Simulation of coupled pelagic-benthic ecosystem of the Yellow Sea Cold Water Mass
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Simulation of coupled pelagic-benthic ecosystem of the Yellow Sea Cold Water Mass
Simulation of coupled pelagic-benthic ecosystem of the Yellow Sea Cold Water Mass
海洋湖沼学报(英文)2005年23卷第4期 页码:393-399
Affiliations:
1. Institute of Physical Oceanography Ocean University of China
2. Third Institute of Oceanography SOA
3. College of Marine Life Sciences Ocean University of China
Author bio:
Funds:
This work is supported by Major State Basic Research Development Program of China (973 Program, G19990437), China International Cooperation Program (No. 2001CB711004) and NSFC (No. 40476045).
Simulation of coupled pelagic-benthic ecosystem of the Yellow Sea Cold Water Mass[J]. 海洋湖沼学报(英文), 2005,23(4):393-399.
Xiaofang, W., Zengmao, W., Zhinan, Z. et al. Simulation of coupled pelagic-benthic ecosystem of the Yellow Sea Cold Water Mass., Chin. J. Ocean. Limnol. 23, 393–399 (2005). https://doi.org/10.1007/BF02842682
Simulation of coupled pelagic-benthic ecosystem of the Yellow Sea Cold Water Mass[J]. 海洋湖沼学报(英文), 2005,23(4):393-399. DOI: 10.1007/BF02842682.
Xiaofang, W., Zengmao, W., Zhinan, Z. et al. Simulation of coupled pelagic-benthic ecosystem of the Yellow Sea Cold Water Mass., Chin. J. Ocean. Limnol. 23, 393–399 (2005). https://doi.org/10.1007/BF02842682DOI:
Simulation of coupled pelagic-benthic ecosystem of the Yellow Sea Cold Water Mass
摘要
Abstract
A one-dimensional coupled pelagic-benthic box model for the Yellow Sea Cold Water Mass (YSCWM) is developed. The model is divided into three boxes vertically according to the depths of thermocline and euphotic layer. It simulates well the oligotrophic shelf ecosystem of the YSCWM considering effects of nutrients deposition and microbial loop. Main features of vertical structure of various variables in ecosystem of the YSCWM were captured and seasonal variability of the ecosystem was well reconstructed. Calculation shows that the contribution of microbial loop to the zooplankton can reach up to 60%. Besides
input of inorganic nutrients from atmospheric deposition is an important mechanism of production in upper layer of the YSCWM when stratified.
关键词
Keywords
references
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