Global Warming Effects Around the World

Cleveland, OH, USA

Top Impact

Freshwater (Extreme wet)

Other Impacts

Temperature (Air)

Freshwater (Land ice)

A father and son team dig out their sidewalk after severe snows in Cleveland, Ohio.

Lake-effect snowfall is a fact of life in Cleveland, OH, located on the southeastern shore of Lake Erie. Scientists expect extreme winter storms to become more frequent and more intense in the area over the next few decades as our climate changes.1

Key Facts

Global warming is causing an increase in extreme precipitation throughout the Midwest.7,8,9 If our heat-trapping emissions continue to rise at current rates, scientists project more intense storms, some of which can produce more snowfall during winter in Cleveland, even as the snowy ground cover season shortens due to a warming climate.9,10,15

  • A phenomenon called lake-effect snow makes Cleveland and other places along the southern and eastern shores of the Great Lakes among the snowiest in North America.9 Global warming has been contributing to an increase in lake-effect snow since 1950.10,12
  • In the Midwest, heavy downpours now occur about twice as often as a century ago, and the amount of rainfall during heavy rainstorms has increased by nearly one-third over the past 50 years.7,8,9,10
  • Scientists expect more intense storms to occur in the Midwest over the next few decades, bringing more precipitation in winter and spring and more lake-effect snowfall.9,10,15

Details

Cleveland, the second-largest city in Ohio, sits on the southern shore of Lake Erie, the shallowest of the Great Lakes.2,3 Historically a manufacturing center, Cleveland remains a science and engineering hub, with a growing service sector that includes industries such as banking, health care, and insurance.4,5 The city is also home to the Rock and Roll Hall of Fame.5,6

Global warming has brought more intense storms and more precipitation to Cleveland and other parts of the Midwest, where heavy downpours now occur about twice as often as they did a century ago.7,8

On average, the amount of precipitation that falls during the heaviest 1 percent of rainstorms and snowstorms in the United States has increased nearly 20 percent during the past 50 years—almost three times the rate of increase in total annual precipitation.9,10 The Midwest saw an even larger average increase of around 31 percent, surpassed only by the Northeast (at around 67 percent).9,10 Scientists attribute the overall rise in heavy precipitation to climate change that has already occurred over the past half-century.11

A phenomenon called lake-effect snow is spurring some of the higher winter precipitation in Cleveland—already among the snowiest places in North America.9 Such snow occurs when cold winds from the northwest flow over the relatively warmer Great Lakes, pick up moisture, and drop it as snow on the lakes' southern and eastern shores.9 The amount of snow that falls during a blizzard is a different measure than the area of ground covered by snow for more than 30 days—this measure has been decreasing in the northern hemisphere and is a clear indicator of climate change.10

Though it may seem counterintuitive, global warming has been contributing to an increase in lake-effect snow south and east of the Great Lakes for the past 60 years.10,12 That is because the less ice there is on the surface of a large lake, the more moisture can evaporate. And if the air is cold enough, that extra water vapor can fall as snow.13

Various pieces of evidence indicate that the Great Lakes are warming. For example, the ice season has been starting later and ending earlier since the 1850s.14 And rising air temperatures during the spring, summer, and autumn may be having more of an impact on water temperatures (setting the conditions for lake-effect snow) than winter air temperatures.15

Ice coverage on the Great Lakes has decreased as the climate has warmed, shrinking at a rate of 8.4 percent per decade from 1973 through 2008.13 This roughly 30 percent decline in ice coverage has created conditions conducive to heavier snowfalls and more extreme storms.10,16

What the Future Holds

Scientists expect more intense storms to occur in the Midwest, and more precipitation to fall in winter and spring.9 According to climate models, lake-effect snowfall is likely to continue rising over the next few decades during periods when winter temperatures remain below freezing.10,15

More snowfall and extreme weather in Cleveland could wreak havoc on transportation and commerce throughout northeast Ohio, requiring more spending on snow removal, and making spring flooding more severe. Heavy lake-effect snows can benefit winter recreation, agriculture, and regional hydrology, but they can also endanger people's lives, damage property, disrupt air and surface transportation, and hurt farming, water supplies, and hydroelectric power.15

Later this century, lake-effect snow is likely to decline as temperatures continue rising, with more precipitation falling as rain.17

