2 edition of Lake Ontario beginning-of-month water levels and monthly rates of change of storage found in the catalog.
Lake Ontario beginning-of-month water levels and monthly rates of change of storage
Frank H. Quinn
by U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, [Great Lakes Environmental Research Laboratory] in Boulder, Colo
Written in English
|Statement||Frank H. Quinn, Jan A. Derecki ; [Great Lakes Environmental Research Laboratory].|
|Series||NOAA technical report -- ERL 365-GLERL 10, GLERL contribution -- no. 10|
|Contributions||Derecki, J. A., Great Lakes Environmental Research Laboratory., Environmental Research Laboratories (U.S.)|
|The Physical Object|
|Pagination||iv, 27 p. :|
|Number of Pages||27|
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Additional Physical Format: Online version: Quinn, Frank H. Lake Ontario beginning-of-month water levels and monthly rates of change of storage. Boulder, Colo.: Environmental Research Laboratories ; Washington: for sale by the Superintendent of Documents U.S. Government Printing Office Energy balance of Lake Ontario.
Proceedings, IFYGL Symposium, 55th Annual Meeting of the American Geophysical Union, National Oceanic and Atmospheric Administration, Rockville, MD, (). QUINN, F.H. Lake Huron beginning-of-month water levels and monthly rates of change of storage. d Cumulative change in lake storage August maximum monthly average Lake Ontario water levels using November levels for all Great Lakes, a non-linear response to the wintertime Niño index.
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environmental protection agency gulf breeze, florida Daily Great Lakes and Seaway Shipping News Archive, new stories and photos from July Bay City - On Tuesday strong southwestern winds and low water levels made for a series of events to occur leading up to the closing of the Saginaw River to navigation for a short period of time connecting Lake Ontario to the Atlantic Ocean, had.
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Soil is a potential water pollutant because (1) as sediment its mass volume often reduces stream and lake capacities; (2) it can cause high levels of turbidity and settle out on stream bottoms upsetting the stream or lake ecosystem; and (3) sediment can be associated with adsorbed substances which are transported on soil particles, The.
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the water input to the aquifers, and d controls the mean residence time of. water in groundwater storage. Parameter c partitions ' runoff into its. direct and indirect components. The reciprocal of parameter d is the. mean residence time of water in aquifers.
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