Evaporation from Lake Erie
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Evaporation from Lake Erie by J. A. Derecki

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Published by U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, for sale by the Supt. of Docs., U. S. Govt. Print. Off. in Boulder, Colo, Washington .
Written in English


  • Evaporation (Meteorology) -- Erie, Lake.,
  • Erie, Lake.

Book details:

Edition Notes

Bibliography: p. 61-62

StatementJan A. Derecki
SeriesNOAA technical report ERL -- 342. -- GLERL -- 3, GLERL contribution ; no. 28, NOAA technical report ERL -- 342., NOAA technical report ERL -- 3., GLERL contribution -- no. 28.
ContributionsEnvironmental Research Laboratories (U.S.), Great Lakes Environmental Research Laboratory.
The Physical Object
Paginationvi, 84 p. :
Number of Pages84
ID Numbers
Open LibraryOL13600781M

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evaporation goes to zero and the water level would increase from the normal October level.! Keeping in mind that this tool is loosely based on Lake Erie, describe how Lake Superior levels might behave differently during January. (Note: more of Lake Erie would be covered in ice than Lake Superior)!   Lake Erie’s water level Wednesday was at feet above sea level – a slight dip from last month’s average of feet, which set the lake’s all-time record high. We’re still Erie Ontario The volume of Lake Superior is over 50% of the total Great Lakes volume compared to the evaporation where it is much less in comparison to the other lakes. Lake Erie on the other hand has a very small volume compared to the other lakes but a high evaporation rate. Why? Volume Evaporation Example 2 of student data comparison for #5.   Lake St. Clair, which connects Lakes Huron and Erie, also set its highest level on record for those two months. AD In August, Lake Superior tied its record high, while lakes St. Clair and Erie.

Home | The Climate Workspace.   Evaporation drives the water cycle. Evaporation from the oceans is the primary mechanism supporting the surface-to-atmosphere portion of the water cycle. After all, the large surface area of the oceans (over 70 percent of the Earth's surface is covered by the oceans) provides the opportunity for large-scale evaporation to occur.   Lisa Borre is a lake conservationist, writer and avid sailor. A native of the Great Lakes region, she served as coordinator of the Lake Champlain Basin Program in the s and co-founded LakeNet, a world lakes network that was active from She is now a Senior Research Specialist at the Cary Institute of Ecosystem Studies and an active member of the Global Lake Ecological .   Hydrologic data of Lake Eire were obtained from the Great Lakes Environmental Research Laboratory, including water temperature, precipitation, lake evaporation, ice cover days, ice melt date, and the water supply (precipitation + runoff - evaporation) (NOAA GLERL ). The annual averages across the whole lake of the above factors in Lake Erie.

  They interviewed Lake Erie experts, from professional historians to long-time residents. The result is a remarkable portrait of daily life, industry and commerce on this dynamic Great Lake. The opening of the Erie Canal in connected the Hudson River to the Great Lakes and unleashed the financial potential of the American interior. The Reviews: 6. levels by increasing rates of evaporation and causing lake ice to form later than usual (see the Lake Ice indicator), which extends the season for evaporation. 1 Lower water levels in the Great Lakes forced ships to reduce their cargo tonnage by 5 to 8 percent between .   This book was much more interesting than I anticipated. I live on Lake Erie, so when I saw the book at the library I picked it up. The Great Lakes are not really lakes, they are inland fresh water seas. If you’ve ever stood on the shore of one, you know what I’m talking about/5(K). 1. Lake Erie basin. 5 2. Lake Erie evaporation by water budget method, 14 3. Lake Erie evaporation by mass transfer method MT-1, 24 4. Lake Erie evaporation by mass transfer method MT-2, 26 5. Comparison of water budget and mass transfer evapora­ tion from Lake Erie, 27 6.