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Outflow physical components e n t r a i n e d w a t e r source water p r o d u c t w a t e r surface water Q, E-P descent and entrainment deep ocean-marginal sea exchange air-sea exchange i s o p y c n a l o c e a n f l o o r A typical dense water outflow from a high-latitude or marginal sea Antarct...

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Bibliographic Details
Main Authors: Xiaobiao Xu, Red Sea, Faroe Bank Channel
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Antarctic
Antarc*
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.690.98
http://hycom.org/attachments/086_Xu.pdf
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Summary:Outflow physical components e n t r a i n e d w a t e r source water p r o d u c t w a t e r surface water Q, E-P descent and entrainment deep ocean-marginal sea exchange air-sea exchange i s o p y c n a l o c e a n f l o o r A typical dense water outflow from a high-latitude or marginal sea Antarctic slope

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