Modelling planktonic ecosystems: parameterizing complexity
暂无分享,去创建一个
[1] J. G. Field,et al. The Ecological Role of Water-Column Microbes in the Sea* , 1983 .
[2] L. Legendre,et al. Effects of pelagic food-web interactions and nutrient remineralization on the biogeochemical cycling of carbon: a modeling approach , 2000 .
[3] P. Boyd,et al. Elevated consumption of carbon relative to nitrogen in the surface ocean , 1993, Nature.
[4] Robert M. May,et al. Stability and Complexity in Model Ecosystems , 2019, IEEE Transactions on Systems, Man, and Cybernetics.
[5] F. Rassoulzadegan,et al. Food-web mediated export of biogenic carbon in oceans: hydrodynamic control , 1996 .
[6] P. Falkowski. Rationalizing elemental ratios in unicellular algae , 2000 .
[7] J. Goering,et al. UPTAKE OF NEW AND REGENERATED FORMS OF NITROGEN IN PRIMARY PRODUCTIVITY1 , 1967 .
[8] R. Armstrong,et al. Grazing limitation and nutrient limitation in marine ecosystems: Steady state solutions of an ecosystem model with multiple food chains , 1994 .
[9] B. Frost. A modelling study of processes regulating plankton standing stock and production in the open Subarctic Pacific Ocean , 1993 .
[10] K. Denman,et al. The structure of pelagic marine ecosystems. , 1978 .
[11] R. Olson,et al. DIFFERENTIAL PHOTOINHIBITION OF MARINE NITRIFYING BACTERIA: A POSSIBLE MECHANISM FOR THE FORMATION OF THE PRIMARY NITRITE MAXIMUM , 1981 .
[12] R. Armstrong. Stable model structures for representing biogeochemical diversity and size spectra in plankton communities , 1999 .
[13] G. Ærtebjerg,et al. Picoalgae in Danish coastal waters during summer stratification , 1991 .
[14] Alan A. Berryman,et al. The Orgins and Evolution of Predator‐Prey Theory , 1992 .
[15] Q. Dortch,et al. The interaction between ammonium and nitrate uptake in phytoplankton , 1990 .
[16] H. Resit Akçakaya,et al. Consequences of Ratio‐Dependent Predation for Steady‐State Properties of Ecosystems , 1992 .
[17] David Archer,et al. Modeling the impact of fronts and mesoscale circulation on the nutrient supply and biogeochemistry of the upper ocean , 2000 .
[18] D. Deibel,et al. Microzooplankton bacterivory and herbivory in the NE subarctic Pacific , 1999 .
[19] Kevin E. Kohler,et al. A four-component ecosystem model of biological activity in the Arabian Sea , 1996 .
[20] P. Wheeler. New production in the subarctic Pacific Ocean: Net changes in nitrate concentrations, rates of nitrate assimilation and accumulation of particulate nitrogen , 1993 .
[21] Nicholas R. Bates,et al. Dissolved Organic Carbon as a Component of the Biological Pump in the North Atlantic Ocean [and Discussion] , 1995 .
[22] A. Oschlies. Model-derived estimates of new production: New results point towards lower values , 2001 .
[23] J. G. Field,et al. General allometric equations for rates of nutrient uptake, ingestion, and respiration in plankton organisms , 1989 .
[24] David M. Karl,et al. Seasonal and interannual variability in primary production and particle flux at Station ALOHA , 1996 .
[25] Frank Lunkeit,et al. Earth system models of intermediate complexity: closing the gap in the spectrum of climate system models , 2002 .
[26] Paul G. Falkowski,et al. Evolution of the nitrogen cycle and its influence on the biological sequestration of CO2 in the ocean , 1997, Nature.
[27] F. A. Richards,et al. The influence of organisms on the composition of sea-water , 1963 .
[28] J. Steele,et al. The role of predation in plankton models , 1992 .
[29] S. Doney. Major challenges confronting marine biogeochemical modeling , 1999 .
[30] Farooq Azam,et al. Microbial Control of Oceanic Carbon Flux: The Plot Thickens , 1998, Science.
[31] J. Riley. Progress in Oceanography , 1964, Nature.
[32] P. Boyd,et al. Does planktonic community structure determine downward particulate organic carbon flux in different oceanic provinces , 1999 .
[33] A. M. Edwards,et al. Zooplankton mortality and the dynamical behaviour of plankton population models , 1999, Bulletin of mathematical biology.
[34] J. Wroblewski,et al. A model of phytoplankton plume formation during variable Oregon upwelling , 1977 .
[35] James J. Elser,et al. Organism size, life history, and N:P stoichiometry , 1996 .
[36] M. Collins,et al. Projections of future climate change , 2002 .
[37] J. Houghton,et al. Climate change 2001 : the scientific basis , 2001 .
[38] R. Goericke,et al. Primary production in the subarctic Pacific Ocean: Project SUPER , 1993 .
