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Articles 2551 - 2580 of 2652
Full-Text Articles in Oceanography and Atmospheric Sciences and Meteorology
Volume 3, Number 10 (October 1979), The Solar Ocean Energy Liaison
Volume 3, Number 10 (October 1979), The Solar Ocean Energy Liaison
The OTEC Liaison
No abstract provided.
Volume 3, Number 9 (September 1979), The Solar Ocean Energy Liaison
Volume 3, Number 9 (September 1979), The Solar Ocean Energy Liaison
The OTEC Liaison
No abstract provided.
An Analysis Of Bathymetric Change In Lower Chesapeake Bay, John C. Ludwick
An Analysis Of Bathymetric Change In Lower Chesapeake Bay, John C. Ludwick
OES Faculty Publications
The purposes of the work-reported in this document are (a) to determine the magnitudes and patterns of water-depth changes in lower Chesapeake Bay within a control area centered on Thimble Shoal Channel; (b) to interpret these changes, insofar as possible, in terms of sediment movements and/or bed erosion and lateral shifting of large shoals and tidal current channels; and (c) to .deduce the relationship of these changes, insofar as possible, to changes in the Chesapeake Bay shoreline from Willoughby Spit to the area of Cape Henry. Virginia.
Volume 3, Number 8 (August 1979), The Solar Ocean Energy Liaison
Volume 3, Number 8 (August 1979), The Solar Ocean Energy Liaison
The OTEC Liaison
No abstract provided.
Volume 3, Number 7 (July 1979), The Solar Ocean Energy Liaison
Volume 3, Number 7 (July 1979), The Solar Ocean Energy Liaison
The OTEC Liaison
No abstract provided.
Feeding Morphologies And Distribution Patterns Of Marine Cladocera In The Lower Chesapeake Bay, Sandra Layne Gilchrist
Feeding Morphologies And Distribution Patterns Of Marine Cladocera In The Lower Chesapeake Bay, Sandra Layne Gilchrist
OES Theses and Dissertations
Temporal and spatial distributions of marine cladocera in the lower Chesapeake Bay estuary were observed over a year-long sampling period. The distributions of cladoceran species throughout the Bay were studied in relation to temperature and salinity. A survey of the species over the entire Bay is included to establish distribution patterns of the various species during a short time period.
Theoretical mathematical principles were used to predict feeding abilities of the Bay species. Mouthparts are described qualitatively and quantitatively to infer function. A mandibular index developed by Itoh (1970) was revised and employed in evaluating feeding methods interspecifically and interspecifically. …
The Spatial And Temporal Distribution Of Fish Eggs And Larvae In Hempstead Bay Estuary, Joseph Adelard Lessard
The Spatial And Temporal Distribution Of Fish Eggs And Larvae In Hempstead Bay Estuary, Joseph Adelard Lessard
OES Theses and Dissertations
The ichthyoplankton of Hempstead Bay estuary was sampled from December 1972 to mid March 1974. Eleven stations were sampled by towing a 0.5 meter diameter plankton net. Eggs were most abundant during June and July with an average concentration calculated to be above 5,500/100m3. Egg densities were the lowest during the fall and winter. Larvae were most frequently taken from March through July with densities varying greatly among the samples. The eggs of Brevoortia tyrannus, Anchoa mitchilli, Tautoga onitis, Tautogolabrus adspersus, and Scophthalmus aguosus and the larvae of Menidia menidia, Ammodvtes hexapterus and Pseudopleuronectes americanus constituted most …
Volume 3, Number 6 (June 1979), The Solar Ocean Energy Liaison
Volume 3, Number 6 (June 1979), The Solar Ocean Energy Liaison
The OTEC Liaison
No abstract provided.
Volume 3, Number 5 (May 1979), The Otec Liaison
Volume 3, Number 5 (May 1979), The Otec Liaison
The OTEC Liaison
No abstract provided.
Volume 3, Number 4 (April 1979), The Otec Liaison
Volume 3, Number 4 (April 1979), The Otec Liaison
The OTEC Liaison
No abstract provided.
Production Of A Population Of The Stout Razor Clam (Tagelus Plebeius Solander) In A Virginia Estuary, Mark James Grussendorf
Production Of A Population Of The Stout Razor Clam (Tagelus Plebeius Solander) In A Virginia Estuary, Mark James Grussendorf
OES Theses and Dissertations
The annual net secondary production of the stout razor clam, Tagelous plebeius, was estimated at three sites on an intertidal sand flat at Lynnhaven Inlet, Virginia. Samples were taken at six week intervals for one year. The range of net production (P), mean annual biomass (B), and P/B ratios was 18.3-28.7 g m-2year-1, 27.2-53.3 g m-2, and 0.54-0.67, respectively. The total biomass did not show significant seasonal variation though differences between sites were significant. Production varied temporally but was not significantly different between sites.