Credits

Endnotes

  1. Photograph used by permission. Chuck Crow/The Plain Dealer /Landov.
  2. U.S. Census Bureau. 2009. Population estimates. Online at http://factfinder.census.gov/ servlet/ GCTTable?_bm=y&-context=gct &-ds_name=PEP_2009_EST &-CONTEXT=gct & -mt_name=PEP_2009_EST_GCTT1R_ST2S &-tree_id=809 &-redoLog=true & -_caller=geoselect &-geo_id=04000US39 &-format=ST-9|ST-9S &-_lang=en. Accessed June 29, 2010.
  3. U.S. Environmental Protection Agency. 2008. Great Lakes: Basic information. Washington, DC. Online at http://www.epa.gov/ glnpo/ basicinfo.html#erie. Accessed June 30, 2010.
  4. City-data.com. 2004. Cleveland: Economy. Online at http://www.city-data.com/ us-cities/ The-Midwest/ Cleveland-Economy.html. Accessed June 30, 2010.
  5. Positively Cleveland. 2010. History of Cleveland. Cleveland, OH. Online at http://www.positivelycleveland.com/ visit/ cleveland_history. Accessed June 30, 2010.
  6. Rock and Roll Hall of Fame and Museum. 2010. Visiting the museum. Cleveland, OH. Online at http://rockhall.com/ visit-the-museum/. Accessed June 30, 2010.
  7. Kunkel, K., K. Andsager, and D. Easterling. 1999. Long-term trends in extreme precipitation events over the conterminous United States and Canada. Journal of Climate 12:2515-2527.
  8. Union of Concerned Scientists. 2009. Confronting climate change in the U.S. Midwest: Ohio. Cambridge, MA. Online at www.ucsusa.org/ mwclimate. Accessed June 30, 2010.
  9. Kunkel, K.E., P.D. Bromirski, H.E. Brooks, T. Cavazos, A.V. Douglas, D.R. Easterling, K.A. Emanuel, P.Ya. Groisman, G.J. Holland, T.R. Knutson, J.P. Kossin, P.D. Komar, D.H. Levinson, and R.L. Smith, 2008: Observed changes in weather and climate extremes. In: Weather and climate extremes in a changing climate: Regions of focus—North America, Hawaii, Caribbean, and U.S. Pacific Islands. Edited by Karl, T.R., G.A. Meehl, C.D. Miller, S.J. Hassol, A.M. Waple, and W.L. Murray. Synthesis and assessment product 3.3. Washington, DC: U.S. Climate Change Science Program, pp. 35-80.
  10. U.S. Global Change Research Program. 2009. Global climate change impacts in the United States. Edited by T.R. Karl, J.M. Melillo, and T.C. Peterson. Cambridge University Press.
  11. Trenberth, K.E., P.D. Jones, P. Ambenje, R. Bojariu, D. Easterling, A. Klein Tank, D. Parker, F. Rahimzadeh, J.A. Renwick, M. Rusticucci, B. Soden, and P. Zhai. 2007. Observations: Surface and atmospheric climate change. In: Climate change 2007: The physical science basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Edited by S. Solomon, D. Qin, M. Manning, Z. Chen, M. Marquis, K.B. Averyt, M. Tignor, and H.L. Miller. Cambridge University Press.
  12. Cook, E.R., P.J. Bartlein, N. Diffenbaugh, R. Seager, B.N. Shuman, R.S. Webb, J.W. Williams, and C. Woodhouse. 2008. Hydrological variability and change. In: Abrupt climate change. Synthesis and assessment product 3.4. Reston, VA: U.S. Geological Survey, 143-257.
  13. U.S. Global Change Research Program. 2009. Global climate change impacts in the United States. Edited by T.R. Karl, J.M. Melillo, and T.C. Peterson. Cambridge University Press.
  14. Assel, R.A., and D.M. Robertson. 1995. Changes in winter air temperatures near Lake Michigan, 1851-1993, as determined from regional lake-ice records. Limnology and Oceanography 40:165-176.
  15. Burnett, A.W., M.E. Kirby, H.T. Mullins, and W.P. Patterson. 2003. Increasing Great Lake-effect snowfall during the twentieth century: A regional response to global warming? Journal of Climate 16 (21):3535-3542.
  16. Assel, R.A. 2003. An electronic atlas of Great Lakes ice cover, winters, 1973-2002. Ann Arbor, MI: National Atmospheric and Oceanic Administration, Great Lakes Environmental Research Laboratory. Online at http://www.glerl.noaa.gov/ data/ ice/ atlas.
  17. Kunkel, K.E., N.E. Westcott, and D.A.R. Knistovich. 2002. Assessment of potential effects of climate changes on heavy lake-effect snowstorms near Lake Erie. Journal of Great Lakes Research 28 (4):521-536.
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