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In the spring of 1861 Matthew Fontaine Maury, whom many of us know as "The Pathfinder of the Seas" and the first Oceanographer of the U.S. Navy, had something of a change of heart and, perhaps as a re...
My purpose in this article is to increase awareness about long-standing problems in science education and then, in Part II, to build a case for how marine scientists, and scientists in general, can he...
Science and Education: two academic cultures with a wall between them. How can scientists surmount their own narrow disciplinary interests and capture some of the other culture's excitement? In a prev...
Typhoon-Ocean Interaction in the Western North Pacific:Part 1
Typhoon-Ocean Interaction Western North Pacific
2015/7/13
The application of new technologies has allowed oceanographers and meteorologists to study the ocean beneath typhoons in detail. Recent studies in the western Pacific Ocean reveal new insights into th...
Typhoon-Ocean Interaction in the Western North Pacific:Part 2
Typhoon-Ocean Interaction Western North Pacific
2015/7/13
During summer 2010, the Taiwan National Science Council and the US Office of Naval Research conducted a large typhoon-ocean field experiment named Impact of Typhoons on the Ocean in the Pacific (ITOP)...
The Circulation of the World Ocean：A Numerical Study. Part I, A Homogeneous Model
World Ocean Homogeneous Model
2009/4/3
Calculations are carried out for a homogeneous model of the World Ocean. Solutions for the large-scale, wind-driven circulation are obtained by numerical integration with respect to time of a numerica...
The Coastal Boundary Layer in Lake Ontario：Part II. The Summer-Fall Regime
Coastal Boundary Layer Lake Ontario The Summer-Fall Regime
2009/4/3
Field observations on coastal currents near Oshawa on the north shore of Lake Ontario during summer and fall are described. The technique of observations (flag-station chain) has been given in Part I,...
The Coastal Boundary Layer in Lake Ontario. Part I: The Spring Regime
Lake Ontario Coastal Boundary Layer Spring Regime
2009/4/3
Originally prompted by a desire to search for theoretically predicted “coastal jets,” an extensive series of observations on currents in the coastal zone near Oshawa, in Lake Ontario, were carried out...
Verification of Numerical Models of Lake Ontario：Part I. Circulation in Spring and Early Summer
Numerical Models Lake Ontario Early Summer
2009/3/26
Data from the 1972 International Field Year on Lake Ontario have been used to test the performance of three-dimensional hydrodynamical models of large lakes. The models vary with regard to computation...
Transient Gulf Stream Meandering. Part II：Analysis via a Quasi-Geostrophic Time-Dependent Model
Transient Gulf Stream Meandering Quasi-Geostrophic Time-Dependent Model
2009/3/26
Simultaneous path and bottom velocity measurements made during the Transient Meander Experiment, reported in Part I, are analyzed in terms of a quasi-geostrophic thin jet model of the meandering Gulf ...
Transient Gulf Stream Meandering. Part I: An Observational Experiment
Transient Gulf Stream Meandering Observational Experiment
2009/3/26
The results from an observational experiment on the mesoscale space-time variability of the Gulf Stream are reported. Various techniques, including aerial surveys, ship trackings of the 15C isotherm a...
Baroclinic Instability over a Slope. Part II：Finite-Amplitude Theory
Baroclinic Instability Finite-Amplitude Theory
2009/3/24
Baroclinic instability of a circular current is modified by the presence of a unidirectional bottom slope. An analytical theory is developed for the slightly unstable flow regime over a weak slope. Th...
Baroclinic Instability over a Slope. Part I：Linear Theory
Baroclinic Instability Slope Linear Theory
2009/3/24
We consider the instability properties of a circular current in the upper layer of a two-layer quasi-geostrophic ocean over a unidirectional slope. This particular flow-topography geometry is intended...
A Global Ocean-Atmosphere Climate Model. Part II. The Oceanic Circulation
Global Ocean-Atmosphere Climate Oceanic Circulation
2009/3/24
A numerical experiment has been carried out with a joint model of the ocean and atmosphere. The 12-level model of the world ocean predicts the fields of horizontal velocity, temperature and salinity. ...
A Global Ocean-Atmosphere Climate Model. Part I. The Atmospheric Circulation
Geophysical Fluid Dynamics Laboratory Atmospheric Circulation Global Ocean-Atmosphere Climate
2009/3/24
A joint ocean-atmosphere model covering the entire globe has been constructed at the Geophysical Fluid Dynamics Laboratory (GFDL) of NOAA. This model differs from the earlier version of the joint mode...