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Sunday, July 12, 2020 | History

2 edition of Investigation of the currents and density structure of Lake Erie found in the catalog.

Investigation of the currents and density structure of Lake Erie

James H. Saylor

Investigation of the currents and density structure of Lake Erie

by James H. Saylor

  • 329 Want to read
  • 33 Currently reading

Published by U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories in [Washington, D.C.?] .
Written in English

    Subjects:
  • Erie, Lake -- Temperature.

  • Edition Notes

    StatementJames H. Saylor, Gerald S. Miller.
    SeriesNOAA technical memorandum ERL GLERL -- 49.
    ContributionsMiller, Gerald S., Environmental Research Laboratories (U.S.)
    The Physical Object
    Paginationix, 80 p. :
    Number of Pages80
    ID Numbers
    Open LibraryOL17830375M

    Point itself, the waters of Lake Erie adjacent to it up to a depth of about 10 m, and the area enclosed by the Point and the year flood height on the north shore of Lake Erie from the Big Creek marsh to Turkey Point (Fig. ). The m depth contour is approximately Cited by: density ontario chad vertical ecology bogs sediment seasonal currents peat concentrations major lakes groundwater michigan lake basins baikal Post a Review. You can write a book review and share your experiences. Other readers will always be interested in your opinion of the books.

      The world fisheries are in a perilous situation with over 75% of stocks being either fully exploited or over exploited. Our ability to harvest fish with unprecedented effectiveness using the technological advances provided by the agents of globalization has put great stress on fish production and their ecosystems. A high demand for fisheries products around the world for nutrition, recreation. adjacent to Lake Erie lies in the Eastern Lake Section of the Central Lowlands Province, and is a relatively narrow zone consisting of a series of lake-parallel, low-relief ridges. Steep-sided, narrow valleys cut through these ridges into the underlying shales and siltstones and flow into Lake Size: 18MB.

    The harmful algal bloom (HAB) season is also long over in the region. The final Lake Erie HAB Bulletin was sent out on Oct. 11, as the Microcystis had declined in satellite imagery and toxins decreased to low detection limits in samples. In the seasonal assessment, sent out by NOAA’s Centers for Coastal Ocean Science on Oct. 26, it was determined that the season saw a relatively mild bloom. This archive presents a list of National Ocean Service Diving Deeper podcast titles, publication dates, audio (mp3) links, and transcripts for all episodes released between This podcast was retired in , replaced by the NOAA Ocean Podcast.


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Investigation of the currents and density structure of Lake Erie by James H. Saylor Download PDF EPUB FB2

Investigation of the currents and density structure of Lake Erie ix, 80 p. (OCoLC) Online version: Saylor, James H. Investigation of the currents and density structure of Lake Erie.

[Washington, D.C.?]: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, [] (OCoLC) Investigation of the currents and density structure of Lake Erie ix, 80 p.

(OCoLC) Material Type: Document, Government publication, National government publication, Internet resource: Document Type: Internet Resource, Computer File: All Authors / Contributors: James H Saylor; Gerald S Miller; Great Lakes Environmental Research Laboratory.

Lake Erie / ˈ ɪər i / (French: Lac Érié) is the fourth-largest lake (by surface area) of the five Great Lakes in North America, and the eleventh-largest globally if measured in terms of surface area.

It is the southernmost, shallowest, and smallest by volume of the Great Lakes and therefore also has the shortest average water residence its deepest point Lake Erie is feet (64 Coordinates: 42°12′N 81°12′W / °N.

Lakefloor geomorphology of western Lake Erie was discussed in a Investigation of the Currents and Density Structure of Lake Erie. NOAA Technical Memorandum no. ERL GLERL Investigation. Two-dimensional, time-dependent numerical models are used to predict the temperatures and currents in a stratified lake.

In this study, (1) essential features of the observed distributions of temperatures and currents in large, stratified lakes, especially Lake Erie, are reproduced, (2) the effects of various governing parameters such as heat flux to the water, wind stresses, and turbulence Cited by: shallow-water approximation, in which the lake geometries and water currents are large in the horizontal directions as compared to corresponding values in the vertical direction.

Indapamide is an indole derivative of chlorosulphonamide and a sulfamyl diuretic with antihypertensive activity. Indapamide may interact directly with the subunits of delayed rectifier potassium channels, thereby blocking both slow and rapid K+ (IKs and IKr) currents through the channels.

