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Articles 4621 - 4650 of 5630
Full-Text Articles in Entire DC Network
Recent Dissolved-Oxygen Measurements In The Gulf Of Mexico Deep Waters, Worth D. Nowlin Jr., David F. Paskausky, Hugh J. Mclellan
Recent Dissolved-Oxygen Measurements In The Gulf Of Mexico Deep Waters, Worth D. Nowlin Jr., David F. Paskausky, Hugh J. Mclellan
Journal of Marine Research
In 1963 it was suggested that rather large gradients in dissolved oxygen exist in the Gulf of Mexico below a sill depth of between 1500 m and 1900 m. However, measurements made on three cruises during 1966 and 1967 indicate that there is no clearly discernable horizontal variation in dissolved oxygen in these waters....
Acoustic Backscattering From A Wind-Driven Water Surface, R. A. Pruitt, S. W. Marshall, R. R. Goodman
Acoustic Backscattering From A Wind-Driven Water Surface, R. A. Pruitt, S. W. Marshall, R. R. Goodman
Journal of Marine Research
This paper reports an attempt to measure the asymmetry of wind-generated water waves by using acoustical methods. A 40-foot wind-tunnel water flume provided a controlled water surface that was insonified from above at 162 kHz with pulses 30 µsec in duration (5 cycles). The scattered-pressure amplitude pulses were analyzed statistically as a function of the shear stress produced at the water surface by the wind....
The Ekman Vertical Velocity In An Enclosed Β-Plane Ocean, W. Lawrence Gates
The Ekman Vertical Velocity In An Enclosed Β-Plane Ocean, W. Lawrence Gates
Journal of Marine Research
The vertical flux beneath the surface boundary layer is determined by balancing the divergence induced in this layer by the prescribed wind stress and surface temperature with the divergence of an assumed geostrophic interior ftow. In this manner the equilibrium surface height over an enclosed basin is formulated as a boundary-value problem, the solution of which leads directly to the Ekman vertical velocity....
Internal Wave Propagation Normal To A Geostrophic Current, David Healey, Paul H. Leblond
Internal Wave Propagation Normal To A Geostrophic Current, David Healey, Paul H. Leblond
Journal of Marine Research
It is shown that (i) internal gravity waves propagating along a horizontal density gradient in a uniformly rotating ocean can exist for a range of slightly smaller frequencies than is possible in the absence of such a gradient, (ii) such waves exhibit a phase difference from top to bottom, and (iii) they exchange energy with the geostrophic current, which balances the density-induced pressure gradient....
On The Dynamics Of The Florida Current, William J. Schmitz Jr.
On The Dynamics Of The Florida Current, William J. Schmitz Jr.
Journal of Marine Research
This paper contains selected results from the first in a series of new efforts directed toward establishing an observational basis for testing hypotheses on the dynamics of the Florida Current. These efforts are based on the application of a recently developed free-instrument method for the collection of density and velocity field data at several sections across the Current....
The Generation Of Longshore Currents On A Plane Beach, Anthony J. Bowen
The Generation Of Longshore Currents On A Plane Beach, Anthony J. Bowen
Journal of Marine Research
The generation of longshore currents on a beach is investigated theoretically, using the concept of radiation stress to describe the flux of momentum associated with the incoming waves. Outside the surf zone, the longshore gradient of the radiation stress is always zero, and the flow is therefore driven only inside the surf zone....
Some New Observations On The Equilibrium Region Of The Wind-Wave Spectrum, John Garrett
Some New Observations On The Equilibrium Region Of The Wind-Wave Spectrum, John Garrett
Journal of Marine Research
Observations made with an array of wave sensors reveal significant differences between the high-frequency regions of spectra measured on different days. These differences suggest that the idea of a universal equilibrium range may not be strictly true.
Oceanic Flow Over Varying Bottom Topography, R. A. Clarke, N. P. Fofonoff
Oceanic Flow Over Varying Bottom Topography, R. A. Clarke, N. P. Fofonoff
Journal of Marine Research
A study has been made of steady barotropic flows on the β plane over a bottom topography that varies in a direction inclined to the circles of latitude. The solutions obtained, starting with both the Eulerian and the Lagrangian systems of equations, are shown to be identical in the case of flow over a single-depth discontinuity....
