A study on the role of sea ice in the nitrous oxide cycle in the Prydz Bay, Antarctica

N2O is one of the most important greenhouse gases and ozone depletor, which was a matter of more and more concerned. The Southern Ocean was considered as one of the most important N2O source and was believed to account for ~1/4 of oceanic budget. However, there is uncertainty about this budget due t...

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Main Authors: Man Wu, Liyang Zhan, Jian Liu, Jiexia Zhang, Wangwang Ye, Bruno Delille
Format: Article
Language:English
Published: Frontiers Media S.A. 2024-12-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2024.1495913/full
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author Man Wu
Liyang Zhan
Jian Liu
Jiexia Zhang
Wangwang Ye
Bruno Delille
author_facet Man Wu
Liyang Zhan
Jian Liu
Jiexia Zhang
Wangwang Ye
Bruno Delille
author_sort Man Wu
collection DOAJ
description N2O is one of the most important greenhouse gases and ozone depletor, which was a matter of more and more concerned. The Southern Ocean was considered as one of the most important N2O source and was believed to account for ~1/4 of oceanic budget. However, there is uncertainty about this budget due to limited data availability. In this study, field and lab works were conducted for better understanding of N2O dynamics during sea ice melting and sea ice formation. In the field study, taking advantage of the Chinese Antarctic cruise, a 10 days’ time series study was carried out at a station in the Prydz Bay, Antarctica, where, surface water N2O was observed continuously, and the adjacent ice cores were taken for N2O analysis. In the lab, an ice growing simulation system was constructed to study the N2O dynamics during the sea ice formation. The result of endmember mixing models and calculation of N2O partition in three phases during sea ice formation provide important information about the dynamics of N2O during ice melting and sea ice formation processes, that is, the sea ice melting regulated N2O concentration and saturation status, which can be an explanation for reported N2O undersaturation observed in polar oceans, whereas during the sea ice formation, most of the N2O will be expelled to the deeper water while a small amount of retain the sea ice and less amount of N2O release to the atmosphere.
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institution Kabale University
issn 2296-7745
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publishDate 2024-12-01
publisher Frontiers Media S.A.
record_format Article
series Frontiers in Marine Science
spelling doaj-art-11c3d3499262473199ba78bbab79687e2024-12-18T14:17:39ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452024-12-011110.3389/fmars.2024.14959131495913A study on the role of sea ice in the nitrous oxide cycle in the Prydz Bay, AntarcticaMan Wu0Liyang Zhan1Jian Liu2Jiexia Zhang3Wangwang Ye4Bruno Delille5Key Laboratory of Global Change and Marine-Atmospheric Chemistry, Third Institute of Oceanography, Ministry of Natural Resources, Xiamen, ChinaKey Laboratory of Global Change and Marine-Atmospheric Chemistry, Third Institute of Oceanography, Ministry of Natural Resources, Xiamen, ChinaKey Laboratory of Global Change and Marine-Atmospheric Chemistry, Third Institute of Oceanography, Ministry of Natural Resources, Xiamen, ChinaKey Laboratory of Global Change and Marine-Atmospheric Chemistry, Third Institute of Oceanography, Ministry of Natural Resources, Xiamen, ChinaKey Laboratory of Global Change and Marine-Atmospheric Chemistry, Third Institute of Oceanography, Ministry of Natural Resources, Xiamen, ChinaUnité d’océanographie chimique, The Freshwater and OCeanic science Unit of reSearch (FOCUS), Universite de Liege, Liege, BelgiumN2O is one of the most important greenhouse gases and ozone depletor, which was a matter of more and more concerned. The Southern Ocean was considered as one of the most important N2O source and was believed to account for ~1/4 of oceanic budget. However, there is uncertainty about this budget due to limited data availability. In this study, field and lab works were conducted for better understanding of N2O dynamics during sea ice melting and sea ice formation. In the field study, taking advantage of the Chinese Antarctic cruise, a 10 days’ time series study was carried out at a station in the Prydz Bay, Antarctica, where, surface water N2O was observed continuously, and the adjacent ice cores were taken for N2O analysis. In the lab, an ice growing simulation system was constructed to study the N2O dynamics during the sea ice formation. The result of endmember mixing models and calculation of N2O partition in three phases during sea ice formation provide important information about the dynamics of N2O during ice melting and sea ice formation processes, that is, the sea ice melting regulated N2O concentration and saturation status, which can be an explanation for reported N2O undersaturation observed in polar oceans, whereas during the sea ice formation, most of the N2O will be expelled to the deeper water while a small amount of retain the sea ice and less amount of N2O release to the atmosphere.https://www.frontiersin.org/articles/10.3389/fmars.2024.1495913/fullsea icenitrous oxidePrydz BayPolar oceangreenhouse gas
spellingShingle Man Wu
Liyang Zhan
Jian Liu
Jiexia Zhang
Wangwang Ye
Bruno Delille
A study on the role of sea ice in the nitrous oxide cycle in the Prydz Bay, Antarctica
Frontiers in Marine Science
sea ice
nitrous oxide
Prydz Bay
Polar ocean
greenhouse gas
title A study on the role of sea ice in the nitrous oxide cycle in the Prydz Bay, Antarctica
title_full A study on the role of sea ice in the nitrous oxide cycle in the Prydz Bay, Antarctica
title_fullStr A study on the role of sea ice in the nitrous oxide cycle in the Prydz Bay, Antarctica
title_full_unstemmed A study on the role of sea ice in the nitrous oxide cycle in the Prydz Bay, Antarctica
title_short A study on the role of sea ice in the nitrous oxide cycle in the Prydz Bay, Antarctica
title_sort study on the role of sea ice in the nitrous oxide cycle in the prydz bay antarctica
topic sea ice
nitrous oxide
Prydz Bay
Polar ocean
greenhouse gas
url https://www.frontiersin.org/articles/10.3389/fmars.2024.1495913/full
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