Through the homeostasis mechanism in balancing total ion concentration (Ca++, Na+), it reduces vascular. FWPCA Lake Erie Surveillance Data SummaryDl, GLR (). Gardner, W., Lee, G.F., Oxygenatlon of lake sediments, Int. Jour, of Air and Water Pollution, pp (). Gorham, E.

Observations on the formation and breakdown of the oxidized micro. The depth of this classical graben lake has recently been found to be in excess of m (Haffner et al., ) which would certainly have qualified it for inclusion. If the lake is always isothermal, as the preliminary data suggest, the ecology of its phytoplankton would make a doubly rewarding by: Area of circles are proportional to the number of angler days in Lake Superior - Lake Michigan - 5 Lake Huron - Lake Erie - 7 Lake Ontario - 2 2.

The data measure sport fishing effort, and are classified according to. In this study, water withdrawals and returns within the Ohio Lake Erie Basin were evaluated to determine their potential impact on the water quality of Lake Erie, and support a policy choice by the State of Ohio: whether or not the water quality impacts are sufficient to justify implementation of the relevant Section management measures.

Home > Journals > Journal of Coastal Research > Volume 33 > Issue 6. Numerical Modeling of Coastal Storms for Ice-Free and Ice-Covered Lake Erie. Ali Farhadzadeh, Jeffery Gangai. 33(6), Numerical oceanographic modeling, solitary wave, surface structure, fully nonlinear wave.

Read Abstract +. Lake Erie (French: Lac Érié) is the fourth-largest lake (by surface area) of the five Great Lakes in North America, and the eleventh-largest globally if measured in terms of surface is the southernmost, shallowest, and smallest by volume of the Great Lakes and therefore also has the shortest average water residence its deepest point Lake Erie is feet deep.

The fact that the temperature of maximum density of most lake waters is close to 4° C (39° F), whereas ice forms at temperatures close to 0° C in response to surface cooling, vertical mixing takes place.

When density increases with depth, the lake is said to be stable. Unstable conditions exist when density decreases with depth.

Sedimentologic, oceanographic, and hydraulic engineering publications on hyperpycnal flows claim that (1) river flows transform into turbidity currents at plunge points near the shoreline, (2) hyperpycnal flows have the power to erode the seafloor and cause submarine canyons, and, (3) hyperpycnal flows are efficient in transporting sand across the shelf and can deliver sediments into the Cited by: 8.

Because of renewed riparian interest stemming from the high Lake Erie water levels of the mids and mids and the need for a concise summary of previous studies, a review and a new assessment of the impact of the Niagara River's Chippawa Grass Island Pool on Lake Erie water levels was undertaken.

In the first section of this chapter, the main physical differences between large and small lakes are outlined, and the concepts of thermocline modelling are reviewed. Thereafter, we present a dynamical simulation of the vertical structure of density in Lake Constance as a case by: 6. 3 Environmental Processes, Behavior, and Toxicity of Diluted Bitumen.

INTRODUCTION. This chapter is concerned with what happens to crude oil after it is released from a pipeline, and with the potential environmental and ecological consequences of that release. Study of the Tide and Tidal Currents in the Bay of Bengal Based on Refined Simulations.

Predicting the Temporal Structure of the Atlantic Multidecadal Oscillation (AMO) for Agriculture Management in Mexico's Coastal Zone BOOK REVIEWS.

BOOK REVIEWS. William J. Neal. 35(1),(1 January ). Scientists and technical staff within the USGS Coastal and Marine Geology Program study coastal and ocean resources from shorelines and estuaries to the continental shelf and deep sea, providing expertise, tools, products, and data that address and inform a broad array of resource challenges facing our Nation.

Sponsored by Coastal Zone Management Committee Waves and Wave Forces Committee, and Rubble Mound Structure Committee of Coasts, Oceans, Ports, and River Institute of ASCE.

This collection contains papers that explore major advances in wave measurement and quantification of ocean and lake waves, including technical knowledge and applications.Returning to a Healthy Lake: Lake Erie Biodiversity Conservation Strategy.

Technical Report. A joint publication of The Nature Conservancy, Nature Conservancy of Canada, and Michigan Natural Features Inventory. pp. with Appendices. Acknowledgements.A dissolved oxygen budget model for Lake Erie in summer.

Freshwater Biology 15(6): Academic Journal: Ivey, G.N. and Patterson, J.C. () A model of the vertical mixing in Lake Erie in summer. Limnology and Oceanography 29(3): Download: Ivey, G.N. and Patterson, J.C. A model of the vertical mixing in Lake Erie in summer.