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天津科技大学海洋地质学课件Section 7 SEA RICHES。
天津科技大学海洋地质学课件Section 6 COASTAL GEOLOGY。  
天津科技大学海洋地质学课件Section 5 SUBMARINE VOLCANOES。  
天津科技大学海洋地质学课件Section 4 RIDGES AND TRENCHES。
天津科技大学海洋地质学课件Section 3 THE DYNAMIC SEAFLOOR。
天津科技大学海洋地质学课件Section 2 MARINE EXPLORATION。  
天津科技大学海洋地质学课件Section 1 INTRODUCTION
The mean density structure in the Northeast Atlantic is described in terms of the stability frequency. Some dynamic considerations are given to account for the observed distribution and to indicate th...
The pressure along a closed hydrographic section can be correctly calculated from density data, in the ideal case of perfectly steady, geostrophic, density-conserving flow; and from dense, error-free ...
Continuous conductivity-temperature-depth-dissolved-oxygen (CTD) data are used to investigate the spatial distribution of fine and microstructure between the Azores and Flemish Cap. The CTD data are u...
Ten anomalous water parcels were detected in the water column of a western Atlantic oceanographic section (0–5550 m; 70°W; 23–33°N). The parcels had extreme properties lying either two standard deviat...
Subtropical Mode Water in the 137°E Section.
The inviscid two-layer hydraulic model of Farmer and Armi has two types of solution in the eastern end of the Strait of Gibraltar for flow that is critical at Camarinal Sill. The solution correspondin...
Pulse-like acoustic transmissions (133 Hz, 60 ms resolution), between a bottom-mounted source near Oahu and a bottom-mounted receiver at about 4000 km range near the coast of Northern California, are ...
The most southerly WOCE one-time section in the South Atlantic, designated A11, was occupied in January 1993. The cruise track lay across the cool subantarctic zone of the Circumpolar Current in the w...

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