Baroclinic dynamics of grounded abyssal ocean currents

接地深海洋流的斜压动力学

• 批准号: 9357-2010
• 负责人: Swaters, Gordon
• 金额: $ 1.6万
• 依托单位: University of Alberta
• 依托单位国家: 加拿大
• 项目类别: Discovery Grants Program - Individual
• 财政年份: 2014
• 资助国家: 加拿大
• 起止时间: 2014-01-01 至 2015-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=544626
• 关键词: Baroclinic; dynamics; grounded; abyssal; ocean

One can categorize ocean currents into two broad groups. The first are the currents that are wind driven. These currents are most intense near the surface of the ocean. Their principal role is to transport warm equatorial waters toward the Polar Regions. The second class of currents are those that are driven by density contrasts with the surrounding waters. In this latter group are the deep, or abyssal, currents flowing along or near the bottom of the oceans along the continental boundaries. Their principal role is to transport cold, dense waters produced in the Polar Regions equatorward (and beyond). Taken together, the warm surface currents and the cold abyssal currents are the means by which the ocean convectively overturns, mixing incoming solar heating meridionally and vertically into the ocean interior.

人们可以将洋流分为两大类。第一种是由风驱动的洋流。这些洋流在靠近海洋表面的地方最为强烈。它们的主要作用是将温暖的赤道沃茨输送到极地地区。第二类海流是由与周围沃茨的密度对比所驱动的海流。在后一类中，有深海流或深海海流，它们沿着或靠近海洋底部沿着大陆边界流动。它们的主要作用是将极地地区产生的寒冷、稠密的沃茨输送到赤道（及更远的地方）。总的来说，温暖的表层洋流和寒冷的深海洋流是海洋对流翻转的手段，将传入的太阳能加热混合到海洋内部。