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The influence of the Three Gorges Reservoir regulation on a typical tributary heat budget

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Abstract

Reservoir regulation and local climate both affect the heat budget of tributary bay. It is difficult for traditional methods to identify the influence of different factors on heat budget quantitatively. In this paper, for analysis of the control mechanisms of the heat budget of a large reservoir tributary, the water temperature distribution, and heat budget processes of the Meixi River, a typical tributary to the Three Gorges Reservoir was measured, and a new method was used to calculate the heat content composition of the tributary bay and identify the key factor of the heat balance. The result shows significant variation in the spatial and temporal distributions of water temperatures in the Meixi River, ranging from 12.4 to 28.9 °C on the surface and 12.0 to 24.4 °C at the bottom. The total heat exchange across the air–water interface that ranges from 0.1 to 6% of the budget is not the primary control factor of the annual tributary heat budget. Rather, the change in water depth produced by regulation of the Three Gorges Reservoir is the primary control factor of the tributary heat budget in the whole year, which ranges from 72 to 99% of the budget. The water temperature difference between the main stream and tributary is the not key factor of the heat budget, which ranges from 0.1 to 28% of the heat budget.

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References

  • Authority TV (1972) Heat and Mass Transfer between a Water Surface and the Atmosphere (Water Resources Research Laboratory Report 14). Tennessee Valley Authority, Division of Water Control Planning, Engineering Laboratory

    Google Scholar 

  • Batalla RJ, Gómez CM, Kondolf GM (2004) Reservoir-induced hydrological changes in the Ebro River basin (NE Spain). J Hydrol 290(1–2):117–136

    Article  Google Scholar 

  • Binyamin J, Rouse WR, Davies JA et al (2006) Surface energy balance calculations for small northern lakes. Int J Climatol 26(15):2261–2273

    Article  Google Scholar 

  • Bolton D (1980) The Computation of Equivalent Potential Temperature. Mon Weather Rev 108(7):1046–1053

    Article  Google Scholar 

  • Bondar C, Blendea V (1997) Water and sediment transport by the Danube into the Black Sea during 1840–1995

  • Bowen IS (1926) The Ratio of Heat Losses by Conduction and by Evaporation from any Water Surface. Phys Rev 27(6):779–787

    Article  Google Scholar 

  • Brandt SA (2000) Classification of geomorphological effects downstream of dams. Catena 40(4):375–401

    Article  Google Scholar 

  • Chen C, Li J, Shen H et al (2001) Yangtze River of China: historical analysis of discharge variability and sediment flux. Geomorphology 41(2):77–91

    Article  Google Scholar 

  • Chen XY, Chau KW, Busari AO (2015) A comparative study of population-based optimization algorithms for downstream river flow forecasting by a hybrid neural network model. Eng Appl Artif Intell 46(A):258–268

    Article  Google Scholar 

  • Chong-yu X, Gong L, Jiang T et al (2006) Analysis of spatial distribution and temporal trend of reference evapotranspiration and pan evaporation in Changjiang (Yangtze River) catchment. J Hydrol 327(1–2):81–93

    Google Scholar 

  • Colomer J, Roget E, Casamitjana X (1996) Daytime heat balance for estimating non-radiative fluxes of Lake Banyoles, Spain. Hydrol Process 10(5):721–726

    Article  Google Scholar 

  • Crutzen PJ (2002) Geology of mankind. Nature 415(6867):23

    Article  Google Scholar 

  • Gill AE (1982) Atmosphere-ocean dynamics. Academic Press, Cambridge

  • Ji Z-G (2008) Hydrodynamics and water quality: modeling rivers, lakes, and estuaries. Wiley, Hoboken

  • Keijman JQ (1974) The estimation of the energy balance of a lake from simple weather data. Bound-Layer Meteorol 7(3):399–407

    Article  Google Scholar 

  • Koel TM, Sparks RE (2002) Historical patterns of river stage and fish communities as criteria for operations of dams on the Illinois river. River Res Appl 18(1):3–19

    Article  Google Scholar 

  • Lewis WM (1983) Temperature, heat, and mixing in lake Valencia, Venezuela. Limnol Oceanogr 28(2):273–286

    Article  Google Scholar 

  • Livingstone DM, Imboden DM (1989) Annual heat balance and equilibrium temperature of Lake Aegeri, Switzerland. Aquat Sci 51(4):351–369

    Article  Google Scholar 

  • Lu XX, Siew RY (2006) Water discharge and sediment flux changes over the past decades in the Lower Mekong River: possible impacts of the Chinese dams. Hydrol Earth Syst Sci 10(2):181–195

    Article  Google Scholar 

  • Mcclelland JW, Holmes RM, Peterson BJ et al (2004) Increasing river discharge in the Eurasian Arctic: Consideration of dams, permafrost thaw, and fires as potential agents of change. J Geophys Res Atmos 109(18):159–172

