Freezing of surface water begins a unique hydrologic period in cold-region climates, one where the resultant ice covers create lotic and lentic environments that are distinctly different physically, chemically and biologically from their open-water counterparts. Many such differences result directly
On the cause of the formation of ice at the bottom of rivers and lakes
โ Scribed by W. J. Altberg
- Publisher
- John Wiley and Sons
- Year
- 2007
- Tongue
- English
- Weight
- 379 KB
- Volume
- 49
- Category
- Article
- ISSN
- 0035-9009
No coin nor oath required. For personal study only.
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