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How does the North Atlantic Oscillation affect the water levels of the Great Lakes with regard to hydro-climatic indicators?

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Abstract

In this study, the changes of long-term mean annual water levels of the Great Lakes in North America are investigated, including the potential impacts of the North Atlantic Oscillation (NAO). The levels of Lakes Superior, Michigan-Huron, St. Clair, Erie and Ontario and the hydro-climatic data, such as precipitation, evaporation and runoff, are evaluated together in view of the influence of NAO. The changes in the lake levels and hydro-climatic indicators are analysed. The annual hydro-climatic data, annual mean lake levels and the NAO indices are nondimensionalized through the nonparametric Mann-Kendall test. Then, the sequential Mann-Kendall test and paired t test are performed to gain insight into the trends of the time series and possible turning points. As a result of this study, the trend direction changes for all of the lakes are determined in the years 1965 and 1987, based on the records of the last 95 years. A similar tendency for evaporation, precipitation and runoff is found in 1982, 1935 and 1965. Regarding the effect of North Atlantic Oscillation on the changes of the lake levels, the same directional variations are found between the lake levels and the NAO FMA (February-March-April) indices. However, the directional variations between the lake levels and NAO JJA (June-July-August) indices are reversed. The absolute values of the correlation coefficients increase from west to east (from Lake Superior to Lake Ontario).

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References

  • Changnon SA (2004) Temporal behavior of levels of the Great Lakes and climate variability. J Great Lakes Res 30(1):184–200

    Article  Google Scholar 

  • Coulibaly P (2010) Reservoir computing approach to Great Lakes water level forecasting. J Hydrol 381:76–88

    Article  Google Scholar 

  • Cripe, D.G. (2005) Investigation of the relationship between the Pacific/North American (PNA) and North Atlantic Oscillation (NAO) teleconnections, and great lake-effect snowfall. PhD Thesis, Kent State University, College of Arts and Sciences/Department of Geography, 301p

  • Dogan M, Ulke A, Cigizoglu HK (2015) Trend direction changes of Turkish temperature series in the first half of 1990s. Theor Appl Climatol 121:23–39

    Article  Google Scholar 

  • Ghanbari RN, Bravo HR (2008) Coherence between atmospheric teleconnections Great Lakes water levels, and regional climate. Advances in Water Resources 31:1284–1298

    Article  Google Scholar 

  • Herche LR, Hartmann HC (1992) Estimation of Great Lakes water level statistics: conditioning via -the bootstrap. J Great Lakes Res 18(1):218–228

    Article  Google Scholar 

  • Hurrell J (1995) Decadal trends in the North Atlantic Oscillation: regional temperatures and precipitation. Science 269:676–679

    Article  Google Scholar 

  • Jones PD, Jonsson T, Wheeler D (1997) Extension to the North Atlantic Oscillation using early instrumental pressure observations from Gibraltar and south-west Iceland. Int J Climatol 17:1433–1450

    Article  Google Scholar 

  • Lofgren BM, Hunter TS, Wilbarger J (2011) Effects of using air temperature as proxy for potential evapotranspiration in climate change scenarios of Great Lakes basin hydrology. J Great Lakes Res 37(4):744–752

    Article  Google Scholar 

  • Polderman NJ, Pryor SC (2004) Linking synoptic-scale climate phenomena to lake-level variability in the Lake Michigan-Huron basin. J Great Lakes Res 30:419–434

    Article  Google Scholar 

  • Quinn FH (2002) Secular changes in Great Lakes water level seasonal cycles. J Great Lakes Res 28(3):451–465

    Article  Google Scholar 

  • Sellinger CE, Stow CA, Lamon EC, Qian SS (2008) Recent water level declines in the Michigan-Huron system. Environ Sci Technol 42:367–373

    Article  Google Scholar 

  • Wang J, Bai X, Hu H, Clites A, Colton M, Lofgren B (2012) Temporal and spatial variability of Great Lakes ice cover, 1973–2010. J Clim 25:1318–1329

    Article  Google Scholar 

  • Yu YS, Zau S, Whittemore D (1993) Nonparametric trend analysis of water quality data of rivers in Kansas. J Hydrol 150:61–80

    Article  Google Scholar 

  • Zhang X, Harvey KD, Hogg WD, Yuzyk TR (2001) Trends in Canadian streamflow. Water Resour Res 37(4):987–998

    Article  Google Scholar 

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Acknowledgments

The author thanks the National Oceanic and Atmospheric Administration Great Lakes Environmental Research Laboratory (http://www.glerl.noaa.gov/) for the free downloadable data used in the present study.

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Authors and Affiliations

  1. Department of Civil Engineering, Dokuz Eylul University, 35160, Buca, Izmir, Turkey

    Mustafa Dogan

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  1. Mustafa Dogan
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Correspondence to Mustafa Dogan.

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Dogan, M. How does the North Atlantic Oscillation affect the water levels of the Great Lakes with regard to hydro-climatic indicators?. Theor Appl Climatol 126, 597–609 (2016). https://doi.org/10.1007/s00704-015-1603-y

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  • DOI: https://doi.org/10.1007/s00704-015-1603-y

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