[39] Paul G. Falkowski,et al. Primary Productivity and Biogeochemical Cycles in the Sea , 1992 .
[40] K. Denman,et al. A coupled 1-D biological/physical model of the northeast subarctic Pacific Ocean with iron limitation , 1999 .
[41] A. Gargett. Physical processes and the maintenance of nutrient‐rich euphotic zones , 1991 .
[42] R. Eppley,et al. Ammonium distribution in southern California coastal waters and its role in the growth of phytoplankton1 , 1979 .
[43] Patrick Raimbault,et al. Size fraction of phytoplankton in the Ligurian Sea and the Algerian Basin (Mediterranean Sea): size distribution versus total concentration , 1988 .
[44] Richard J. Matear,et al. Parameter optimization and analysis of ecosystem models using simulated annealing: a case study at Station P , 1995 .
[45] K. Denman,et al. Simulation of the planktonic ecosystem response to pre- and post-1976 forcing in an isopycnic model of the North Pacific , 2001 .
[46] W. K. Johnson,et al. Seasonal and interannual variability in particle fluxes of carbon, nitrogen and silicon from time series of sediment traps at Ocean Station P, 1982–1993: relationship to changes in subarctic primary productivity , 1999 .
[47] V. A. Ryabchenko,et al. Chaotic behaviour of an ocean ecosystem model under seasonal external forcing , 1997 .
[48] G. Evans,et al. The role of local models and data sets in the Joint Global Ocean Flux Study , 1999 .
[49] Andrew M. Edwards,et al. Adding Detritus to a Nutrient–Phytoplankton–Zooplankton Model:A Dynamical-Systems Approach , 2001 .
[50] D. Hutchins,et al. Size-fractionated biological iron and carbon uptake along a coastal to offshore transect in the NE Pacific , 1999 .
[51] S. Doney,et al. An intermediate complexity marine ecosystem model for the global domain , 2001 .
[52] M. Fasham. Variations in the seasonal cycle of biological production in subarctic oceans: A model sensitivity analysis , 1995 .
[53] W. Sunda,et al. Interrelated influence of iron, light and cell size on marine phytoplankton growth , 1997, Nature.
[54] K. Denman,et al. Simulations of Marine Ecosystem Response to Climate Variation with a One Dimensional Coupled Ecosystem/Mixed Layer Model , 2002 .
[55] Donald L. DeAngelis,et al. Multiple nutrient limitations in ecological models , 1989 .
[56] Ricardo M Letelier,et al. Ecosystem changes in the North Pacific subtropical gyre attributed to the 1991–92 El Niño , 1995, Nature.
[57] J. G. Field,et al. The size-based dynamics of plankton food webs. I. A simulation model of carbon and nitrogen flows , 1991 .
[58] K. Denman,et al. The response of two coupled one-dimensional mixed layer/planktonic ecosystem models to climate change in the NE subarctic Pacific Ocean , 2002 .
[59] J. Steele. Incorporating the microbial loop in a simple plankton model , 1998, Proceedings of the Royal Society of London. Series B: Biological Sciences.
[60] B. Irwin,et al. The kinetics of nitrogen utilization in the oceanic mixed layer: Nitrate and ammonium interactions at nanomolar concentrations , 1996 .
[61] Andrew M. Edwards,et al. The role of higher predation in plankton population models , 2000 .
[62] F. Chai,et al. Iron and grazing constraints on primary production in the central equatorial Pacific: An EqPac synthesis , 1997 .
[63] P. Harrison,et al. Seasonal variability in nitrogenous nutrition of phytoplankton assemblages in the northeastern subarctic Pacific Ocean , 1999 .
[64] H. Ducklow,et al. A nitrogen-based model of plankton dynamics in the oceanic mixed layer , 1990 .
[65] M. M. Mullin,et al. Relation between biomass and body weight of plankton in a steady state oceanic ecosystem1 , 1986 .
[66] David M. Glover,et al. A new coupled, one-dimensional biological-physical model for the upper ocean: Applications to the JGOFS Bermuda Atlantic Time-series Study (BATS) site , 1996 .
[67] R. W. Sheldon,et al. The Size Distribution of Particles in the OCEAN1 , 1972 .
[68] J. McCarthy,et al. Nitrogenous nutrition of the plankton in the Chesapeake Bay. 1. Nutrient availability and phytoplankton preferences , 1977 .
[69] R. Riegman,et al. The relative preference index (RPI) for phytoplankton nitrogen use is only weakly related to physiological preference , 1996 .
[70] W. G. Sprules,et al. Plankton Size Spectra in Relation to Ecosystem Productivity, Size, and Perturbation , 1986 .
[71] D. Olson,et al. Modelling pelagic biogeography , 1994 .
[72] V. A. Ryabchenko,et al. What causes short-term oscillations in ecosystem models of the ocean mixed layer? , 1997 .