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Net primary production (NPP) is the foundation of the oceans’ ecosystems and the fisheries they support. In the Arctic Ocean, NPP is controlled by a complex interplay of light and nutrients supplied by upwelling as well as lateral inflows from adjacent oceans and land. But so far, the role...
“Eddies are like the weather systems of the ocean, playing a major role in transporting heat and carbon from the upper ocean to deeper layers – a critical buffer against global warming. “Knowledge of the depth and shape of the sea floor is crucial for us to quantify the influence of un...
This forms in areas of long parallel valleys such as in folded mountain belts. Rivers occupy the valleys, and tributary streams join them at right angles.Trench A long, narrow, deep depression in the ocean floor that parallels a convergent plate boundary involving at least one oceanic plate....
A map of the physical and geological characteristics, such as seabed topography, bathymetry and bottom currents and information on the reliability of such data; 一份显示海底地形、水深和底层流等物理和地质特征的图件和关于这些数据的可靠性的资料; UN-2 a map of the physical and geological charac...
Acoustic stratigraphy and current-generated bedforms in deep ocean basins off southeastern AfricaA bathymetric map of the deep-sea floor off southeastern Africa shows the Agulhas Plateau to be separated from the continental margin of southeastern Africa by a narrow (50 km) elongate depression, the ...
The magnetic lineations give the history of this production back into the late Mesozoic and illuminate the history of the new aseismic parts of the ocean floor. This naturally directed attention to the relation of the sea-floor to the continents. There are two approaches: in the first, one ...
extremely difficult and expensive to survey by ship due to the remoteness of the region and the regularity of violent storms. The depth of the Southern Ocean, more than 7,000 meters (23,000 feet) deep in certain areas, make ADCP instruments fixed to the ocean floor impractical, to say ...
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These two sources, together with deep waters originating from the Southern Ocean, comprise the northward-flowing return path balancing the southward migration of the Circumpolar Deep Water component of the Atlantic Meridional Overturning Circulation (AMOC)1,2,19,20,21. Fig. 1: Location map. Core ...