scholarly journals Historical Trends, Drivers, and Future Projections of Ice Phenology in Small North Temperate Lakes in the Laurentian Great Lakes Region

Water ◽  
2018 ◽  
Vol 10 (1) ◽  
pp. 70 ◽  
Author(s):  
Bailey Hewitt ◽  
Lianna Lopez ◽  
Katrina Gaibisels ◽  
Alyssa Murdoch ◽  
Scott Higgins ◽  
...  
Keyword(s):  
Great Lakes ◽  
Laurentian Great Lakes ◽  
Great Lakes Region ◽  
Temperate Lakes ◽  
Historical Trends ◽  
Future Projections ◽  
North Temperate Lakes ◽  
Ice Phenology

scholarly journals Spatial analysis of ice phenology trends across the Laurentian Great Lakes region during a recent warming period

2007 ◽  
Vol 52 (5) ◽  
pp. 2013-2026 ◽  
Author(s):  
Olaf P. Jensen ◽  
Barbara J. Benson ◽  
John J. Magnuson ◽  
Virginia M. Card ◽  
Martyn N. Futter ◽  
...  
Keyword(s):  
Spatial Analysis ◽  
Great Lakes ◽  
Laurentian Great Lakes ◽  
Great Lakes Region ◽  
Recent Warming ◽  
Warming Period ◽  
Ice Phenology

A 900-year record of effective moisture in the Laurentian Great Lakes region

2021 ◽  
Vol 270 ◽  
pp. 107174
Author(s):  
R.M. Doyle ◽  
Z. Liu ◽  
J.T. Walker ◽  
R. Hladyniuk ◽  
K.A. Moser ◽  
...  
Keyword(s):  
Great Lakes ◽  
Laurentian Great Lakes ◽  
Great Lakes Region ◽  
Effective Moisture

scholarly journals Climatic-change implications from long-term (1823-1994) ice records for the Laurentian Great Lakes

1995 ◽  
Vol 21 ◽  
pp. 383-386 ◽  
Author(s):  
R.A. Assel ◽  
D.M. Robertson ◽  
M.H. Hoff ◽  
J.H. Selgeby
Keyword(s):  
Great Lakes ◽  
Climatic Changes ◽  
The Other ◽  
Laurentian Great Lakes ◽  
Great Lakes Region ◽  
Lake Mendota ◽  
Air Temperatures ◽  
The 1960S ◽  
Different Parts

Long-term ice records (1823-1994) from six sites in different parts of the Laurentian Great Lakes region were used to show the type and general timing of climatic changes throughout the region. The general timing of both freeze-up and ice loss varies and is driven by local air temperatures, adjacent water bodies and mixing, and site morphometry. Grand Traverse Bay and Buffalo Harbor represent deeper-water environments affected by mixing of off-shore waters; Chequamegon Bay, Menominee, Lake Mendota, and Toronto Harbor represent relatively shallow-water, protected environments. Freeze-up dates gradually became later and ice-loss dates gradually earlier from the start of records to the 1890s in both environments, marking the end of the “Little lce Age”. After this, freeze-up dates remained relatively constant, suggesting little change in early-winter air temperatures during the 20th century. Ice-loss dates at Grand Traverse Bay and Baffalo Harbor but not at the other sites became earlier during the 1940s and 1970s and became later during the 1960s. The global warming of the 1980s was marked by a trend toward earlier ice-loss dates in both environments.

Toxicological significance of mercury in yellow perch in the Laurentian Great Lakes region

2012 ◽  
Vol 161 ◽  
pp. 350-357 ◽  
Author(s):  
James G. Wiener ◽  
Mark B. Sandheinrich ◽  
Satyendra P. Bhavsar ◽  
Joseph R. Bohr ◽  
David C. Evers ◽  
...  
Keyword(s):  
Great Lakes ◽  
Yellow Perch ◽  
Laurentian Great Lakes ◽  
Great Lakes Region ◽  
Toxicological Significance

Lake Ice phenology of small lakes: Impacts of climate variability in the Great Lakes region

2011 ◽  
Vol 76 (3-4) ◽  
pp. 166-185 ◽  
Author(s):  
Vimal Mishra ◽  
Keith A. Cherkauer ◽  
Laura C. Bowling ◽  
Matthew Huber
Keyword(s):  
Climate Variability ◽  
Great Lakes ◽  
Great Lakes Region ◽  
Small Lakes ◽  
Lake Ice ◽  
Ice Phenology
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