the western region and merge with the slope current.
Erwan Garel, Ping Zhang, and Huayang Cai
Ocean Sci., 17, 1605–1621, https://doi.org/10.5194/os-17-1605-2021, https://doi.org/10.5194/os-17-1605-2021, 2021
Short summary
Short summary
Understanding tidal hydrodynamics is essential for water resources management in estuarine environments. In this study, we propose an analytical model to examine the fortnightly water level variations due to tidal motions alone in tide-dominated estuaries. Details of the analytical model show that changes in the mean depth or length of semi-arid estuaries affect the fortnightly tide amplitude, which has significant potential impacts on the estuarine ecosystem management.
Tongtiegang Zhao, Haoling Chen, Quanxi Shao, Tongbi Tu, Yu Tian, and Xiaohong Chen
Hydrol. Earth Syst. Sci., 25, 5717–5732, https://doi.org/10.5194/hess-25-5717-2021, https://doi.org/10.5194/hess-25-5717-2021, 2021
Short summary
Short summary
This paper develops a novel approach to attributing correlation skill of dynamical GCM forecasts to statistical El Niño–Southern Oscillation (ENSO) teleconnection using the coefficient of determination. Three cases of attribution are effectively facilitated, which are significantly positive anomaly correlation attributable to positive ENSO teleconnection, attributable to negative ENSO teleconnection and not attributable to ENSO teleconnection.
Leicheng Guo, Chunyan Zhu, Huayang Cai, Zheng Bing Wang, Ian Townend, and Qing He
Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2021-75, https://doi.org/10.5194/hess-2021-75, 2021
Revised manuscript not accepted
Short summary
Short summary
Overtide is a shallow water tidal component and its interaction with astronomical tides induces tidal wave deformation, which is an important process that controls sediment transport. We use a numerical tidal model to examine overtide changes in estuaries under varying river discharges and find spatially nonlinear changes and the threshold of an intermediate river that benefits maximal overtide generation. The findings inform management of sediment transport and flooding risk in estuaries.
Tian Lan, Kairong Lin, Chong-Yu Xu, Zhiyong Liu, and Huayang Cai
Hydrol. Earth Syst. Sci., 24, 5859–5874, https://doi.org/10.5194/hess-24-5859-2020, https://doi.org/10.5194/hess-24-5859-2020, 2020
Cited articles
Cai, H., Savenije, H. H. G., Zuo, S., Jiang, C., and Chua, V.: A predictive
model for salt intrusion in estuaries applied to the Yangtze estuary, J.
Hydrol., 529, 1336–1349,
https://doi.org/10.1016/j.jhydrol.2015.08.050, 2015.
Chow, V. T., Maidment, D., and Mays, L. W.: Applied hydrology, New York,
McGraw-Hill, ISBN 0-07-100174-3, 1988.
Dijkstra, Y. M. and Schuttelaars, H. M.: A unifying approach to subtidal
salt intrusion modeling in tidal estuaries, J. Phys. Oceanogr., 51,
147–167, https://doi.org/10.1175/jpo-d-20-0006.1, 2021.
Gay, P. and O'Donnell, J.: Comparison of the salinity structure of the
Chesapeake Bay, the Delaware Bay and Long Island Sound using a linearly
tapered advection-dispersion model, Estuar. Coast., 32, 68–87,
https://doi.org/10.1007/s12237-008-9101-4, 2009.
Gay, P. S. and O'Donnell, J.: A simple advection-dispersion model for the
salt distribution in linearly tapered estuaries, J. Geophys. Res.-Oceans,
112, C070201, https://doi.org/10.1029/2006JC003840, 2007.
Guo, J.: General and analytic unit hydrograph and its applications, J.
Hydrol. Eng., 27, 04021046,
https://doi.org/10.1061/(ASCE)HE.1943-5584.0002149, 2022a.
Guo, J.: General unit hydrograph from Chow's linear theory of hydrologic
systems and its applications, J. Hydrol. Eng., 27, 04022020,
https://doi.org/10.1061/(ASCE)HE.1943-5584.0002184, 2022b.
