On the Existence of Benthic Storms

Quirchmayr Ronald

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On the Existence of Benthic Storms

机译：论底栖风暴的存在

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We study a model for the wind-induced current field of the Pacific ocean in order to demonstrate that currents in the surface layer are carried down to the deepest regions above the abyssal sea floor, which indicates the existence of the phenomenon of comparably strong currents in bottom regions as a result of wind-stress forces at the surface, also known as benthic storms.

机译：我们研究了太平洋风致洋流场的模型，以证明表层的洋流被带到深海海底以上的最深处，这表明由于表层的风应力，底部区域存在相对强的洋流现象，也称为底栖风暴。

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来源
《Journal of nonlinear mathematical physics》 |2015年第4期|540-544|共5页
作者
Quirchmayr Ronald;
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作者单位

Univ Vienna, Fac Math, A-1090 Vienna, Austria;

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原文格式 PDF
正文语种英语
中图分类理论物理学;
关键词
equatorial flows; eddy viscosity; stratification;

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On the Existence of Benthic Storms

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