A model-based analysis of physical and biological controls on ice algal and pelagic primary production in Resolute Passage

dc.contributor.authorMortenson, Eric
dc.contributor.authorHayashida, Hakase
dc.contributor.authorSteiner, Nadja
dc.contributor.authorMonahan, Adam H.
dc.contributor.authorBlais, Marjolaine
dc.contributor.authorGale, Matthew A.
dc.contributor.authorGalindo, Virginie
dc.contributor.authorGosselin, Michel
dc.contributor.authorHu, Xianmin
dc.contributor.authorLavoie, Diane
dc.contributor.authorMundy, Christopher John
dc.date.accessioned2018-10-10T12:29:52Z
dc.date.available2018-10-10T12:29:52Z
dc.date.copyright2017en_US
dc.date.issued2017
dc.description.abstractA coupled 1-D sea ice-ocean physical-biogeochemical model was developed to investigate the processes governing ice algal and phytoplankton blooms in the seasonally ice-covered Arctic Ocean. The 1-D column is representative of one grid cell in 3-D model applications and provides a tool for parameterization -development. The model was applied to Resolute Passage in the Canadian Arctic Archipelago and assessed with observations from a field campaign during spring of 2010. The factors considered to limit the growth of simulated ice algae and phytoplankton were light, nutrients, and in the case of ice algae, ice melt. In -addition to the standard simulation, several model experiments were conducted to determine the sensitivity of the simulated ice algal bloom to parameterizations of light, mortality, and pre-bloom biomass. Model results indicated that: (1) ice algae limit subsequent pelagic productivity in the upper 10 m by depleting nutrients to limiting levels; (2) light availability and pre-bloom biomass determine the onset timing of the ice algal bloom; (3) the maximum biomass is relatively insensitive to the pre-bloom biomass, but is limited by nutrient availability; (4) a combination of linear and quadratic parameterizations of mortality rate is required to adequately simulate the evolution of the ice algal bloom; and (5) a sinking rate for large detritus greater than a threshold of similar to 10 m d(-1) effectively strips the surface waters of the limiting nutrient (silicate) after the ice algal bloom, supporting the development of a deep chlorophyll maximum.en_US
dc.description.reviewstatusRevieweden_US
dc.description.scholarlevelFacultyen_US
dc.description.sponsorshipEM and HH were funded via the NETCARE and ArcticNet projects. NS and DL were supported by Fisheries and Oceans Canada. VG, MG, AM, and CJM were supported by funding from Natural Sciences and Engineering Research Council of Canada (NSERC), Fonds de recherche du Quebec Nature et Technologies (FRQNT), Canada Economic Development and Polar Continental Shelf Program (PCSP) of Natural Resources Canada.en_US
dc.identifier.citationMortenson, E.; Hayshida, H.; Steiner, N.; Monahan, A.; Blais, M.; Gale, M.A.; … & Mundy, C.J. (2017). A model-based analysis of physical and biological controls on ice algal and pelagic primary production in Resolute Passage. Elementa: Science of the Anthropocene, 5, article 39. https://doi.org/10.1525/elementa.229en_US
dc.identifier.urihttps://doi.org/10.1525/elementa.229
dc.identifier.urihttp://hdl.handle.net/1828/10144
dc.language.isoenen_US
dc.publisherElementa: Science of the Anthropoceneen_US
dc.subjectsea ice algaeen_US
dc.subjectbiogeochemistry modelen_US
dc.subjectmarine Arcticen_US
dc.subjectprimary productionen_US
dc.titleA model-based analysis of physical and biological controls on ice algal and pelagic primary production in Resolute Passageen_US
dc.typeArticleen_US

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