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Study of the nutrient and plankton dynamics in Lake Tanganyika using a reduced-gravity model

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dc.contributor Australian Institute Of Marine Science
dc.contributor Inst Astron & Geophys Georges Lemaitre
dc.contributor Lab Ecol Eaux Douces
dc.contributor Ctr Syst Engn & Appl Mech
dc.contributor Fac Univ Notre Dame Paix
dc.contributor Australian Inst Marine Sci
dc.contributor Universite Catholique Louvain
dc.contributor Univ Catholique Louvain
dc.contributor University Of Namur
dc.contributor Australian Institute Of Marine Science (aims) en
dc.contributor.author WOLANSKI, ERIC
dc.contributor.author NAITHANI, JAYA
dc.contributor.author DARCHAMBEAU, FRANCOIS
dc.contributor.author DELEERSNIJDER, ERIC
dc.contributor.author DESCY, JEAN-PIERRE
dc.date.accessioned 2017-03-21T00:52:59Z
dc.date.accessioned 2017-03-21T00:52:59Z
dc.date.accessioned 2013-02-28T06:44:45Z
dc.date.accessioned 2019-05-09T01:10:28Z
dc.date.available 2013-02-28T06:44:45Z
dc.date.available 2013-02-28T06:44:45Z
dc.date.available 2017-03-21T00:52:59Z
dc.date.available 2019-05-09T01:10:28Z
dc.date.issued 2007-01-10
dc.identifier 7383 en
dc.identifier.citation Naithani J, Darchambeau F, Deleersnijder E, Descy J-P and Wolanski EJ (2007) Study of nutrient and plankton dynamics in Lake Tanganyika using a reduced-gravity model. Ecological Modelling. 200: 225-233. en
dc.identifier.issn 0304-3800
dc.identifier.uri http://epubs.aims.gov.au/11068/7383
dc.description Link to abstract/full text - http://dx.doi.org/10.1016/j.ecolmodel.2006.07.035 en
dc.description.abstract An eco-hydrodynamic (ECOH) model is proposed for Lake Tanganyika to study the plankton productivity. The hydrodynamic sub-model solves the non-linear, reduced-gravity equations in which wind is the dominant forcing. The ecological sub-model for the epilimnion comprises nutrients, primary production, phytoplankton biomass and zooplankton biomass. In the absence of significant terrestrial input of nutrients, the nutrient loss is compensated for by seasonal, wind-driven, turbulent entrainment of nutrient-rich hypolimnion water into the epilimnion, which gives rise to high plankton productivity twice in the year, during the transition between two seasons. Model simulations predict well the seasonal contrasts of the measured physical and ecological parameters. Numerical tests indicate that the half saturation constant for grazing by zooplankton and the fish predation rate on zooplankton affect the zooplankton biomass measurably more than that of phytoplankton biomass. This work has implications for the application of this model to predict the climatological biological productivity of Lake Tanganyika. (c) 2006 Elsevier B.V. All rights reserved.
dc.description.uri http://dx.doi.org/10.1016/j.ecolmodel.2006.07.035 en
dc.language English
dc.language en en
dc.relation.ispartof Ecological Modelling - pages: 200: 225-233 en
dc.relation.ispartof Null
dc.subject Phytoplankton
dc.subject Ecology
dc.subject Phosphorus
dc.subject Plankton Productivity
dc.subject Growth
dc.subject Stoichiometry
dc.subject Reservoirs
dc.subject Water-quality
dc.subject Lake Tanganyika
dc.subject Trophic State
dc.subject Environmental Sciences & Ecology
dc.subject Rates
dc.subject Ecological Modelling
dc.subject Carbon
dc.title Study of the nutrient and plankton dynamics in Lake Tanganyika using a reduced-gravity model
dc.type journal article en
dc.identifier.doi 10.1016/j.ecolmodel.2006.07.035
dc.identifier.wos WOS:000243600800022


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