On mathematical simulation of a pelagic ecosystem in tropical waters of the ocean
β Scribed by M. E. Vinogradov; V. V. Menshutkin; E. A. Shushkina
- Publisher
- Springer-Verlag
- Year
- 1972
- Tongue
- English
- Weight
- 887 KB
- Volume
- 16
- Category
- Article
- ISSN
- 0025-3162
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β¦ Synopsis
Consideration is given to a finite-difference model of functioning of a pelagic community inhabiting the upper 0 to 200 m layer of the tropical waters of the ocean. The model was developed on the basis of original data, obtained mainly on the 44th cruise of the I~.V. "Vityaz" in the western Equatorial Pacific Ocean. Changes in the system are studied in time (up to 100 days, with I day intervals) and in depth (from surface to 200 m depth, with 10 m intervals). The state of the system in the upwelling zone, assumed ~o be characterized by a homogeneous vertical distribution of all its elements, is regarded as initial. The system then develops with time while it moves with the water flow. The model was realized on a BESM-3~ computor. The computations yidded a pattern of changes in time of the biomass of the elements (expressed in calories), and a pattern of their vertical distribution at different instants. The vertical distribution pattern of the major elements of the model shows a rather close correlation with their observed distribution in the ocean at the corresponding instant.
π SIMILAR VOLUMES
The high rates of produetien by plank~nio bacteria reported by Sorokin for the warm surface layer of the oceans cannot be reconciled with the geographic distaqbution of dissolved organic carbon. Those rates, as well as Sorokin's figure8 of bactewial production and, hence, consumption of oxygen in th