Guo, J.: Application of general unit hydrograph model for baseflow
separation from rainfall and streamflow data, J. Hydrol. Eng., 27,
04022027, https://doi.org/10.1061/(ASCE)HE.1943-5584.0002217,
2022c.
Kuijper, K. and Van Rijn, L. C.: Analytical and numerical analysis of tides
and salinities in estuaries; part II: salinity distributions in prismatic
and convergent tidal channels, Ocean Dynam., 61, 1743–1765,
https://doi.org/10.1007/s10236-011-0454-z, 2011.
Lewis, R. E. and Uncles, R. J.: Factors affecting longitudinal dispersion in
estuaries of different scale, Ocean Dynam., 53, 197–207,
https://doi.org/10.1007/s10236-003-0030-2, 2003.
Nash, J. E.: The form of instantaneous unit hydrograph, Int. Assoc. Sci.
Hydrol. Publ., 45, 114–121, 1957.
Pein, J., Valle-Levinson, A., and Stanev, E. V.: Secondary circulation
asymmetry in a meandering, partially stratified estuary, J. Geophys.
Res.-Oceans, 123, 1670–1683,
https://doi.org/10.1002/2016JC012623, 2018.
Prandle, D.: Salinity intrusion in estuaries, J. Phys. Oceanogr., 11,
1311–1324, https://doi.org/10.1175/1520-0485(1981)011<1311:SIIE>2.0.CO;2, 1981.
Savenije, H. H. G.: A one-dimensional model for salinity intrusion in alluvial
estuaries, J. Hydrol., 85, 87–109,
https://doi.org/10.1016/0022-1694(86)90078-8, 1986.
Savenije, H. H. G.: Salt intrusion model for high-water slack, low-water
slack, and mean tide on spread sheet, J. Hydrol., 107, 9–18,
https://doi.org/10.1016/0022-1694(89)90046-2, 1989.
Savenije, H. H. G.: Predictive model for salt intrusion in estuaries, J.
Hydrol., 148, 203–218,
https://doi.org/10.1016/0022-1694(89)90046-2, 1993.
Savenije, H. H. G.: Salinity and tides in alluvial estuaries, New York,
Elsevier, https://doi.org/10.1016/B978-0-444-52107-1.X5000-X,
2005.
Savenije, H. H. G.: Salinity and tides in alluvial estuaries, completely
revised 2nd edition, http://www.salinityandtides.com
(last access: 22 March 2022), 2012.
Savenije, J. H.: Data_SalinityandTides, WordPress [data set], https://salinityandtides.com/data-sources/ (last access: 3 May 2023), 2012.
Van der Burgh, P.: Ontwikkeling van een methode voor het voorspellen van
zoutverdelingen in estuaria, kanalen en zeeen, Den Haag, Rijkwaterstaat
Rapport, 10–72, 1972 (in Dutch).
Wei, X., Williams, M. E., Brown, J. M., Thorne, P. D., and Amoudry, L. O.:
Salt intrusion as a function of estuary length in periodically weakly
stratified estuaries, Geophys. Res. Lett., 49, e2022GL099082, https://doi.org/10.1029/2022GL099082, 2022.
Zhang, Z. and Savenije, H. H. G.: The physics behind Van der Burgh's empirical equation, providing a new predictive equation for salinity intrusion in estuaries, Hydrol. Earth Syst. Sci., 21, 3287–3305, https://doi.org/10.5194/hess-21-3287-2017, 2017.
Zhang, Z. and Savenije, H. H. G.: Thermodynamics of saline and fresh water mixing in estuaries, Earth Syst. Dynam., 9, 241–247, https://doi.org/10.5194/esd-9-241-2018, 2018.
Short summary
For many problems concerning water resource utilization in estuaries, it is essential to be able to express observed salinity distributions based on simple theoretical models. In this study, we propose an analytical salt intrusion model inspired from a theory for predictions of flood hydrographs in watersheds. The newly developed model can be well calibrated using a minimum of three salinity measurements along the estuary and has been successfully applied in 21 estuaries worldwide.
For many problems concerning water resource utilization in estuaries, it is essential to be able...