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Minimizing Long-Term Wind Set-Up Errors in Estimated Mean Erie and Superior Lake Levels

By Croley Ii, Thomas E.

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Book Id: WPLBN0000662000
Format Type: PDF eBook
File Size: 636.74 KB.
Reproduction Date: 2005



Title: Minimizing Long-Term Wind Set-Up Errors in Estimated Mean Erie and Superior Lake Levels  
Author: Croley Ii, Thomas E.
Volume:
Language: English
Subject: Science., Ecology & environment, National Oceanic and Atmospheric Administration (U.S.)
Collections: National Oceanographic Data Center
Historic
Publication Date:
Publisher: Government Reference Publication

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Croley Ii, T. E. (n.d.). Minimizing Long-Term Wind Set-Up Errors in Estimated Mean Erie and Superior Lake Levels. Retrieved from https://gutenberg.cc/


Excerpt
Excerpt: Minimizing Long-Term Wind Set-Up Errors In Estimated Mean Erie And Superior Lake. Errors in computed mean lake levels, caused by wind set-up, are estimated from linearized hydrodynamic shallow-water equations applied to Lakes Erie and Superior for historical and current gage networks. Observations of maximum unit error (that results from a unit wind stress) with each of the historical networks and with the current network are consistent with lake orientation and network placement considerations. Optimum network gage selections are made from the 16 available Lake Erie gages to minimize mean square set-up error estimated over one season's wind data, mean square total error estimated from daily data for 12 years, and mean square total error with constraints on the network size. Optimum network gage selections for Lake Superior are made from the 10 available gages to minimize mean square total error estimated from 12 years of daily data with and without constraints on the network size. It is not possible to eliminate wind set-up errors in mean lake levels if Thiessen weights must be used (although errors can be kept quite small); without this constraint, wind set-up errors can be eliminated from mean lake level computations. This allows selection of the weights that minimize other types of errors. The differences in net basin supply and lake volume computations that result by using optimum weights instead of Thiessen weights appear significant on both Lakes Erie and Superior.

Table of Contents
CONTENTS PAGE ABSTRACT....................................................................l 1. 2. 3. 4. 5. 6. 7. 8. 9. 10. 11. 12. 13. 14. INTRODUCTION .......................................................... 1 LAKE ERIE ............................................................. 2 LONG-TERM LAKE ERIE SET-UP ERROR ...................................... 4 MINIMUM SET-UP ERROR FOR LAKE ERIE .................................... 8 TOTAL ERROR FOR LAKE ERIE ............................................ 11 MINIMUM TOTAL ERROR FOR LAKE ERIE .................................... 14 SPATIAL-OPTIMUM AND THIESSEN WEIGHTING DIFFERENCES FOR LAKE ERIE ..... 21 LAKE SUPERIOR ........................................................ 25 LONG-TERM LAKE SUPERIOR SET-UP ERROR ................................. 26 MINIMUM TOTAL ERROR FOR LAKE SUPERIOR ................................ 29 SPATIAL-OPTIMUM AND THIESSEN WEIGHTING DIFFERENCES FOR LAKE SUPERIOR ........................................................ 31 NET BASIN SUPPLY COMPARISONS ......................................... 35 smMARY .............................................................. 38 REFERENCES ........................................................... 40 iii

 

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Science., Ecology & environment, National Oceanic and Atmospheric Administration (U.S.)


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