Coupled physical-ecological modelling in the central part of Jiaozhou Bay II. Coupled with an ecological model

Cui Mao-chang; Zhu Hai

doi:10.1007/BF02842785

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Coupled physical-ecological modelling in the central part of Jiaozhou Bay II. Coupled with an ecological model

OriginalPaper | Updated：2023-05-16

- Coupled physical-ecological modelling in the central part of Jiaozhou Bay II. Coupled with an ecological model
- Coupled physical-ecological modelling in the central part of Jiaozhou Bay II. Coupled with an ecological model
- 海洋湖沼学报（英文） 2001年19卷第1期页码：21-28
- Affiliations：
  
  1. Institute of Oceanology Chinese Academy of Sciences
  2. Laboratory of Marine Science and Numerical modeling of SOA
- Author bio：
- Funds：
  
  Contribution No. 3774 from the Institute of Oceanology, Chinese Academy of Sciences.;Key Project 39630060 supported by NSFC and Key Lab. of Geophysical Fluid Dynamics and Numerical Modelling.
- DOI：10.1007/BF02842785
  中图分类号：
- 纸质出版：2001
- Accepted：
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Coupled physical-ecological modelling in the central part of Jiaozhou Bay II. Coupled with an ecological model[J]. 海洋湖沼学报（英文）, 2001,19(1):21-28.

Mao-chang, C., Hai, Z. Coupled physical-ecological modelling in the central part of Jiaozhou Bay II. Coupled with an ecological model., Chin. J. Ocean. Limnol. 19, 21–28 (2001). https://doi.org/10.1007/BF02842785
Coupled physical-ecological modelling in the central part of Jiaozhou Bay II. Coupled with an ecological model[J]. 海洋湖沼学报（英文）, 2001,19(1):21-28. DOI： 10.1007/BF02842785.

Mao-chang, C., Hai, Z. Coupled physical-ecological modelling in the central part of Jiaozhou Bay II. Coupled with an ecological model., Chin. J. Ocean. Limnol. 19, 21–28 (2001). https://doi.org/10.1007/BF02842785 DOI：

摘要

Abstract

Sharples' 1-D physical model employing tide-wind driven turbulence closure and surface heating-cooling physics

was coupled with an ecological model with 9-biochemical components: phytoplankton

zooplankton

shellfish

autotrophic and heterotrophic bacterioplankton

dissolved organic carbon (DOC)

suspended detritus and sinking particles to simulate the annual evolution of ecosystem in the central part of Jiaozhou Bay. The coupled modeling results showed that the phytoplankton shading effect could reduce seawater temperature by 2°C

so that photosynthesis efficiency should be less than 8%; that the loss of phytoplankton by zooplankton grazing in winter tended to be compensated by phytoplankton advection and diffusion from the outside of the Bay; that the incident irradiance intensity could be the most important factor for phytoplankton growth rate; and that it was the bacterial secondary production that maintained the maximum zooplankton biomass in winter usually observed in the 1990s

indicating that the microbial food loop was extremely important for ecosystem study of Jiaozhou Bay.

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Keywords

references

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