Effects Of Friction And Surface Tide Angle Of Incidence On The Coastal Generation Of Internal Tides, J. G. Weigand, H. G. Farmer, S. J. Prinsenberg, Maurice Rattray Jr.
Effects Of Friction And Surface Tide Angle Of Incidence On The Coastal Generation Of Internal Tides, J. G. Weigand, H. G. Farmer, S. J. Prinsenberg, Maurice Rattray Jr.
Journal of Marine Research
For the generation of internal waves by long surface waves, the normal-mode equations and solutions that satisfy the boundary conditions in a two-layer system are found analytically. Frictional effects decrease the amplitude of an internal wave over the shelf, changing it from a standing wave to a wave that progresses coastward and decreases the interference on the amplitude of the offshore progressive wave traveling seaward. Model studies, using a two-layer system of fresh water and saline water in a 9.9-m-long channel, gave favorable results relative to the theoretical results.
Average Velocities Of Some Ocean Currents As Deduced From The Recovery Of Plastic Drift Cards, G. H. Stander, L. V. Shannon, J. A. Campbell
Average Velocities Of Some Ocean Currents As Deduced From The Recovery Of Plastic Drift Cards, G. H. Stander, L. V. Shannon, J. A. Campbell
Journal of Marine Research
Twenty-four drift cards, released in 1964 through 1966 in the vicinity of Cape Town and at various locations in the Atlantic Ocean, have been recovered on the coasts of: North and South America, three islands in the South Atlantic, England, France, Nigeria, and Australia. The travel times indicated by 19 of these cards have been used to estimate the mean velocities of the presumed current systems involved. The rate of card recovery and the long distances traveled by the cards have proved conclusively that the solid polythene drift card is durable.
An Underwater Spectral Irradiance Collector, Raymond C. Smith
An Underwater Spectral Irradiance Collector, Raymond C. Smith
Journal of Marine Research
The design, testing, and evaluation of the accuracy of a collector for measuring underwater spectral irradiance is the subject of this paper. A successful underwater irradiance collector is described. Emphasis is placed on the experimental techniques employed in testing its collecting properties and in measuring the immersion effect so that its accuracy can be estimated....
Naviface, Oxyty, And Epichthon: Words Versus Terms, John Lyman
Naviface, Oxyty, And Epichthon: Words Versus Terms, John Lyman
Journal of Marine Research
The suggestions by R. B. Mongomery (1969) concerning the need for new words in marine research raise in my mind the question of whether in fact it is new words or new terms that are necessary. By coining new words, are we not in danger of surrounding our discipline with a jargon that, while it may facilitate slightly communication among insiders, restricts to a greater extent communication with those in other fields?....
Redefinition Of Salinity, Warren S. Wooster, Arthur J. Lee, Gunter Dietrich
Redefinition Of Salinity, Warren S. Wooster, Arthur J. Lee, Gunter Dietrich
Journal of Marine Research
Two definitions of salinity have been in use since the early part of the present century (Knudsen 1901, Forch et al. 1902). According to the procedural definition, salinity is the amount (in grams) of dissolved solid material in a kilogram of seawater after all the bromine has been replaced by an equivalent quantity of chlorine, after all the carbonate has been converted to oxide, and after all of the organic matter has been destroyed....
The Use Of Moire Fringes In Laboratory Oceanography, D. James Baker Jr.
The Use Of Moire Fringes In Laboratory Oceanography, D. James Baker Jr.
Journal of Marine Research
The purpose of this note is to present a sketch of the inexpensive Moire fringe technique, which provides a quick and easy visualization of concentration gradients and which can be used for quantitative measurements….
