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  • 1990-1994  (2)
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  • 1
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    In:  Philosophical Transactions of the Royal Society B: Biological Sciences, 343 (1303). pp. 27-31.
    Publication Date: 2020-06-11
    Description: Understanding the plankton ecosystem in the ocean requires detailed demographic analysis. It is impossible to sample the ocean adequately for such analysis, but progress can be made by analysing data sets generated by mathematical models provided they realistically simulate the ecosystem. The Lagrangian Ensemble method is well suited to demographic studies because it generates large data sets containing complete information on all the families living in the simulated ecosystem. It provides audit trails of individual families for unambiguous analysis of mechanisms responsible for the simulated changes in community and environment. Recent papers based on the Lagrangian Ensemble method are reviewed.
    Type: Article , PeerReviewed
    Format: text
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  • 2
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    AGU (American Geophysical Union)
    In:  In: The Polar Oceans and Their Role in Shaping the Global Environment. , ed. by Johannessen, O. M., Muench, R. D. and Overland, J. E. Geophysical Monograph Series, 85 . AGU (American Geophysical Union), pp. 247-254.
    Publication Date: 2012-07-12
    Description: The current status of the Sverdrup theory for the initiation of plankton blooms is examined. A prescription is given for the computation of the Sverdrup critical depth, using recently-published algorithms for mixed-layer primary production and a generalised loss term. Using no further information, the intrinsic rate of increase of phytoplankton biomass in the mixed layer can also be found. This rate, compared against the local frequency of storm occurrence, provides an alternative criterion for the initiation of blooms. The Eulerian (bulk property) methods used to derive these results are contrasted with the Lagrangian Ensemble method. The Lagrangian approach provides one avenue to the elaboration of the Sverdrup criterion to include the effect of processes with characteristic timescales small compared to one day. The incidence of blooms in the apparent absence of vertical stratification is reviewed: it is concluded that these observations do not undermine the basic logic of the Sverdrup theory. However, they do provoke interest in a re-examination of the feedbacks between the physical and biological dynamics in the mixed layer: an example is given. Finally, suggestions are made for further work in this subject area.
    Type: Book chapter , NonPeerReviewed
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