Freshwater ice is a major component of the terrestrial
cryosphere. It affects an extensive portion of the global
hydrologic system, including the rivers and lakes found
throughout high-latitude and alpine areas, mainly in the
Northern Hemisphere. Seasonal ice cover can develop as
far south as 33°N in North America and 26°N in Eurasia
producing effects on 7 of the world’s 15 largest rivers
and 11 of the 15 largest lakes.
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