00000nam 2200000za 4500 9.850787 CaOODSP 20241203113642 cr ||||||||||| 180126s1986 onca|||fob f000 0 eng d CaOODSP eng eng fre n-cn-on En13-5/86-201E-PDF Boyce, F. M. A study of inertial frequency current oscillation in the central basin of Lake Erie [electronic resource] / by F.M. Boyce, F. Chiocchio. [Burlington, Ont.] : [National Water Research Institute], [1986]. 1 v. (various pagings) : ill. NWRI ; # 86-201 Digitized edition from print [produced by Environment and Climate Change Canada]. Includes bibliographical references. "Circularly polarized, clockwise rotating currents at or near the local inertial frequency are a common occurrence in the offshore regions of the Great Lakes during the stratified season. Often they are the most energetic component of water motion and because they are associated with large vertical shears supported by the stably stratified layers, they may modify, through shear-generated turbulence, the very stratification they depend on. ... This paper focusses on a singlular feature of the Central Basin current records, the occurrence of a marked maximum of inertial frequency motion in July. Just above the seasonal thermocline. After review of the relevant theory for the generation of inertial frequency motion, the authors propose a simple model that extends Ekman theory to the case of surface wind forcing and subsurface forcing by the pressure gradients (or surface slope) due to wind set-up"--Exec. summary. Includes executive summary in French. gccst Water gccst Hydrology Chiocchio, F. Canada. Environment Canada. National Water Research Institute (Canada) NWRI contribution ; no. 86-201 (CaOODSP)9.844121 PDF 3.82 MB https://publications.gc.ca/collections/collection_2018/eccc/En13-5-86-201-eng.pdf