Turbulence Spectra In A Well-Mixed Estuary, Jong Yul Chung
Turbulence Spectra In A Well-Mixed Estuary, Jong Yul Chung
OES Theses and Dissertations
This dissertation is an attempt to determine and describe some of the turbulent process in a well-mixed estuary. The processes are identified by the study of turbulent velocity fluctuations. These velocity records have been analyzed using standard digital methods to obtain spectral density, spectral energy, and cross-spectra of velocity. In order to study the generation and transfer of the turbulent moment and energy, and the intermittent nature of the so-called "Bursting or "ejections and sweeps," the distribution of u, v, w, and the Reynolds stress has been studied.
Volume 3, Number 3 (March 1979), The Otec Liaison
Volume 3, Number 3 (March 1979), The Otec Liaison
The OTEC Liaison
No abstract provided.
Volume 3, Number 2 (February 1979), The Otec Liaison
Volume 3, Number 2 (February 1979), The Otec Liaison
The OTEC Liaison
No abstract provided.
Volume 3, Number 1 (January 1979), The Otec Liaison
Volume 3, Number 1 (January 1979), The Otec Liaison
The OTEC Liaison
No abstract provided.
Alkalinity And Ph In The Southern Chesapeake Bay And The James River Estuary, George T. F. Wong
Alkalinity And Ph In The Southern Chesapeake Bay And The James River Estuary, George T. F. Wong
OES Faculty Publications
The ranges of alkalinity and pH in the southern Chesapeake Bay and the James River estuary were 2.25 meq·liter−1 at 32‰ to
Geology Of The Mafic/Ultramafic Transition, Table Mountain, Western Newfoundland, Suzanne O'Connell
Geology Of The Mafic/Ultramafic Transition, Table Mountain, Western Newfoundland, Suzanne O'Connell
Geology Theses and Dissertations
A thin (<200 m.) mafic suite and well developed mafic/ultramafic transition zone are exposed above a flat lying peridotite contact on northwestern Table Mountain. The igneous layering and sedimentary features indicate mineral deposition under conditions which promoted adcumulate growth, were capable of minor transport, and were subjected to at least minor tectonic activity during consolidation. Feldspathic,. mafic, and ultramafic dikes and veins cross-cut the layering. Microscopic futures indicate deformation at elevated temperature and/or low strain rates. Deformation is best developed within the transition zone, but cataclastic zones are most common in the hornblende gabbros. Orientations of layering, foliation, and lineation indicate a variable mafic/ultramafic transition and macroscopic folding. Geometric analysis indicates three distinct fold axis orientations: an east-west horizontal fold axis, a northeast trending modestly plunging axis, and a vertical though poorly defined axis. Such features demonstrate that an apparently simple contact relationship may be extremely complex. This has important implications for ocean floor accretion. The relatively simple ocean floor seismic stratigraphy masks very complex petrological and structural processes. Such processes may involve deposition in an actively convecting magma chamber with a differentially subsiding wedge (Dewey and Kidd, 1977), in which folding occurs in response to the steepening angle between the cumulate banding and the base of the magma chamber. The instability is enhanced by the different accumulation rates and densities of the minerals involved. The lineation may originally be a sedimentary feature indicative of transport direction from the convection cell, and perpendicular to the compressive stress which produced. the folding. The different orientations of lineations and fold axes could be produced by rotation of the ocean crustal blocks during lateral transport along the ocean floor and/or obduction. Further detailed study of ophiolite complexes will continue to shed light upon the nature and development of oceanic crust.
Paleoclimatic Implications Of Oxygen Isotope And Sedimentological Study Of Late Miocene And Early Pliocene Sediments From The South Atlantic, Western Indian Ocean, And The Gulf Of Aden, Kathryn M. Scanlon
Geology Theses and Dissertations
Previous work by many authors has implied that the Antarctic ice sheet underwent a major expansion in the latest Miocene. It was intended in the present study to use the oxygen isotope event, which could be expected to accompany this glacial expansion, as a stratigraphic marker to aid in the correlation of several DSDP Sites. Samples were taken at approximately 100,000 year intervals throughout the latest Miocene and early Pliocene sections at Sites 237 and 249 in the western Indian Ocean, Site 360 in the South Atlantic and Site 231 in the Gulf of Aden. Oxygen isotope analyses were done …
Volume 2, Number 12 (December 1978), The Otec Liaison
Volume 2, Number 12 (December 1978), The Otec Liaison
The OTEC Liaison
No abstract provided.
