Great Lakes Ice Cover
Understanding the major effect of ice on the Great Lakes is crucial because it impacts a range of societal benefits provided by the lakes,
from hydropower generation to commercial shipping to the fishing industry. The amount of ice cover varies from year to year, as well as how
long it remains on the lakes. Studying, monitoring, and predicting ice coverage on the Great Lakes plays an important role in determining regional weather patterns, lake water levels, water movement patterns, water temperature structure, and spring plankton blooms.
NOAA-GLERL has been exploring the relationships between ice cover, lake thermal structure,
and regional weather for over 30 years through development, maintenance, and analysis of
historical model simulations and observations of ice cover, surface water temperature, and
other variables. Weekly ice cover imaging products produced by the Canadian Ice Service
started in 1973. Beginning in 1989, the U.S. National Ice Center
produced Great Lakes ice cover charts that combined both Canadian and U.S. agency satellite imagery. These products
are downloaded at GLERL by our Coastwatch
program, a nationwide NOAA program within which the GLERL functions as the Great Lakes regional node. In this capacity, GLERL obtains,
produces, and delivers environmental data and products for near real-time observation of the
Great Lakes to support environmental science, decision making, and supporting research. This
is achieved by providing access to near real-time and retrospective satellite observations and in-situ Great Lakes data.
Current Ice Cover Conditions
Coastwatch and GLSEA
CoastWatch is a nationwide National Oceanic and Atmospheric Administration
(NOAA) program within which the Great Lakes Environmental Research Laboratory (GLERL) functions as the Great Lakes regional node. In this capacity,
GLERL obtains, produces, and delivers environmental data and products for near real-time observation of the Great Lakes to support environmental science,
decision making, and supporting research. This is achieved by providing access to near real-time and retrospective satellite observations and in-situ Great Lakes data.
GLSEA (The Great Lakes Surface Environmental Analysis) is a digital map of the Great Lakes surface water temperature and ice cover which is produced daily at GLERL.
The lake surface temperatures are derived from NOAA polar-orbiting satellite imagery.
The addition of ice cover information was implemented in early 1999, using data provided by the US National Ice Center (USNIC). Lake surface temperatures are updated daily with information from the cloud-free portions of the previous day's satellite imagery. If no imagery is available,
a smoothing algorithm is applied to the previous day's map.
Graphs of Daily Ice Cover for the Current Season:
Historical Ice Cover
NOAA/GLERL has been monitoring and documenting Great Lakes ice cover since the early 1970's using the ice products developed by the
U.S. National Ice Center and the Canadian Ice Service. Research conducted on hydrometeorological processes and regional weather trends
has led to models of lake thermal structure that play an integral role in ecosystem forecasting.
Annual Maximum Ice Cover Plots
Click image to enlarge:
Data files:
Annual Maximum Ice Cover by Lake
Annual Maximum Ice Cover by Lake with Dates
Great Lakes Ice Cover Database
This database simplifies access to Great Lakes ice cover data by bringing the basic units of data together for the entire time period,
1973-present. The (now retired) Great Lakes Ice Atlas summarized ice cover for the period 1973-2002,
with addendums in a separate report for 2003-2005, in addition to providing a number of statistical products. Using the same methods, the
original ice charts for 2006 through present were processed and added to this database. In 2020, the entire dataset (1973 - present) was standardized to
the newer, high resolution grid and is described in Yang et al. 2020.
About the raw data:
Original ice charts are provided in three forms: asci grid files, jpeg image files, and ArcGIS shapefiles. From 1973 through 1988, the source was
the Canadian Ice Service. Beginning with 1989, the source was the
U.S. National Ice Center, (NIC). Data from both Canadian and U.S.
sources is combined in NIC's daily products.
Files that align ascii grid data with location
and lake are here: geographic metadata
Ice Cover Forecasting
GLERL conducts research on ice cover forecasting on two different time scales: short-term (1-3 days) and seasonal. GLERL's short-term ice forecasting
is part of the Great Lakes Coastal Forecasting System, a model used by the National Ocean Service to predict wind, waves, currents, and more. These ice
nowcast and forecast products (concentration, thickness, velocity, and vessel icing) are still experimental but being transitioned to operations. GLERL's
seasonal ice cover forecast is based on statistical and physical analysis and is also experimental.
Short-term Ice Forecasting (1 to 3 days)
Great Lakes Coastal Forecasting System (GLCFS) is a short-term physical modeling framework for predicting waves, currents, water temperature, and ice. GLCFS uses observed and forecasted atmospheric conditions to predict ice conditions up to 3 days in the future. Ice forecast products under development include ice thickness, vessel icing, and ice velocity. The ice concentration output has been validated extensively against avaiable observations
(Anderson et al. 2019.)
The following links to the
pages which contain visual summaries of current Great Lakes ice conditions.
