Handbook of Electric Cable Technology for Deep Ocean Applications

1970 ◽  
Author(s):  
Robert J. Forbes ◽  
Michael A. De Lucia ◽  
Samuel H. Behr
Keyword(s):  
Deep Ocean ◽  
Electric Cable

Test and Research Development of Electric Cable toward to Security and Reliability

2012 ◽  
Vol 132 (4) ◽  
pp. 200-203
Author(s):  
Masayuki NAGAO ◽  
Muneaki KURIMOTO ◽  
Risyun KIN ◽  
Tomohiro KAWASHIMA ◽  
Yoshinobu MURAKAMI
Keyword(s):  
Research Development ◽  
Electric Cable ◽  
Security And Reliability

On the impact of sea ice in a global ocean circulation model

1997 ◽  
Vol 25 ◽  
pp. 111-115 ◽  
Author(s):  
Achim Stössel
Keyword(s):  
Southern Ocean ◽  
Sea Ice ◽  
Ocean Circulation ◽  
General Circulation ◽  
Thermohaline Circulation ◽  
Circulation Model ◽  
Deep Ocean ◽  
Global Ocean ◽  
Convective Activity ◽  
The Impact

This paper investigates the long-term impact of sea ice on global climate using a global sea-ice–ocean general circulation model (OGCM). The sea-ice component involves state-of-the-art dynamics; the ocean component consists of a 3.5° × 3.5° × 11 layer primitive-equation model. Depending on the physical description of sea ice, significant changes are detected in the convective activity, in the hydrographic properties and in the thermohaline circulation of the ocean model. Most of these changes originate in the Southern Ocean, emphasizing the crucial role of sea ice in this marginally stably stratified region of the world's oceans. Specifically, if the effect of brine release is neglected, the deep layers of the Southern Ocean warm up considerably; this is associated with a weakening of the Southern Hemisphere overturning cell. The removal of the commonly used “salinity enhancement” leads to a similar effect. The deep-ocean salinity is almost unaffected in both experiments. Introducing explicit new-ice thickness growth in partially ice-covered gridcells leads to a substantial increase in convective activity, especially in the Southern Ocean, with a concomitant significant cooling and salinification of the deep ocean. Possible mechanisms for the resulting interactions between sea-ice processes and deep-ocean characteristics are suggested.

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