Investigation of relationship between base flow index and flow duration curve indices at national scale in Iran

Document Type : Complete scientific research article

Authors

1 1Assistant Prof., Soil Conservation and Watershed Management Research Institute, Agricultural Research, Education and Extension Organization, Tehran, Iran

2 Prof., Soil Conservation and Watershed Management Research Institute, Agricultural Research, Education and Extension Organization, Tehran, Iran

Abstract

Investigation of relationship between base flow index and flow duration curve indices at national scale in Iran

Rahim Kazemi1 *Jahangir porhemmat2, Forood Sharifi3
1Assistant Prof., Soil Conservation and Watershed Management Research Institute, Agricultural Research, Education and Extension Organization, Tehran, Iran
2,3 Prof., Soil Conservation and Watershed Management Research Institute, Agricultural Research, Education and Extension Organization, Tehran, Iran

Abstract:

Background and Objectives: Recognizing and understanding the relationship between the different components of the catchments can help improvement and development of predictions in ungagged catchments. The true value of the base flow is unclear, and since the flow duration curve (FDC) is generated using observational data, therefore recognizing and analyzing the relationships between FDC and the base flow index (BFI) leads to achieving information for optimal use of FDC indices as the estimating parameter of BFI. The purpose of this study is to investigate and identify the relationship between BFI and FDC indices in catchments of different climates of Iran.

Materials and Methods: First, by preparing the climate map of the country and its intersection with the border of the 4th order of watersheds, the catchments located in each climatic zone were separated. Then, at least 30 stations with appropriate statistics and the common period of 1976-2011 were selected in each climatic zone. The FDC was prepared using long-term daily stream flow data, and indices of, Q2, Q5, Q10, Q15, Q20, Q50, Q75, Q90, extracted. The index of the last inflection point of FDC at the zero slope of FDC was extracted using coding in MATLAB. Then BFI was calculated using one parameter recursive digital filtering algorithm and using long-term daily stream flow data. Finally, regression relationships between the average annual FDC indices and BFI in different climatic zones were computed and analyzed.

Results: The results showed that the highest correlation between FDC and BFI in catchments of very humid region with a coefficient of determination of 0.84 was related to first part of FDC, but in both humid and semi-humid regions, the highest correlation were related to the last part of FDC with 0.63 and 0.69 coefficient of determination. The highest coefficient of determination (0.85) between FDC index at the zero slope point (QFinal) and the BFI were related to the catchments of very humid region. Correlation between end-of of FDC indices with BFI in catchments of humid, semi-humid, Mediterranean and semi-arid climate zones were strong relation and could be recommended for regional analysis, forecasting and estimation purposes in ungauged catchment. However, in the catchments of the arid region, this relationship was exceptional, and indices of first part of FDC play this role. In very humid region, the coefficient of determination of FDC indices with BFI was reliable and usable.

Conclusion: In overall conclusion, it is noteworthy that the correlation between the endpoint FDC indices with the average annual BFI in the humid, semi-humid, Mediterranean and semi-arid climate zones were strong, reliable and recommended for regional analysis, forecasting and estimation in ungagged catchments. However, in the catchments of the arid region, this relationship was exceptional, and first part of FDC indices play this role, and have the highest correlation. In catchments located in very humid region, the coefficient of determination of all indices with the BFI has the ability to be trusted and used. The overall results in the catchments of all climatic zones show FDC indices as a reliable and predictive parameter of BFI.

Key words: Base flow index, Correlation , Estimation , Flow duration curve Index, Hydrograph separation

