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Yang Dianrong,Zhou Dejian,Zhang Yulin. 1992. Cross thermocline mixing effect due to tide in the shallow sea. Acta Oceanologica Sinica, (1):1－11
Cross thermocline mixing effect due to tide in the shallow sea
Cross thermocline mixing effect due to tide in the shallow sea
Received:June 19, 1989  Revised:August 15, 1990
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Author NameAffiliation
Yang Dianrong Institute of Physical Oceanography, Ocean University of Qingdao, Qingdao 266003, China 
Zhou Dejian Institute of Physical Oceanography, Ocean University of Qingdao, Qingdao 266003, China 
Zhang Yulin Institute of Physical Oceanography, Ocean University of Qingdao, Qingdao 266003, China 
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Abstract:
      Using the data specially observed on the Bohai Sea oil platform by the authors for studying thermocline for two weeks,the thermocline depth,the temperature and the salinity of the layers below and above the thermocline were numerically modelled.The model is based on the Stigebrandt model and some important supplements are made in this paper in accordance with the local condition of the sea.The modelling results fit well in the observations.It is proved that the entrainmem due to both the tide and the wind can give rise to rather intense mixing cross the thermocline.This process makes the temperature rising below the thermocline,and causes the nutrient increasing above it,which has important significance for the marine physical environment and the marine organism.
中文摘要:
      Using the data specially observed on the Bohai Sea oil platform by the authors for studying thermocline for two weeks,the thermocline depth,the temperature and the salinity of the layers below and above the thermocline were numerically modelled.The model is based on the Stigebrandt model and some important supplements are made in this paper in accordance with the local condition of the sea.The modelling results fit well in the observations.It is proved that the entrainmem due to both the tide and the wind can give rise to rather intense mixing cross the thermocline.This process makes the temperature rising below the thermocline,and causes the nutrient increasing above it,which has important significance for the marine physical environment and the marine organism.
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