Climate change in East Central Minnesota

skyline view of minneapolis and the mississippi river

Aitkin, Crow Wing, Carlton, Pine, Mille Lacs, Kanabec, Isanti, Chisago, Anoka, Washington, Hennepin, and Ramsey counties

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Key Terms

Time Periods

  • Historical Simulations: 1995-2014
  • Mid-century: 2040-2059
  • Late-century: 2060-2079
  • End-of-century: 2080-2099
     

Emissions Scenarios

  • Intermediate emissions: "business as usual" economic, social and technology trends (SSP245)
  • Very high emissions: driven by increased fossil fuel consumption (SSP585)

Learn more about climate modeling and emissions scenarios

Download this summary as a PDF

Changes we've already observed

Between 1895 and 2023, the average annual temperature in East Central Minnesota has increased by 3.5°F. The statewide average increase over the same period was 3.1°F

Most of this warming is concentrated during the coldest months of the year, with average winter temperatures increasing by 5.6°F and average winter low temperatures increasing by 6.7°F. 

The region also experienced, on average, an increase of 4.1 inches of precipitation per year between 1895 and 2023. The statewide increase, meanwhile, was 3.3 inches of precipitation per year.

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Figure: Observed and projected temperature change in MN

map of observed temperature change in MN
Figure 1: Observed and projected temperature changes in Minnesota under “lower” (teal) and “higher” (red) emissions scenarios out to 2100 compared to historical temperature observations (orange). 

Projected changes in temperature

By mid-century, annual average daily maximum temperature in East Central Minnesota is projected to increase between 3.4°F under an intermediate emissions scenario and 4.1°F under a very high emissions scenario. This is similar to the statewide average, which is projected to increase between 3.6°F under an intermediate emissions scenario and 4.2°F under a very high emissions scenario.

Similar to observed trends, projected increases in wintertime lows are greater than projected increases in summertime highs. On average, daily minimum temperatures in the winter are projected to increase by 6.1°F and daily maximum temperatures in the summer are projected to increase by 4.8°F by mid-century under a very high emissions scenario.

By mid-century, warming temperatures could result in 22-25 fewer days with a low below freezing (32°F) in East Central Minnesota in a given year.

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Map: Projected change in average daily maximum temperature

Projected change in temperature in East Central Minnesota

Table: Projected change in days with highs above 90°F and lows below 32°F in East Central MN

Emissions Scenario

Change in number of days that exceed 90°F

Change in number of days with a minimum temperature below 32F

Intermediate

+11

-21

Very High

+17

-25

Projected changes in precipitation

Average annual precipitation in East Central Minnesota is projected to increase between 0.1 inches (0.3%) under a very high emissions scenario and 1.4 inches (4.3%) in an intermediate emissions scenario by mid-century. This is similar to the statewide average, which is projected to increase by 0.1 inches (0.3%) under a very high emissions scenario and by 1.2 inches (4.1%) under an intermediate emissions scenario. 

Note: Precipitation is not expected to change uniformly throughout the year, often with wintertime and springtime averages projected to increase, and summertime averages projected to decrease. In the higher emissions scenarios, summertime averages are expected to decrease so much that they can lower annual average values overall.

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Map: Projected change in average spring and summer precipitation

map of projected change in spring and summer precipitation in East Central Minnesota

Table: Projected change in maximum 1-day and 7-day precipitation in East Central MN

Emissions Scenario

Change in maximum 1-day total precipitation  (inches)

Change in maximum 7-day total precipitation (inches)

Intermediate

+0.37

+0.72

Very High

+0.19

+0.38

Key climate impacts for East Central Minnesota

Water Resources

  • As more rain falls in a shorter period of time, the risk of flooding increases. Because of the higher proportion of paved surfaces in urban areas, floods are particularly hazardous — leading to transportation disruptions and overwhelming aging stormwater-sewer systems [2,3].
  • Higher summertime temperatures and the associated risk of summertime drought [4] increase the likelihood that water demand will outpace supply, particularly in heavily populated areas.  

Agriculture

  • Crop models suggest that corn and soybean yields decline at sustained temperatures above 86°F [5].
  • Increased spring precipitation is expected to result in greater pest and disease transmission for a variety of crops and farm animals [6], and decreased summer precipitation results in potential declines for crops ranging from fresh market vegetables to grains [7].

Tribal Lifeways

  • Culturally important species are threatened by rising temperatures and changing precipitation patterns. For example, cold-water fish like walleye — vital to fisheries such as Mille Lacs — face habitat loss [8].
  • Wild rice harvests may decline because of increasing spring precipitation, along with less snowfall in the winter [8].

Tourism & Recreation

  • Increasing temperatures in the winter months could prevent lake ice formation [9, 6] and reduce snowpack, creating unsuitable conditions for popular activities such as ice fishing, skiing and snowmobiling.
  • Warmer surface waters increase the risk of harmful algal blooms [10], which are detrimental to human health and make lakes unsuitable for swimming and water sports.

Human Health

  • Exposure to temperatures above 90°F increases the risk of heat illnesses that can turn into a medical emergency [12]. Urban areas can trap heat — hot spots have been measured up to 20°F warmer than surrounding areas [13]. Those who work outdoors are especially vulnerable [14, 15].
  •  Warming temperatures will expand the habitat and lifecycle for carriers of vector-borne diseases, such as the black-legged tick (Lyme Disease) [16, 17] — even in urban areas.

 

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Disclosure

The historical data in this summary are from the National Oceanic and Atmospheric Administration (NOAA) and the Minnesota Department of Natural Resources (DNR). Climate projection data are provided by the University of Minnesota Climate Adaptation Partnerships MN-CliMAT tool, which provides highly localized climate projections for Minnesota out to 2100. This is not a comprehensive summary; for other time horizons, variables, regions, and climate scenarios, please go to app.climate.umn.edu. Email [email protected] with any questions. © 2024 Regents of the University of Minnesota. University of Minnesota Extension is an equal opportunity educator and employer. In accordance with the Americans with Disabilities Act, this publication/material is available in alternative formats upon request. Direct requests to 612-624-9282.

References

  1. Akinsanola et al., 2020. Environ. Res. Lett.
  2. Payton et al., 2023. USGCRP
  3. Olds et al., 2018. PLOS Med.
  4. Otkin et al., 2022. Bull. Am. Meteorol. Soc.
  5. Roop et al., 2024 USDA Climate Hubs
  6. Wilson et al., 2023. USGCRP 
  7. Grotjahn et al., 2021. Extrm Evts and Clmt Chng
  8. GLIFWC Climate Change Team, 2023. Grt Lks Indian Fish and Wildlife Cmsn 
  9. Sharma et al., 2001. JGR Biogeosci.
  10. Paerl and Huisman, 2008. Science.
  11. United States, 2024. DHS
  12. NIHHS, n.d.
  13. FEMA, 2024. DHS.
  14. NIOSH, 2020. CDC.
  15. Hayden et al., 2023. NCA5
  16. Johnson et al., 2018. Am. J. Trop. Med. Hyg.

Suggested citation

Coffman, D., Black, K., Boyd, K., Clark, S., Greene, B., Saravana, D., Weske, C. 2024. Climate Change in East Central Minnesota. Prepared for the University of Minnesota Climate Adaptation Partnership. Version 1; September 2024. www.climate.umn.edu/regional-climate-summaries