Keywords


1.Alizadeh, A. 2007.Principal of Applied Hydrology, 14rd Edn. Mashhad. Emamreza University Press, 807p. (In Persian)
2.Bahrami, E., Mohammadrezapour, O., Salarijazi, M., and Jou, P.H. 2019. Effect of base flow and rainfall excess separation on runoff hydrograph estimation using gamma model (case study: Jong catchment). KSCE J. Civil Engin. 23 :3. 1420-1426.
3.Blumenfeld, S., Lu, C., Christopehersen, T., and Coates, D. 2009. Water, wetlands and forests: a review of ecological, economic and policy linkages. Secretariat of the Convention on Biological Diversity and Secretariat of the Ramsar Convention on Wetlands, Montreal and Gland. CBD Technical Series. 47: 1-38.
4.Bosch, D.D., Arnold, J.G., Allen, P.G., Lim, K.J., and Park, Y.S. 2017. Temporal variations in baseflow for the Little River experimental watershed in South Georgia, USA. J. Hydrol: Reg. Stud. 10: 110-121.
5.Brodie, R.S., and Hostetle, S. 2005. A review of techniques for analyzing base-flow from stream hydrographs. Proceedings of the NZHS-IAH-NZSSS Conference, Auckland, New Zealand.
28: 1-13.
6.Castellarina, A., Galeatib, G., Brandimartea, L., Montanaria, L., and Bratha, A.A. 2004. Regional flow-duration curves: reliability for ungauged basins, J. Adv. Water Resour. 27: 953-965.
7.Chapman, T.G., and Maxwell, A.I. 1996. Baseflow separation-comparison of numerical methods with tracer experiments, Hydrology and Water Resources Symposium, Institution of Engineers, Australia, Hobart, 5: 539-545.
8.Choi, W., Rasmussen, P.F., Moore, A.R., and Kim, S.J. 2009. Simulating stream flow response to climate scenarios in central Canada using a simple statistical downscaling method. Climate Research, 40: 1. 89-102.
9.Cook, P.G., Lamontagne, S., Berhane, D., Clark, J.F. 2006. Quantifying groundwater discharge to Cockburn River, southeastern Australia, using dissolved gas tracers222Rn and SF6. Water Resour. Res. 42: 10. 1-12.
10.Costa, V., Fernandez, W., and Naghettini, M. 2014. Regional models of flow-duration curves of perennial
and intermittent streams and their use for calibrating the parameters of a rainfall–runoff model. Hydrol. Sci. J. 59: 2. 262-277.
11.Dario, P., Noto, L.V., and Viola, F. 2013. Eco hydrological modeling of flow duration curve in Mediterranean river basins, J. Adv. Water Resour. 52: 314-327.
12.Deitch, M.J., and Dolman, B. 2017. Restoring summer base flow under a decentralized water management regime: Constraints, opportunities and outcomes in Mediterranean-climate California. Water. 9: 1. 1-21.
13.Eckhardt, K. 2008. A comparison of baseflow indices, which were calculated with seven different baseflow separation methods. J. Hydrol. 352: 1-2. 168-173.
14.Eslami, A.R., and Shokohi, A. 2013. Analysis of river flow, using Hydrological and environmental index, J. Water. Engin. Manage. 5: 2. 125-133. (In Persian)
15.Eslamian, S.S., Ghasemi, M., and Soltani-Gerdefaramarzi, S. 2012. Computation and Regionalization of Low Flow Indices and Determination of Hydrological Drought Durations in Karkhe Watershed, J. Sci. Technol. Agric. Natur. Resour. Water Soil Sci. 16: 59. 1-14. (In Persian)
16.Ghanbarpor, M., Teymori, M., and Gholami, Sh.A. 2008. Comparison of Base Flow Estimation Methods Based on Hydrograph Separation (Case study: Karun Basin). J. Sci. Technol. Agric. Natur. Resour. Water Soil Sci. 1: 1-10. (In Persian)
17.Hisdal, H., Tallaksen, L.M., Clausen, M.B., Peters, E., and Gus-tard, A. 2004. Hydrological drought characteristics, in: Hydrological Drougth - Processes and estimation methods for streamflow and groundwater, edited by: Tallaksen, L.M. and van Lanen, H.A.J., Developments in Water Science, Elsevier Science. 48: 139-198.
18.Hosseini-Doki, S.R., Seyedian, S.M., Rouhani, H., and Farasati, M. 2019. Investigation of the relationship between base flow index with temperature and rainfall using wavelet coherence (Case study: Gorganroud watershed), J. Water Soil Cons. 26: 1. 1-25. (In Persian)
19.Juckem, P.F., Hunt, R.J., Anderson, M.P., and Robertson, D.M. 2008. Effects of climate and land management change on streamflow in the driftless area of Wisconsin. J. Hydrol.355: 1. 123-130.
20.Kazemi, R., and Ghiasi, N. G.2016. Investigation of the Role of Physiographical and Hydrological Parameters on the Shape of Flow Duration Curve (Case Study: Khazar Region), J. Water. Manage. Res.7: 14. 119-127. (In Persian)
21.Kazemi, R., and Sharifi, F. 2019. Investigation and analysis of factors affecting base flow in different climates of Iran, J. Water. Engin. Manage.10: 4. 645-658. (In Persian)
22.Kazemi, R., Ghermez-Cheshmeh, B. 2016. Investigation of Different Base Flow Separation Methods ‎ Using Flow Duration Indices, case study: Khazar region, J. Water Soil Cons. 23: 2. 131-146. (In Persian)
23.Kazemi, R., Karam, A., Saffari, A., and Porhemmat. 2018. Modeling of flow duration curve deformation in Karkheh Basin. J. Geographic. - Space. 17: 60. 131-147. (In Persian)