Volume 2, Number 11 (November 1978), The Otec Liaison
Volume 2, Number 11 (November 1978), The Otec Liaison
The OTEC Liaison
No abstract provided.
Volume 2, Number 10 (October 1978), The Otec Liaison
Volume 2, Number 10 (October 1978), The Otec Liaison
The OTEC Liaison
No abstract provided.
Volume 2, Number 9 (September 1978), The Otec Liaison
Volume 2, Number 9 (September 1978), The Otec Liaison
The OTEC Liaison
No abstract provided.
Volume 2, Number 8 (August 1978), The Otec Liaison
Volume 2, Number 8 (August 1978), The Otec Liaison
The OTEC Liaison
No abstract provided.
Volume 2, Number 7 (July 1978), The Otec Liaison
Volume 2, Number 7 (July 1978), The Otec Liaison
The OTEC Liaison
No abstract provided.
Spring Phytoplankton Composition And Distribution In Coastal Waters Between Nova Scotia And The Chesapeake Bay, Larry William Neal
Spring Phytoplankton Composition And Distribution In Coastal Waters Between Nova Scotia And The Chesapeake Bay, Larry William Neal
OES Theses and Dissertations
This investigation was directed toward satisfying a recognized lack of informat on regarding phytoplankton composition and density in shelf waters between Nova Scotia and the Chesapeake Bay. A sedimentation technique was used in determining the phytoplankton composition of 99 samples collected between 2 March and 3 April 1971. Chlorophyll-a samples collected concurrently were analyzed fluorometrically. Simple correlation analyses were utilized in describing distributional patterns of phytoplankton density and chlorophyll-a concentration with respect to water temperature, salinity, density, depth, distance from shore and latitude. Analysis of variance was employed in assessing regional differences in phytoplankton density and chlorophyll-a.
The phytoplankton flora …
Mercury, Copper, And Zinc In Selected Ichthyofauna Of Lower Chesapeake Bay And Hampton Roads, Virginia, W. Bruce Aitenhead
Mercury, Copper, And Zinc In Selected Ichthyofauna Of Lower Chesapeake Bay And Hampton Roads, Virginia, W. Bruce Aitenhead
OES Theses and Dissertations
Anchovys, croaker, spat, summer flounder and hogchokers were collected monthly to seasonally from November 1972 to October 1973 at three locations in the southern Chesapeake Bay region of Virginia.
The concentrations of mercury, copper and zinc were determined by atomic absorption spectrophotometry in whole fishes. Metal concentration varied with species and location. Anchovys had the highest mean concentrations of mercury and zinc while hog- chokers had the highest mean copper concentration. Mercury levels exceeding O.5 ppm were observed in species from all three loca- tions, but maximum heavy metal concentrations per species were highest in Craney Island fishes.
Temporal variations …
Volume 2, Number 6 (June 1978), The Otec Liaison
Volume 2, Number 6 (June 1978), The Otec Liaison
The OTEC Liaison
No abstract provided.
Volume 2, Number 5 (May 1978), The Otec Liaison
Volume 2, Number 5 (May 1978), The Otec Liaison
The OTEC Liaison
No abstract provided.
Volume 2, Number 4 (April 1978), The Otec Liaison
Volume 2, Number 4 (April 1978), The Otec Liaison
The OTEC Liaison
No abstract provided.
The Response Of An Idealized Continental Shelf To Atmospheric Forcing, Paul Francis Moersdorf
The Response Of An Idealized Continental Shelf To Atmospheric Forcing, Paul Francis Moersdorf
OES Theses and Dissertations
The response of continental shelf water to cooling and wind stress is investigated using a two-dimensional numerical model. The topography of the east coast continental shelf was idealized by connecting a shallow (50 m) rectangular nearshore basin to a deeper (100 m) rectangular offshore basin. Numerous cases were examined using a wide range of values for both the air•sea temperature difference and the Wind speed, although the direction of the wind was always perpendicular to the coast.
The model predicts large excursions of shelf water offshore, and the subsequent surfacing of lower waters. Upwelling velocities of close to five meters …