2016GB005615_Manuscript_Revised.docx (112.65 kB)
Variability in the mechanisms controlling Southern Ocean phytoplankton bloom phenology in an ocean model and satellite observations
journal contributionposted on 2023-07-17, 06:05 authored by Tyler RohrTyler Rohr, Matthew C Long, Maria T Kavanaugh, Keith Lindsay, Scott C Doney
A coupled global numerical simulation (conducted with the Community Earth System Model) is used in conjunction with satellite remote sensing observations to examine the role of top-down (grazing pressure) and bottom-up (light, nutrients) controls on marine phytoplankton bloom dynamics in the Southern Ocean. Phytoplankton seasonal phenology is evaluated in the context of the recently proposed “disturbance-recovery” hypothesis relative to more traditional, exclusively “bottom-up” frameworks. All blooms occur when phytoplankton division rates exceed loss rates to permit sustained net population growth; however, the nature of this decoupling period varies regionally in Community Earth System Model. Regional case studies illustrate how unique pathways allow blooms to emerge despite very poor division rates or very strong grazing rates. In the Subantarctic, southeast Pacific small spring blooms initiate early cooccurring with deep mixing and low division rates, consistent with the disturbance-recovery hypothesis. Similar systematics are present in the Subantarctic, southwest Atlantic during the spring but are eclipsed by a subsequent, larger summer bloom that is coincident with shallow mixing and the annual maximum in division rates, consistent with a bottom-up, light limited framework. In the model simulation, increased iron stress prevents a similar summer bloom in the southeast Pacific. In the simulated Antarctic zone (70°S–65°S) seasonal sea ice acts as a dominant phytoplankton-zooplankton decoupling agent, triggering a delayed but substantial bloom as ice recedes. Satellite ocean color remote sensing and ocean physical reanalysis products do not precisely match model-predicted phenology, but observed patterns do indicate regional variability in mechanism across the Atlantic and Pacific.
Publication titleGLOBAL BIOGEOCHEMICAL CYCLES
PublisherAMER GEOPHYSICAL UNION
Rights statementCopyright 2017 American Geophysical Union. All Rights Reserved. This is the author manuscript accepted for publication and has undergone full peer review but has not been through the copyediting, typesetting, pagination and proofreading process, which may lead to differences between this version and the Version of Record. Please cite this article as doi: 10.1002/2016GB005615
Science & TechnologyLife Sciences & BiomedicinePhysical SciencesEnvironmental SciencesGeosciences, MultidisciplinaryMeteorology & Atmospheric SciencesEnvironmental Sciences & EcologyGeologyEARTH SYSTEM MODELSURFACE WATERSNORTH-ATLANTICGROWTH-RATESGLOBAL OCEANTIME-SERIESCARBON FLUXROSS SEAIRONDISTRIBUTIONS