熱水プルームの挙動(<特集>海洋底熱水活動の物理・化学・生物過程)
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概要
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Physical behavior of plumes in the ocean was demonstrated by model calculation with some applications to a hydrothermal plume observed in the Okinawa Trough. In a special case where the initial momentum of a plume is so large that the plume was driven mainly by the momentum, a water mass of a colder and lower salinity campared to the surrounding water was formed. In other cases, a wamer and saltier water mass was formed. Concerning the behavior of the plume cloud, some phenomena caused by the differenece between diffusivities of heat and salt were also discussed qualitatively.
- 日本地球化学会の論文
- 1988-06-30
著者
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深澤 理郎
東海大 海洋
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深澤 理郎
Division of Physical Oceanography, Ocean Research Institute, University of Tokyo
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蒲生 俊敬
Division of Marine Inorganic Chemistry, Ocean Research Institute, University of Tokyo
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- 熱水プルームの挙動(海洋底熱水活動の物理・化学・生物過程)