In the tropics, large warm pools of near-surface water are enclosed by continental land boundaries and constant annual mean temperature surfaces at depth. Water which enters such a volume is of the same temperature as the water which leaves it and hence no net heat can accumulate by mean advection; the ocean surface heat flux into this volume is balanced by turbulent transport out of it...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
Heat and turbulent energy balances in the central equatorial Indian Ocean are examined using over tw...
Thesis (M.S.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Sciences, 1969.Bi...
Hydrographic sections that span the Antarctic Circumpolar Current are used to estimate the zonal hea...
The Mediterranean and Red Seas are used as test volumes in an attempt to assess the accuracy of esti...
Under usual conditions, the Western Equatorial Pacific is characterized by a low heat content on the...
A simple concept model of the climatology of a subtropical ocean gyre is developed on the basis of a...
Oceanic motions are partly driven by thermal forces associated with differential heating of the surf...
Numerical solutions for a model of the World Ocean are analyzed to illustrate the important changes ...
We review current understanding of the warm water formation and escape process in the tropical Atlan...
We review current understanding of the warm water formation and escape process in the tropical Atlan...
A new map of the potential temperature at the bottom of the Pacific Ocean has been prepared It allow...
The average monthly variation of the heat and salt balance of the upper 200 m is investigated for ei...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
Heat and turbulent energy balances in the central equatorial Indian Ocean are examined using over tw...
Thesis (M.S.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Sciences, 1969.Bi...
Hydrographic sections that span the Antarctic Circumpolar Current are used to estimate the zonal hea...
The Mediterranean and Red Seas are used as test volumes in an attempt to assess the accuracy of esti...
Under usual conditions, the Western Equatorial Pacific is characterized by a low heat content on the...
A simple concept model of the climatology of a subtropical ocean gyre is developed on the basis of a...
Oceanic motions are partly driven by thermal forces associated with differential heating of the surf...
Numerical solutions for a model of the World Ocean are analyzed to illustrate the important changes ...
We review current understanding of the warm water formation and escape process in the tropical Atlan...
We review current understanding of the warm water formation and escape process in the tropical Atlan...
A new map of the potential temperature at the bottom of the Pacific Ocean has been prepared It allow...
The average monthly variation of the heat and salt balance of the upper 200 m is investigated for ei...
From the Global Weather Experiment in 1979, four one-year data records are juxtaposed which simultan...
Merchant ship observations were summarized for one-degree squares along the eastern shore of the Atl...
In studies of basins along the western rim of the Pacific, Wyrtki (1961 a, b) found no significant d...
Heat and turbulent energy balances in the central equatorial Indian Ocean are examined using over tw...
Thesis (M.S.)--Massachusetts Institute of Technology, Dept. of Earth and Planetary Sciences, 1969.Bi...