Direct Measurements of Ocean Currents over the Continental Slope off Sydney

1979 ◽  
Vol 30 (6) ◽  
pp. 833 ◽  
Author(s):  
BV Hamon
Keyword(s):  
Continental Slope ◽  
Deep Ocean ◽  
Surface Current ◽  
Ocean Currents ◽  
North East ◽  
Direct Measurements ◽  
Deep Ocean Currents ◽  
Neutrally Buoyant ◽  
Tracking Period

The results of measurements of deep ocean currents over the continental slope off Sydney in May 1979 are presented and discussed. The measurements were made using neutrally buoyant floats. Four floats were used, at mean depths of 766, 1251, 1519 and 1886 m. All four floats moved towards north-north-east, approximately parallel to the depth contours, with mean speeds, over the 34-day tracking period, in the range 5-9 cm s-1. The surface current, estimated from ship's set, was towards north-east, at 25 cm s-1.

Using acoustic tomography to monitor deep ocean currents in the eastern Gulf of Mexico

OCEANS 2009 ◽  
2009 ◽  
Author(s):  
D. A. Rosenfield ◽  
J. W. Caruthers ◽  
D. A. Nechaev ◽  
G. E. Ioup ◽  
J. W. Ioup ◽  
...  
Keyword(s):  
Gulf Of Mexico ◽  
Deep Ocean ◽  
Ocean Currents ◽  
Acoustic Tomography ◽  
Eastern Gulf Of Mexico ◽  
Deep Ocean Currents

scholarly journals Generation of Hydroacoustic Waves by an Oscillating Ice Block in Arctic Zones

2016 ◽  
Vol 2016 ◽  
pp. 1-7 ◽  
Author(s):  
Usama Kadri
Keyword(s):  
Free Surface ◽  
Ocean Circulation ◽  
Deep Ocean ◽  
Ocean Currents ◽  
Snowball Earth ◽  
Acoustic Modes ◽  
Time Harmonic ◽  
Arctic Conditions ◽  
Deep Ocean Currents ◽  
Harmonic Problem

The time harmonic problem of propagating hydroacoustic waves generated in the ocean by a vertically oscillating ice block in arctic zones is discussed. The generated acoustic modes can result in orbital displacements of fluid parcels sufficiently high that may contribute to deep ocean currents and circulation. This mechanism adds to current efforts for explaining ocean circulation from a snowball earth Neoproterozoic Era to greenhouse earth arctic conditions and raises a challenge as the extent of ice blocks shrinks towards an ice-free sea. Surprisingly, unlike the free-surface setting, here it is found that the higher acoustic modes exhibit a larger contribution.

scholarly journals Retention of ice-associated amphipods: possible consequences for an ice-free Arctic Ocean

2012 ◽  
Vol 8 (6) ◽  
pp. 1012-1015 ◽  
Author(s):  
J. Berge ◽  
Ø. Varpe ◽  
M. A. Moline ◽  
A. Wold ◽  
P. E. Renaud ◽  
...  
Keyword(s):  
Sea Ice ◽  
Arctic Ocean ◽  
Marine Mammals ◽  
Deep Ocean ◽  
Arctic Sea Ice ◽  
Ocean Currents ◽  
The Arctic ◽  
Arctic Sea ◽  
The Arctic Ocean ◽  
Deep Ocean Currents

Recent studies predict that the Arctic Ocean will have ice-free summers within the next 30 years. This poses a significant challenge for the marine organisms associated with the Arctic sea ice, such as marine mammals and, not least, the ice-associated crustaceans generally considered to spend their entire life on the underside of the Arctic sea ice. Based upon unique samples collected within the Arctic Ocean during the polar night, we provide a new conceptual understanding of an intimate connection between these under-ice crustaceans and the deep Arctic Ocean currents. We suggest that downwards vertical migrations, followed by polewards transport in deep ocean currents, are an adaptive trait of ice fauna that both increases survival during ice-free periods of the year and enables re-colonization of sea ice when they ascend within the Arctic Ocean. From an evolutionary perspective, this may have been an adaptation allowing success in a seasonally ice-covered Arctic. Our findings may ultimately change the perception of ice fauna as a biota imminently threatened by the predicted disappearance of perennial sea ice.

Lagrangian studies of deep ocean currents

Eos ◽  
1984 ◽  
Vol 65 (10) ◽  
pp. 82
Author(s):  
T. Rossby
Keyword(s):  
Deep Ocean ◽  
Ocean Currents ◽  
Deep Ocean Currents
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