Abstract
A seven-compartment model of the mixed layer ecosystem was used to fit a time series of observations derived from data obtained during the 1989 JGOFS North Atlantic Bloom Experiment. A nonlinear optimization technique was used to obtain the best fit to the combined observation set. It was discovered that a solution which gave a good fit to primary production gave a bad fit to zooplankton and vice versa. The solution which fitted primary production also showed good agreement with a number of other independent data sets, but overestimated bacterial production. Further development is necessary to create a model capable of reproducing all the important features of the nitrogen flows within the mixed layer.
Subject
General Agricultural and Biological Sciences,General Biochemistry, Genetics and Molecular Biology
Reference18 articles.
1. Berger W.H. 1989 Global maps of ocean productivity. In Productivity of the ocean:present and past (ed. W.H Berger V.S. Smetacek & G. Wefer) pp. 429-456. Chichester: Wiley-Interscience.
2. Calculating solar radiation for ecological studies
3. Microzooplankton and their herbivorous activity in the northeastern Atlantic Ocean
4. Primary production at 47°N and 20°W in the North Atlantic Ocean: a comparison between the 14C incubation method and the mixed layer carbon budget
5. AtlantisII leg 2) the simulated Dortch Q. 1990 The interaction between ammonium and
Cited by
117 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献