    Google Scholar 

  • Myrup LO, Powell TM, Godden DA et al (1979) Climatological estimate of the average monthly energy and water budgets of Lake Tahoe California-Nevada. Water Resour Res 15(6):1499–1508

    Article  Google Scholar 

  • Nilsson C, Reidy CA, Dynesius M et al (2005) Fragmentation and flow regulation of the world’s large river systems. Science 308(5720):405

    Article  Google Scholar 

  • Oswald CJ, Rouse WR (2004) Thermal characteristics and energy balance of various-size Canadian Shield Lakes in the Mackenzie River Basin. J Hydrometeorol 5(1):129–144

    Article  Google Scholar 

  • Power ME, Dietrich WE, Finlay JC (1996) Dams and downstream aquatic biodiversity: potential food web consequences of hydrologic and geomorphic change. Environ Manag 20(6):887–895

    Article  Google Scholar 

  • Rouse WR, Oswald CM, Binyamin J et al (2009) Interannual and seasonal variability of the surface energy balance and temperature of central great Slave Lake. J Hydrometeorol 4(2003):720

    Google Scholar 

  • Tanny J, Cohen S, Berger D et al (2011) Evaporation from a reservoir with fluctuating water level: correcting for limited fetch. J Hydrol 404(3–4):146–156

    Article  Google Scholar 

  • Topping DJ, Rubin DM, Jr LEV (2000) Colorado River sediment transport: 1. Natural sediment supply limitation and the influence of Glen Canyon Dam. Water Resour Res 36(2):515–542

    Article  Google Scholar 

  • Villanueva RJB (2003) Sediment deficit in rivers caused by dams and instream gravel mining: a review with examples from NE Spain. 17:79–91

  • Vösösmarty CJ, Sharma KP, Fekete BM et al (1997) The storage and aging of continental runoff in large reservoir systems of the world. Ambio 26(4):210–219

    Google Scholar 

  • Walling DE, Fang D (2003) Recent trends in the suspended sediment loads of the world’s rivers. Global Planet Change 39(1):111–126

    Article  Google Scholar 

  • Wang J, Sheng Y, Gleason CJ et al (2013) Downstream Yangtze River levels impacted by Three Gorges Dam. Environ Res Lett 8(4):4012

    Google Scholar 

  • Wang WC, Xu DM, Chau KW et al (2014) Assessment of River Water Quality Based on Theory of Variable Fuzzy Sets and Fuzzy Binary Comparison Method. Water Resour Manage 28(12):4183–4200

    Article  Google Scholar 

  • Willis CM, Griggs GB (2003) Reductions in fluvial sediment discharge by coastal dams in California and implications for beach sustainability. J Geol 111(2):167–182

    Article  Google Scholar 

  • Wu CL, Chau KW (2006) A flood forecasting neural network model with genetic algorithm. Int J Environ Pollut 28(3):261–273

    Article  Google Scholar 

  • Xu J (1996) Channel pattern change downstream from a reservoir: An example of wandering braided rivers. Geomorphology 15(2):147–158

    Article  Google Scholar 

  • Yang SL, Zhang J, Dai SB et al (2007) Effect of deposition and erosion within the main river channel and large lakes on sediment delivery to the estuary of the Yangtze River. J Geophys Res Earth Surface 112(F2):111–119

    Article  Google Scholar 

  • Zalasiewicz J, Williams M, Steffen W et al (2010) The new world of the anthropocene1. Environ Sci Technol 44(7):2228

    Article  Google Scholar 

  • Zheng H (2015) Birth of the Yangtze river: age and tectonic-geomorphic implications. Nat Sci Rev 2(4):438–453

    Article  Google Scholar 

Download references

Acknowledgements

We thank the anonymous reviewers for their valuable comments which greatly improve the manuscript. The study was financially supported by the National Key Research and Development Program (2017YFC0505305), the Major Science and Technology Program for Water Pollution Control and Treatment in China (2017ZX07301006005), National Natural Science Foundation of China (51509066, 91647208, 51679258 and 91547109), Open Research Fund of the State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research (SKL2016ZY04, SKL2018ZY04) and Applied Basic Research Program of Hebei Province (14964206D-3).

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Correspondence to Yao Cheng.

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This article is a part of a Topical Collection in Environmental Earth Sciences on Water Resources and Hydraulic Engineering, guest edited by Drs. Yanqing Lian, Walton Kelly, and Fulin Li.

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Cheng, Y., Wang, Y., Zhou, H. et al. The influence of the Three Gorges Reservoir regulation on a typical tributary heat budget. Environ Earth Sci 77, 764 (2018). https://doi.org/10.1007/s12665-018-7940-2

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