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Exploring the Roles of Iron and Irradiance in Dynamics of Diatoms and Phaeocystis in the Amundsen Sea Continental Shelf Water

Cited 3 time in wos
Cited 6 time in scopus

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dc.contributor.authorKwon, Young Shin-
dc.contributor.authorLa, Hyoung Sul-
dc.contributor.authorJung, Jinyoung-
dc.contributor.authorLee, Sang Heon-
dc.contributor.authorKim, Tae-Wan-
dc.contributor.authorKang, Hyoun-Woo-
dc.contributor.authorLee, SangHoon-
dc.date.accessioned2022-07-07T00:25:55Z-
dc.date.available2022-07-07T00:25:55Z-
dc.date.issued2021-03-
dc.identifier.urihttps://repository.kopri.re.kr/handle/201206/13548-
dc.description.abstractThe Amundsen Sea continental shelf (ACS) water ecosystem is expected to undergo changes since increasing melt rate of glacier and decreasing sea ice extent by global warming would lead to the mitigation of iron and light limitation. We investigated how diatoms and Phaeocystis, two dominant taxa, and primary production in the ACS water would respond to variations in iron and light availabilities by using a 1-D pelagic ecosystem model. In the model, we added sea ice effects that reduce light penetration and optimized model parameters for diatoms and Phaeocystis. The results from our model showed good agreement with 20-year observations of Chl-a as well as the biomass proportion of diatoms and Phaeocystis and nutrient distributions during the growing season. Our model experimental results suggest that the current moderate iron and high light conditions favor the growth of Phaeocystis over diatoms. Moreover, as iron increases, the organic carbon exudation by phytoplankton increases more rapidly than net primary production (NPP), leading to a decline in phytoplankton biomass. On the other hand, irradiance plays a role in controlling NPP in terms of photoinhibition which is reduced by increasing iron. Increases in both iron and irradiance lead to an advance in the timing of the bloom peak (surface Chl-a maximum) due to increases in phytoplankton carbon loss and photoinhibition. Our results imply that the dominance of Phaeocystis can continue and that the carbon uptake capacity of the ACS in the summer seasons might increase given that iron availability will increase with future climate change.en_US
dc.languageEnglishen_US
dc.language.isoenen_US
dc.subjectOceanographyen_US
dc.subject.classification해당사항없음en_US
dc.titleExploring the Roles of Iron and Irradiance in Dynamics of Diatoms and Phaeocystis in the Amundsen Sea Continental Shelf Wateren_US
dc.title.alternative아문젠해 규조류와 패오시스티스의 역학에 대한 철과 일사량의 역할 이해 연구en_US
dc.typeArticleen_US
dc.identifier.bibliographicCitationKwon, Young Shin, et al. 2021. "Exploring the Roles of Iron and Irradiance in Dynamics of Diatoms and Phaeocystis in the Amundsen Sea Continental Shelf Water". <em>JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS</em>, 126(3): 1-23.-
dc.citation.titleJOURNAL OF GEOPHYSICAL RESEARCH-OCEANSen_US
dc.citation.volume126en_US
dc.citation.number3en_US
dc.identifier.doi10.1029/2020JC016673-
dc.citation.startPage1en_US
dc.citation.endPage23en_US
dc.description.articleClassificationSCIE-
dc.description.jcrRateJCR 2019:10.448en_US
dc.identifier.localId2021-0293-
dc.identifier.scopusid2-s2.0-85103170582-
dc.identifier.wosid000636285300013-
Appears in Collections  
2021-2021, Carbon cycle change and ecosystem response under the Southern Ocean warming (21-21) / Park, Jisoo (PE21110)
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