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A physical oceanographic study of the nearshore zone at Newport, Oregon

ScholarsArchive at Oregon State University

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Title A physical oceanographic study of the nearshore zone at Newport, Oregon
Names Keene, Donald Frederick (creator)
Neal, Victor T. (advisor)
Date Issued 1971-05-10 (iso8601)
Note Graduation date: 1971
Abstract The nearshore zone at Newport, Oregon was studied during the
period September, 1968 to August, 1969. Particular emphasis was
placed on those physical factors affecting the distribution of pulp mill
wastes discharged within the study area (referred to as Yaquina Bight
in this thesis). Temperatures and seawater samples were obtained
from a small boat. Nearshore and longshore currents were measured
from a light aircraft using dye markers and drift bottles, respectively.
Winds, waves and tides were measured from shore stations. This
thesis describes the waters of the bight throughout the year and how
they are affected by the effluent of the pulp mill and by seasonal
oceanic and local conditions.
The waters within Yaquina bight reflect the large scale seasonal
oceanic conditions which occur off the Oregon coast, i.e., the summer
upwelling season and the winter Davidson current season. On a
smaller scale the waters of the bight are influenced by the pulp mill
effluent. The effluent mixes rapidly with seawater and the mixture is
generally colder, Less saline and less dense than the surrounding
surface waters. The dissolved oxygen content of the mixture is also
lower than the surrounding seawater. The analyses of different
effluent-seawater dilutions indicated that the low oxygen content is not
caused by chemical reactions of the effluent.
Measurements of current velocity at a depth of two meters were
regressed on concurrent measurements of the prevailing wind, waves
and tide. The local wind of the hour previous to the time of observation
accounted for 56.9% of the variance of the currents flowing in the
north-south direction at the outfall station. The wind also accounted
for 26.6% of the variance of the east-west flowing currents at the
outfall station. Currents at other stations within the bight were also
analyzed. The unexplained variance of the currents at the other
stations was higher than those at the outfall station.
Deviations between the surface current direction and the current
direction at two meters ware apparently related to the season and to
the wind speed. At wind speeds greater than seven meters per second
the angle between the two current directions approached zero. The
data did not indicate that the deeper current flowed to the left or the
right of the surface current as a function of wind speed. However,
during the upwelling season the current at two meters was observed to
flow consistently to the left of the surface current.
Genre Thesis/Dissertation
Topic Waste disposal in the ocean
Identifier http://hdl.handle.net/1957/22013

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