Tidal Propagation in Chesterfield Inlet, N.W.T.

Chesterfield Inlet drains an area of 290,000 km^2, between Great Slave Lake and northern Hudson Bay, of predominantly continuous permafrost terrain. The 220-kilometre-long inlet may be used as an important navigation link to Baker Lake and potential pipeline sites. The inlet forms a complex network...

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Bibliographic Details
Main Author: Budgell, William Paul
Other Authors: James, W., Civil Engineering
Format: Thesis
Language:English
Published: 1976
Subjects:
Online Access:http://hdl.handle.net/11375/17521
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record_format openpolar
spelling ftmcmaster:oai:macsphere.mcmaster.ca:11375/17521 2023-05-15T15:35:54+02:00 Tidal Propagation in Chesterfield Inlet, N.W.T. Budgell, William Paul James, W. Civil Engineering 1976-09 http://hdl.handle.net/11375/17521 en_US eng http://hdl.handle.net/11375/17521 Chesterfield Inlet Hudson Bay tidal water levels Thesis 1976 ftmcmaster 2022-03-22T21:13:03Z Chesterfield Inlet drains an area of 290,000 km^2, between Great Slave Lake and northern Hudson Bay, of predominantly continuous permafrost terrain. The 220-kilometre-long inlet may be used as an important navigation link to Baker Lake and potential pipeline sites. The inlet forms a complex network and is characterized by strong tidal forcing. A one-dimensional numerical model, using a weighted, implicit, finite difference scheme, was modified for application to the network. Sparse matrix techniques were incorporated into the model to speed Gaussian Elimination in the solution of the equations. Tidal constituents, derived from admittance calculations, were used to predict water levels at eight tide gauge locations. Tidal predictions at Sandpiper Island were used as the downstream boundary condition for the numerical model, while tidal predictions at the other gauge locations were used in the model calibration. The observed and model-computed water levels are in good agreement over the lower half of the inlet. Appreciable differences between the observed and computed values were encountered in the upper reaches. Although some of these discrepancies are attributable to errors in the upstream boundary condition and schematization of the model, there is evidence to suggest that time and range errors may exist in some of the recorded tidal data. The variation in the phase and amplitude of the tide throughout the inlet is determined through an examination of the tidal constituents and the model results. Power spectra of the observed and model-predicted water levels reveal that nonlinear interactions of the major tidal constituents take place in the upper portion of the inlet. Thesis Master of Engineering (MEngr) Thesis Baker Lake Chesterfield Inlet Great Slave Lake Hudson Bay permafrost MacSphere (McMaster University) Hudson Bay Hudson Great Slave Lake ENVELOPE(-114.001,-114.001,61.500,61.500) Chesterfield Inlet ENVELOPE(-90.705,-90.705,63.342,63.342) Long Inlet ENVELOPE(-132.278,-132.278,53.202,53.202)
institution Open Polar
collection MacSphere (McMaster University)
op_collection_id ftmcmaster
language English
topic Chesterfield Inlet
Hudson Bay
tidal
water levels
spellingShingle Chesterfield Inlet
Hudson Bay
tidal
water levels
Budgell, William Paul
Tidal Propagation in Chesterfield Inlet, N.W.T.
topic_facet Chesterfield Inlet
Hudson Bay
tidal
water levels
description Chesterfield Inlet drains an area of 290,000 km^2, between Great Slave Lake and northern Hudson Bay, of predominantly continuous permafrost terrain. The 220-kilometre-long inlet may be used as an important navigation link to Baker Lake and potential pipeline sites. The inlet forms a complex network and is characterized by strong tidal forcing. A one-dimensional numerical model, using a weighted, implicit, finite difference scheme, was modified for application to the network. Sparse matrix techniques were incorporated into the model to speed Gaussian Elimination in the solution of the equations. Tidal constituents, derived from admittance calculations, were used to predict water levels at eight tide gauge locations. Tidal predictions at Sandpiper Island were used as the downstream boundary condition for the numerical model, while tidal predictions at the other gauge locations were used in the model calibration. The observed and model-computed water levels are in good agreement over the lower half of the inlet. Appreciable differences between the observed and computed values were encountered in the upper reaches. Although some of these discrepancies are attributable to errors in the upstream boundary condition and schematization of the model, there is evidence to suggest that time and range errors may exist in some of the recorded tidal data. The variation in the phase and amplitude of the tide throughout the inlet is determined through an examination of the tidal constituents and the model results. Power spectra of the observed and model-predicted water levels reveal that nonlinear interactions of the major tidal constituents take place in the upper portion of the inlet. Thesis Master of Engineering (MEngr)
author2 James, W.
Civil Engineering
format Thesis
author Budgell, William Paul
author_facet Budgell, William Paul
author_sort Budgell, William Paul
title Tidal Propagation in Chesterfield Inlet, N.W.T.
title_short Tidal Propagation in Chesterfield Inlet, N.W.T.
title_full Tidal Propagation in Chesterfield Inlet, N.W.T.
title_fullStr Tidal Propagation in Chesterfield Inlet, N.W.T.
title_full_unstemmed Tidal Propagation in Chesterfield Inlet, N.W.T.
title_sort tidal propagation in chesterfield inlet, n.w.t.
publishDate 1976
url http://hdl.handle.net/11375/17521
long_lat ENVELOPE(-114.001,-114.001,61.500,61.500)
ENVELOPE(-90.705,-90.705,63.342,63.342)
ENVELOPE(-132.278,-132.278,53.202,53.202)
geographic Hudson Bay
Hudson
Great Slave Lake
Chesterfield Inlet
Long Inlet
geographic_facet Hudson Bay
Hudson
Great Slave Lake
Chesterfield Inlet
Long Inlet
genre Baker Lake
Chesterfield Inlet
Great Slave Lake
Hudson Bay
permafrost
genre_facet Baker Lake
Chesterfield Inlet
Great Slave Lake
Hudson Bay
permafrost
op_relation http://hdl.handle.net/11375/17521
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