Seasonal Ice Cover Forecasting
Research at NOAA’s Great Lakes Environmental Research Laboratory (GLERL) has shown that the interannual variability of Great Lakes ice cover is heavily
influenced by four global weather patterns referred to as teleconnections: the North Atlantic Oscillation (NAO),
the Atlantic Multidecadal Oscillation (AMO), the El Nino/Southern Oscillation (ENSO) and the Pacific Decadal Oscillation (PDO). These teleconnection patterns impact Great Lakes
regional weather and ice cover by influencing the location of the westerly jet stream over North America
(Wang et. al, 2018; Bai and Wang 2012).
The position of the jet stream largely dictates the origin of the air masses (e.g. North Pacific or the arctic) that will reach the Great Lakes region as weather systems move
across the continent. The temperature and moisture content of these air masses play a key role in determining ice cover.
Note: For
official NOAA ice cover forecasts on seasonal to sub-seasonal scales, see the
US National Ice Center
Great Lakes Water Temperatures and Ice Cover - Frequently Asked Questions
What are the current Great Lakes surface water temperatures and what is the current extent of Great Lakes ice cover?
Current Conditions
Graphic displaying the current Great Lakes surface water temperatures and extent of ice cover as observed by NOAA Coastwatch's
Great Lakes Surface Environmental Analysis (GLSEA).
GLSEA is a digital map of the Great Lakes surface water temperature and
ice cover which is produced daily.
How does today's Great Lakes surface water temperatures and ice cover extent compare with the previous years?
When was ice cover the highest (or lowest) for each of the Great Lakes?
View the records* for Great Lakes Annual Ice Cover (percent) from 1973-2018 below:
|
Highest Annual Maximum Ice Cover (%) |
Year |
Lowest Annual Maximum Ice Cover (%) |
Year |
| Basin |
94.7 |
1979 |
11.9 |
2002 |
| Superior |
100 |
1996 |
8.5 |
2012 |
| Michigan |
93.1 |
2014 |
12.4 |
2002 |
| Huron |
98.2 |
1994 |
22.8 |
2012 |
| Erie |
100 |
1978, 1979, 1996 |
5.4 |
1998 |
| Ontario |
86.2 |
1979 |
1.9 |
2012 |
*See Table 1 from: Wang, J., J. Kessler, F. Hang, H. Hu, A.H. Clites, and P. Chu. Analysis of Great Lakes ice cover climatology: Winters 2012-2017. NOAA Technical Memorandum GLERL-171. NOAA Great Lakes Environmental Research Laboratory, Ann Arbor, MI, 24 pp. (2017). http://www.glerl.noaa.gov/pubs/tech_reports/glerl-171/tm-171.pdf
from: Wang, J, J. Kessler, F. Hang, H. Hu, A.H. Clites, and P. Chu. Great Lakes Ice Climatology Update of Winters 2012-2017: Seasonal Cycle, Interannual Variability,
Decadal Variability, and Trend for the Period 1973-2017
http://www.glerl.noaa.gov/pubs/tech_reports/glerl-170/tm-170.pdf
Why does Lake Ontario generally have the least ice cover of all the Great Lakes?
Lake Ontario's extreme depth (86 m average; 244 m maximum) translates to tremendous heat storage capacity.
It also has a smaller surface area for heat loss. In addition, cold air outbreaks from the northwest and west are
moderated by the waters of Lakes Superior, Michigan, and Huron. These factors combine to keep ice cover on Lake Ontario at a relatively low level most years.
When does ice cover peak on the Great Lakes?
Maximum ice cover on the lower lakes (like Lake Erie) normally occurs between mid-February and end of February.
Maximum ice cover on the upper lakes (like Lake Superior) normally occurs between end of February and early March.
Does more ice cover reduce evaporation and lead to higher water levels?
The relationship between ice cover, evaporation, and water levels is complex. Data on modeled evaporation shows that
this process peaks in the fall, before ice cover formation. In a severe ice cover year such as 2014, the thermal structure
of the lake could be impacted for the rest of the year, potentially reducing evaporation from the lakes next fall. Evaporation
and precipitation are the major drivers of seasonal water level changes in the Great Lakes.
Does more ice now mean cooler water temperatures this summer?
Ice extent plays a part in determining water temperature in the lakes later in the year, as incoming heat will have to melt
the ice before it warms the water below. However, meteorological conditions and heat storage in the lakes are also critical components
to the thermal cycle in the lakes.
How does blue ice form?
Sometimes blue ice develops on the Great Lakes. This is an unusual phenomenon in the Great Lakes that is usually short-lived.
What causes blue ice?
- Selective absorption by water/ice in the yellow/red part of the spectrum, so the reflected light is blue. Ice can also absorb orange and green light as light energy absorbed by the ice causes the water molecules to vibrate, which can lead to absorption of orange and green light.
- Ice that is very thick, compressed, and has a lack of bubbles and other inclusions, allows light to penetrate farther thus absorbing more of the longer wavelengths (colors). This leaves shorter wavelength blue light to reflect back or pass through the ice, making the ice look blue.
- In deep, mid-lake water, where chlorophyll content is low, the reflection of the water can make the ice appear even more blue.
