Add to ORKGThe Mediterranean and Red Seas are used as test volumes in an attempt to assess the accuracy of estimates of climatological air-sea fluxes calculated using meteorological observations from merchant ships…
Numerical solutions for a model of the World Ocean are analyzed to illustrate the important changes ...
The quasi-isothermal halocline between depths of about 100 and 200 m is a striking feature of the te...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Sciences, 1970....
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
In the tropics, large warm pools of near-surface water are enclosed by continental land boundaries a...
The average monthly variation of the heat and salt balance of the upper 200 m is investigated for ei...
Little information is available on the temperature differences in the first several centimeters of a...
The nature and quality of portions of the Marine Deck of sea-surface temperature (SST) records for M...
Because of the large tidal velocities and small dimensions of estuaries, it is not justified to igno...
A model is given that describes the local response of the upper ocean to an imposed surface wind str...
Hydrographic sections that span the Antarctic Circumpolar Current are used to estimate the zonal hea...
Terrestrial heat flow through the ocean floor is determined by measuring the temperature gradient an...
Basin-wide geostrophic shear profiles have been computed for several latitudes in the eastern Atlant...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
A simple model is used to explore a feedback mechanism which may be significant in the formation of ...
Numerical solutions for a model of the World Ocean are analyzed to illustrate the important changes ...
The quasi-isothermal halocline between depths of about 100 and 200 m is a striking feature of the te...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Sciences, 1970....
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
In the tropics, large warm pools of near-surface water are enclosed by continental land boundaries a...
The average monthly variation of the heat and salt balance of the upper 200 m is investigated for ei...
Little information is available on the temperature differences in the first several centimeters of a...
The nature and quality of portions of the Marine Deck of sea-surface temperature (SST) records for M...
Because of the large tidal velocities and small dimensions of estuaries, it is not justified to igno...
A model is given that describes the local response of the upper ocean to an imposed surface wind str...
Hydrographic sections that span the Antarctic Circumpolar Current are used to estimate the zonal hea...
Terrestrial heat flow through the ocean floor is determined by measuring the temperature gradient an...
Basin-wide geostrophic shear profiles have been computed for several latitudes in the eastern Atlant...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
A simple model is used to explore a feedback mechanism which may be significant in the formation of ...
Numerical solutions for a model of the World Ocean are analyzed to illustrate the important changes ...
The quasi-isothermal halocline between depths of about 100 and 200 m is a striking feature of the te...
Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Sciences, 1970....