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Even the most stable cover types (hardwood trees and herbs) had low absolute stability, with over 65% of their plots changing to another cover type by 1993.
George Leshkevich, who tracks current ice conditions for the Great Lakes Environmental Research Laboratory told the Milwaukee Journal Sentinel the sprawling ice cover could give the the fishing season a boost since "some species of fish need a stable cover of ice to protect their spawning beds from winter storms".
Species number of woody plants>1 m height in the regeneration forests was less variable (range 17 24, n = 5 plots) compared to the forest with stable cover (range 8 19, n = 4 plots) (Table 1).
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On larger lakes where the wind prevents a stable ice cover from initially forming, large floes may be formed, and the ice cover may ultimately stabilize as these floes freeze together, sometimes forming large ridges and piles of ice.
In some cases particularly before a stable ice cover forms wind mixing may be sufficient to entrain ice particles and supercooled water to considerable depths.
In some large lakes, such as Lake Erie in North America, wind effects are so great that a stable ice cover rarely forms over the entire lake, and the water is very near 0° C throughout the winter.
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In addition, in very deep lakes the thermal reserve built up during summer heating may be too large to allow cooling to the freezing point, or the action of wind over large fetches may prevent a stable ice cover from forming.
A large part of the Great Plains is in relatively stable land cover.
An increase in erosion and run-off processes in association with decreasing or stable vegetation cover was observed over shallow soils, which occupy 30% of the area.
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Since I tried Ludwig back in 2017, I have been constantly using it in both editing and translation. Ever since, I suggest it to my translators at ProSciEditing.

Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com