Synchronicity between ice retreat and phytoplankton bloom in circum-Antarctic polynyas

International audience Phytoplankton in Antarctic coastal polynyas has a temporally short yet spatially variant growthwindow constrained by ice cover and day length. Using 18-year satellite measurements (1997–2015) of seaice and chlorophyll concentrations, we assessed the synchronicity between the s...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Li, Yun, Ji, Rubao, Jenouvrier, Stéphanie, Jin, Meibing, Stroeve, Julienne
Other Authors: College of Marine Science St Petersburg, FL, University of South Florida Tampa (USF), Biology Department - Woods Hole Oceanographic Institution, Woods Hole Oceanographic Institution (WHOI), Biology Department (WHOI), Centre d'Études Biologiques de Chizé - UMR 7372 (CEBC), Université de La Rochelle (ULR)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE), International Arctic Research Center (IARC), University of Alaska Fairbanks (UAF), Center for Polar Observation and Modelling, University College of London London (UCL), National Snow and Ice Data Center (NSIDC), University of Colorado Boulder
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2016
Subjects:
[SDE]Environmental Sciences
Antarctic
Antarc*
Sea ice
Online Access:https://hal.archives-ouvertes.fr/hal-01358134
https://doi.org/10.1002/2016GL067937
Description
Summary:International audience Phytoplankton in Antarctic coastal polynyas has a temporally short yet spatially variant growthwindow constrained by ice cover and day length. Using 18-year satellite measurements (1997–2015) of seaice and chlorophyll concentrations, we assessed the synchronicity between the spring phytoplankton bloomand light availability, taking into account the ice cover and the incident solar irradiance, for 50 circum-Antarcticcoastal polynyas. The synchronicity was strong (i.e., earlier ice-adjusted light onset leads to earlier bloom andvice versa) in most of the western Antarctic polynyas but weak in a majority of the eastern Antarctic polynyas.The west-east asymmetry is related to sea ice production rate: the formation ofmany eastern Antarctic polynyasis associated with strong katabatic wind and high sea ice production rate, leading to stronger water columnmixing that could damp phytoplankton blooms and weaken the synchronicity.

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