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
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
Binyamin J, Rouse WR, Davies JA et al (2006) Surface energy balance calculations for small northern lakes. Int J Climatol 26(15):2261–2273
Bolton D (1980) The Computation of Equivalent Potential Temperature. Mon Weather Rev 108(7):1046–1053
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
Brandt SA (2000) Classification of geomorphological effects downstream of dams. Catena 40(4):375–401
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
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
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
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
Crutzen PJ (2002) Geology of mankind. Nature 415(6867):23
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
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
Lewis WM (1983) Temperature, heat, and mixing in lake Valencia, Venezuela. Limnol Oceanogr 28(2):273–286
Livingstone DM, Imboden DM (1989) Annual heat balance and equilibrium temperature of Lake Aegeri, Switzerland. Aquat Sci 51(4):351–369
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
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
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
Nilsson C, Reidy CA, Dynesius M et al (2005) Fragmentation and flow regulation of the world’s large river systems. Science 308(5720):405
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
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
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
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
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
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
Walling DE, Fang D (2003) Recent trends in the suspended sediment loads of the world’s rivers. Global Planet Change 39(1):111–126
Wang J, Sheng Y, Gleason CJ et al (2013) Downstream Yangtze River levels impacted by Three Gorges Dam. Environ Res Lett 8(4):4012
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
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
Wu CL, Chau KW (2006) A flood forecasting neural network model with genetic algorithm. Int J Environ Pollut 28(3):261–273
Xu J (1996) Channel pattern change downstream from a reservoir: An example of wandering braided rivers. Geomorphology 15(2):147–158
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
Zalasiewicz J, Williams M, Steffen W et al (2010) The new world of the anthropocene1. Environ Sci Technol 44(7):2228
Zheng H (2015) Birth of the Yangtze river: age and tectonic-geomorphic implications. Nat Sci Rev 2(4):438–453
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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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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DOI: https://doi.org/10.1007/s12665-018-7940-2