Osteology Of Deinonychus Antirrhopus, An Unusual Theropod From The Lower Cretaceous Of Montana, John H. Ostrom
Osteology Of Deinonychus Antirrhopus, An Unusual Theropod From The Lower Cretaceous Of Montana, John H. Ostrom
Bulletin of the Peabody Museum of Natural History
A detailed description is presented of the skeletal anatomy and adaptations of Deinonychus antirrhopus Ostrom (1969), a very unusual carnivorous dinosaur (Order Saurischia, Suborder Theropoda) from the Cloverly Formation (Early Cretaceous) of Montana….
Tertiary Pongidae Of East Africa: Evolutionary Relationships And Taxonomy, David R. Pilbeam
Tertiary Pongidae Of East Africa: Evolutionary Relationships And Taxonomy, David R. Pilbeam
Bulletin of the Peabody Museum of Natural History
Recently recovered pongid specimens of Dryopithecus (Proconsul) major from Moroto and Napak in Uganda are described and compared to material of the same species from Songhor and Koru in Kenya….
A Revision Of The Moths Of The Subfamily Geometrinae Of America North Of Mexico (Insecta, Lepidoptera), Douglas C. Ferguson
A Revision Of The Moths Of The Subfamily Geometrinae Of America North Of Mexico (Insecta, Lepidoptera), Douglas C. Ferguson
Bulletin of the Peabody Museum of Natural History
A new classification of the Geometrinae of the United States and Canada is presented, based largely on original investigations of male and female genitalia and larval characters….
The Cuban Health Care System; A Study In The Evaluation Of Health Care Systems, Michael Liebowitz
The Cuban Health Care System; A Study In The Evaluation Of Health Care Systems, Michael Liebowitz
Yale Medicine Thesis Digital Library
No abstract provided.
Influence Of The Amazon River Outflow On The Ecology Of The Western Tropical Atlantic. Iii. The Planktonic Flora Between The Amazon River And The Windward Island, E. M. Hulburt, Nathaniel Corwin
Influence Of The Amazon River Outflow On The Ecology Of The Western Tropical Atlantic. Iii. The Planktonic Flora Between The Amazon River And The Windward Island, E. M. Hulburt, Nathaniel Corwin
Journal of Marine Research
An abundant diatomaceous flora was observed in shallow waters along the coasts of French Guiana and Dutch Guiana during the fall of 1964 and the spring of 1965. In the fall, these diatoms were apparently carried far beyond the continental shelf by the Amazon effluent, which crossed the northwestward Guiana Current and became entrained in a southeastward countercurrent....
Description Of A Freely Dropped Instrument For Measuring Current Velocity, William S. Richardson, Allan R. Carr, Henry J. White
Description Of A Freely Dropped Instrument For Measuring Current Velocity, William S. Richardson, Allan R. Carr, Henry J. White
Journal of Marine Research
A new form of freely dropped instrument for current-velocity measurements is described. Operational procedures for using the instrument and its auxiliary equipment are given.
Comparison Between Wind Waves At Sea And In The Laboratory, G. D. Hess, G. M. Hidy, E. J. Plate
Comparison Between Wind Waves At Sea And In The Laboratory, G. D. Hess, G. M. Hidy, E. J. Plate
Journal of Marine Research
Correlations between laboratory and geophysical data are presented for certain statistical properties of wind waves. The parameters chosen include: (i) relationships between wave height and the height of the highest one-third or one-tenth waves, as given by a Rayleigh probability distribution, and (ii) amplitude spectra for waves, as given by Phillips' equilibrium theory. The correlation between laboratory results and geophysical data is satisfactory over a wide range of wave size.
Geostrophy And Direct Measurements In The Straits Of Florida, Saul Broida
Geostrophy And Direct Measurements In The Straits Of Florida, Saul Broida
Journal of Marine Research
Quantitative agreement between geostrophic computations and direct measurements of current and transport in the Straits of Florida, and elsewhere as well, is found only when observations are made under synoptic conditions. Under other conditions, geostrophic computations often show a multiaxial structure (i.e., bands of current) not found with direct measurements; this apparent multiaxial structure could be caused largely by periodic disturbances related to the tides....