24.Kazemi, R., and Porhemmat, J. 2020. Calibration of recursive digital filters to separate the base flow, case study: Karkheh Basin, J. Water. Engin. Manage. 12: 1. 30-43. (In Persian)
25.Kazemi, R., Porhemmat, J., and Sharifi, F. 2018. Investigation and determination of factors affecting the shape of the flow duration curve in different climates of Iran, J. Water. Manage. Res.
25: 1. 85-105. (In Persian)
26.Kazemi, R., Porhemmat, J., and Sharifi, F. 2019. Investigating and presenting regional relationships of flow duration curve indices in semi-arid regions, J. Water. Engin. Manage. 11: 3. 676-690. (In Persian)
27.Khosrobeygi-Bozcheloei, S., and Vafakhah, M. 2017. Regional Analysis of Flow Duration Curve in Namak Lake Basin, Iran. J. Water. Manage. Res. 7: 14. 236-228. (In Persian)
28.Kinkela, K., and Pearce, L. 2014. Assessment of baseflow seasonality and application to design flood events in southwest Western Australia. Aust. J. Water Resour. 18: 1. 27-38.
29.Lee, S., Kim, J., and Hur, J.W. 2013. Assessment of ecological flow rate by flow duration and environmental management class in the Geum River, Korea, J. Environ. Earth Sci. 68: 4. 1107-1118.
30.Lee, T.H., Lee, M.H., and Yi, J. 2016. Development of Regional Regression Model for Estimating Flow Duration Curves in Ungauged Basins. J. Korea. Soc. Civil Engin. 36: 3. 427-437.
31.Nathan, R.J., and McMahon, T.A. 1992. Estimating low flow characteristics in ungauged catchments. J. Water Resour. Manage. 6: 85-100.
32.Nathan, R.J., and McMahan, T.A. 1990. Evaluation of automated techniques for baseflow and recession analysis. Water Resour. Res. 26: 7. 1465-1473.
33.Neff, B.P., Day, S.M., Piggott, A.R., and Fuller, L.M. 2005. Base flow in the Great Lakes basin. Scientific Investigations Report, No. 2005-2517. Reston, VA: US Geological Survey.
34.Niazi, A., Bentley, L.R., and Hayashi, M. 2017. Estimation of spatial distribution of groundwater recharge from stream baseflow and groundwater chloride. J. Hydrol. 546: 380-392.
35.Reichl, F., and Hack, J. 2017. Derivation of flow duration curves to estimate hydropower generation potential in data-scarce regions. J. Water. 9: 8. 572.1-15.
36.Shamaee-Zadeh, M., and Soltani, S. 2011. Regional analysis of low flow in North Karoon basin, J. Sci. Technol. Agric. Resour. Water and Soil Science. 18: 70. 231-242. (In Persian)
37.Sun, W., Song, X., Zhang, Y., Chiew, F., Post, D., Zheng, H., and Song, S. 2020. Coal mining impacts on baseflow detected using paired catchments. Water Resources Research. 56: 2. 257-270.
38.Swain, J.B., and Patra, K.C. 2017. Streamflow estimation in ungauged catchments using regional flow duration curve: comparative study. J. Hydrol. Engin. 22: 7. 04017010.
39.Tague, C., Grant, G., Farrell, M., Choate, J., and Jefferson, A. 2008. Deep groundwater mediates streamflow response to climate warming in the Oregon Cascades. Climatic Change. 86: 1. 89-210.
40.Teimouri, M., Ghanbarpour, M.R., Bashirgonbad, M., Zolfaghari, M., and Kazemikia, S. 2011. Comparison of Base Flow Index in Hydrograph Separation with Different Methods in Some Rivers of West Azarbaijan Province. J. Sci. Technol. Agric. Natur. Resour. Water and Soil Science.
15: 219-228. (In Persian)
41.Verma, R.K., Murthy, S., Verma, S., and Mishra, S.K. 2017. Design flow duration curves for environmental flows estimation in Damodar River Basin, India. Applied Water Science,
7: 3. 1283-1293.
42.Wagener, T., Blöschl, G., Goodrich, D., Gupta, H., Sivapalan, M., Tachikawa, Y., Troch, P., and Weiler, M. 2013. A synthesis framework for runoff predictions in ungauged basins, in: chapt. 2, Runoff Predictions in Ungauged Basins, edited by: Blöschl, G., Sivapalan, M., Wagener, T., Viglione, A., and Savenije, H., Cambridge University Press, Cambridge, UK, Pp: 11-28.
43.Welderufael, W.A., and Woyessa, Y.E. 2010. Stream flow analysis and comparison of base flow separation methods, Case Study of the Modder River Basin in central South Africa. J. Europ. Water. 31: 3-12.
44.Westerberg, I.K., Guerrero, J.L., Younger, P.M., Beven, K.J., Seibert, J., Halldin, S., Freer, J.E., and Xu, C.Y. 2011. Calibration of hydrological models using flow-duration curves. J. Hydrol. Earth Syst. Sci. 15: 2205-2227.
45.Zare Chahouki, A., Salajegheh, A., Mahdavi, M., Khalighi, Sh., and Asadi, S. 2013. Regional flow duration curve in arid regions for ungauged basins (Case study: Central Iran). 66: 2. 251-265.
(In Persian)
46.Zhang, L., Brutsaert, W., Crosbie, R., and Potter, N. 2014. Long-term annual groundwater storage trends in Australian catchments. Adv. Water Resour. 74: 156-165.
47.Zhu, Y., Chen, L., Wang, K., Wang, W., Wang, C., and Shen, Z. 2019. Evaluating the spatial scaling effect of baseflow and baseflow nonpoint source pollution in a nested watershed. J. Hydrol. 579: 12.42-21.