NDLI: Coupled physical-ecological modelling of the central part of Jiaozhou Bay I. Physical modelling

Content Provider	Springer Nature Link
Author	Hai, Zhu Mao chang, Cui
Copyright Year	2000
Abstract	Sharples's 1-D physical model, employing tide-wind driven turbulence closure and surface heating-cooling physics, was used to simulate the evolution of seawater temperature in the central part of Jiaozhou Bay. The results were consistent with observation after application of a large value of vertical eddy diffusivity to the upper layer in the case of rainy season. The simulated bottom seawater temperature varies regularly in sinusoidal pattern. The simulated surface seawater temperature clearly indicates that stratification begins in the middle of April, lasting about 6 days, and ends in later August, lasting only 2 days; and that the strongest stratification occurs in June, when the surface net heat flux is close to zero. Since the rainfall process not considered in the present model could cause very strong vertical mixing in the upper layer of bay water, the physical meaning of applying a larger vertical eddy diffusivity is supposed to be a parametrization of the rainfall created mixing in the upper layer. To prove this hypothesis more complex models have to be used and more observations have to be made in future study.
Starting Page	309
Ending Page	314
Page Count	6
File Format	PDF
ISSN	02544059
Journal	Chinese Journal of Oceanology and Limnology
Volume Number	18
Issue Number	4
e-ISSN	19935005
Language	English
Publisher	Science Press
Publisher Date	2000-01-01
Publisher Place	Beijing
Access Restriction	Subscribed
Subject Keyword	physical modelling rainfall created mixing in the upper sea the central part of Jiaozhou Bay Oceanography
Content Type	Text
Resource Type	Article
Subject	Water Science and Technology Oceanography

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