Bone Marrow As The Source Of Inflammatory Cells In Adjuvant Arthritis, Deborah Alden Putnam
Bone Marrow As The Source Of Inflammatory Cells In Adjuvant Arthritis, Deborah Alden Putnam
Yale Medicine Thesis Digital Library
No abstract provided.
Deep Water Properties And Flow In The Central North Pacific, R. K. Reed
Deep Water Properties And Flow In The Central North Pacific, R. K. Reed
Journal of Marine Research
Values of potential temperature, salinity, and dissolved oxygen at deep levels in the central North Pacific are presented and discussed, and the direction of flow is inferred. Deep water from the south appears to spread into the northern region by way of a western route rather than directly through the central region.
Analyses Of Coccolith Ooze From The Deep Tropical Atlantic, Geoffrey Thompson, Vaughan T. Bowen
Analyses Of Coccolith Ooze From The Deep Tropical Atlantic, Geoffrey Thompson, Vaughan T. Bowen
Journal of Marine Research
Analyses of samples from a 200-cm core of coccolith ooze from the deep tropical Atlantic (00° 07'S, 17° 34'W) show it to be uniformly composed of low-magnesium calcite. The levels of most trace elements were found to be low for pelagic marine carbonate sediments.
The Words Naviface And Oxyty, R. B. Montgomery
The Words Naviface And Oxyty, R. B. Montgomery
Journal of Marine Research
It is amazing that English-speaking scientists and seamen have muddled along without a noun for the all-important interface between atmosphere and ocean, sometimes designated with the phrase "air-sea interface," more often with the vague phrase "sea surface." For clarity and economy of expression, a single word is needed for this floor of the atmosphere and ceiling of the ocean....
On The Roles Of Vertical Velocity And Eddy Conductivity In Maintaining A Thermocline, Roy Overstreet, Maurice Rattray Jr.
On The Roles Of Vertical Velocity And Eddy Conductivity In Maintaining A Thermocline, Roy Overstreet, Maurice Rattray Jr.
Journal of Marine Research
Steady-state solutions of the vertical heat-balance equation have been obtained for various assumed vertical profiles of the vertical component of velocity and eddy conductivity. Relationships have been found for the depth and the thickness of the thermocline in terms of parameters that characterize the vertical velocity and eddy conductivity. Two of the solutions agree with observations in regions having respectively divergent and convergent Ekman mass transport.
Comparison Of The Hydrographic Structure Of Equatorial Waters North Of New Guinea And At 170°E, Philippe Hisard, Yves Magnier, Bruno Wauthy
Comparison Of The Hydrographic Structure Of Equatorial Waters North Of New Guinea And At 170°E, Philippe Hisard, Yves Magnier, Bruno Wauthy
Journal of Marine Research
The Equatorial Undercurrent was observed from March through August 1967 on a transect along 170°E during five cruises of the R. V. CORIOLIS. The velocity structure changed markedly from cruise to cruise….
Concentrations Of Mn, Co, Cu, Fe, And Zn In The Northern Indian Ocean And Arabian Sea, Graham Topping
Concentrations Of Mn, Co, Cu, Fe, And Zn In The Northern Indian Ocean And Arabian Sea, Graham Topping
Journal of Marine Research
Samples of seawater from the Indian Ocean (RRS DISCOVERY Sts. 5102-5206) and the Arabian Sea (Sts. 5077-5094), obtained in 1962 through 1964 with N.I.O. sampling bottles, have been analyzed for Mn, Co, Cu, Fe, and Zn. This investigation has indicated that, in the northwestern Indian Ocean and the Arabian Sea, higher values of these trace elements are found in the surface layers compared with the bottom layer and that there is a tendency for these trace elements to decrease in concentration with depth....
Evaporation In The Laboratory And At Sea, Allen H. Schooley
Evaporation In The Laboratory And At Sea, Allen H. Schooley
Journal of Marine Research
A short-fetch water-wind tunnel has been used to measure the evaporation rate for wind velocities between 200 and 800 cm/sec and for three water-air temperature differences. Sverdrup's assumption of a molecular diffusion sublayer at the naviface bas been used to compare laboratory evaporation measurements with existing measurements at sea....