Antarctic meltwater-induced dynamical changes in phytoplankton in the Southern Ocean

It has been suggested that the freshwater flux due to the recent melting of the Antarctic ice-sheet/shelf will suppress ventilation in the Southern Ocean (SO). In this study, we performed idealized earth-system simulations to examine the impacts of Antarctic meltwater on the biomass of surface phyto...

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Main Authors: Ji-Hoon Oh, Kyung Min Noh, Hyung-Gyu Lim, Emilia Kyung Jin, Sang-Yoon Jun, Jong-Seong Kug
Format: Article
Language:English
Published: IOP Publishing 2022-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/ac444e
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author Ji-Hoon Oh
Kyung Min Noh
Hyung-Gyu Lim
Emilia Kyung Jin
Sang-Yoon Jun
Jong-Seong Kug
author_facet Ji-Hoon Oh
Kyung Min Noh
Hyung-Gyu Lim
Emilia Kyung Jin
Sang-Yoon Jun
Jong-Seong Kug
author_sort Ji-Hoon Oh
collection DOAJ
description It has been suggested that the freshwater flux due to the recent melting of the Antarctic ice-sheet/shelf will suppress ventilation in the Southern Ocean (SO). In this study, we performed idealized earth-system simulations to examine the impacts of Antarctic meltwater on the biomass of surface phytoplankton in the Antarctic Ocean. The enhanced stratification due to the meltwater leads to a decrease in surface nitrate concentration, but an increase in the surface concentration of dissolved iron. These changes are associated with the reduced upwelling of nitrate-rich deep water and the trapped iron exported from terrestrial sediment. Because of the limited iron availability in the SO, the trapped iron in surface water enhances the chlorophyll concentration in the open ocean. However, in the marginal sea along the Antarctic coastline where the iron is relatively sufficient, a nitrate reduction induces a chlorophyll decrease, indicating a regime shift from iron-limited to nitrate-limited conditions.
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spelling doaj.art-81a25b5b233a492aa706dd2d0b94fddb2023-08-09T15:23:28ZengIOP PublishingEnvironmental Research Letters1748-93262022-01-0117202402210.1088/1748-9326/ac444eAntarctic meltwater-induced dynamical changes in phytoplankton in the Southern OceanJi-Hoon Oh0https://orcid.org/0000-0001-8484-8997Kyung Min Noh1Hyung-Gyu Lim2Emilia Kyung Jin3Sang-Yoon Jun4Jong-Seong Kug5https://orcid.org/0000-0003-2251-2579Division of Environmental Science and Engineering, Pohang University of Science and Technology (POSTECH) , Pohang 37673, Republic of KoreaDivision of Environmental Science and Engineering, Pohang University of Science and Technology (POSTECH) , Pohang 37673, Republic of KoreaDivision of Environmental Science and Engineering, Pohang University of Science and Technology (POSTECH) , Pohang 37673, Republic of Korea; Princeton University/Atmosphere and Oceanic Sciences Program , Princeton, NJ 08540, United States of AmericaKorea Polar Research Institute (KOPRI) , Incheon 21990, Republic of KoreaKorea Polar Research Institute (KOPRI) , Incheon 21990, Republic of KoreaDivision of Environmental Science and Engineering, Pohang University of Science and Technology (POSTECH) , Pohang 37673, Republic of Korea; Institute for Convergence Research and Education in Advanced Technology, Yonsei University , Seoul, Republic of KoreaIt has been suggested that the freshwater flux due to the recent melting of the Antarctic ice-sheet/shelf will suppress ventilation in the Southern Ocean (SO). In this study, we performed idealized earth-system simulations to examine the impacts of Antarctic meltwater on the biomass of surface phytoplankton in the Antarctic Ocean. The enhanced stratification due to the meltwater leads to a decrease in surface nitrate concentration, but an increase in the surface concentration of dissolved iron. These changes are associated with the reduced upwelling of nitrate-rich deep water and the trapped iron exported from terrestrial sediment. Because of the limited iron availability in the SO, the trapped iron in surface water enhances the chlorophyll concentration in the open ocean. However, in the marginal sea along the Antarctic coastline where the iron is relatively sufficient, a nitrate reduction induces a chlorophyll decrease, indicating a regime shift from iron-limited to nitrate-limited conditions.https://doi.org/10.1088/1748-9326/ac444eAntarctic meltwaterAntarctic ice-sheet/shelfSouthern Oceanchlorophyllphytoplankton
spellingShingle Ji-Hoon Oh
Kyung Min Noh
Hyung-Gyu Lim
Emilia Kyung Jin
Sang-Yoon Jun
Jong-Seong Kug
Antarctic meltwater-induced dynamical changes in phytoplankton in the Southern Ocean
Environmental Research Letters
Antarctic meltwater
Antarctic ice-sheet/shelf
Southern Ocean
chlorophyll
phytoplankton
title Antarctic meltwater-induced dynamical changes in phytoplankton in the Southern Ocean
title_full Antarctic meltwater-induced dynamical changes in phytoplankton in the Southern Ocean
title_fullStr Antarctic meltwater-induced dynamical changes in phytoplankton in the Southern Ocean
title_full_unstemmed Antarctic meltwater-induced dynamical changes in phytoplankton in the Southern Ocean
title_short Antarctic meltwater-induced dynamical changes in phytoplankton in the Southern Ocean
title_sort antarctic meltwater induced dynamical changes in phytoplankton in the southern ocean
topic Antarctic meltwater
Antarctic ice-sheet/shelf
Southern Ocean
chlorophyll
phytoplankton
url https://doi.org/10.1088/1748-9326/ac444e
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AT hyunggyulim antarcticmeltwaterinduceddynamicalchangesinphytoplanktoninthesouthernocean
AT emiliakyungjin antarcticmeltwaterinduceddynamicalchangesinphytoplanktoninthesouthernocean
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