해양 생물기원 DMS에 의한 북극 대기 미세입자 형성 관측

Doctor Atmospheric new particle formation and growth significantly influence climate by supplying new seeds for cloud condensation. Thus, observations of chemical processes in the atmosphere are crucial to understanding and predicting climate change. There is still a lack of knowledge on whether and...

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Main Author: 장세현
Other Authors: 환경공학부
Format: Thesis
Language:English
Published: 포항공과대학교 2021
Subjects:
Online Access:http://postech.dcollection.net/common/orgView/200000506926
https://oasis.postech.ac.kr/handle/2014.oak/114200
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spelling ftponangunivst:oai:oasis.postech.ac.kr:2014.oak/114200 2023-05-15T14:46:08+02:00 해양 생물기원 DMS에 의한 북극 대기 미세입자 형성 관측 Contribution of dimethyl sulfide to new particle formation in the Arctic atmosphere 장세현 환경공학부 2021- 8 http://postech.dcollection.net/common/orgView/200000506926 https://oasis.postech.ac.kr/handle/2014.oak/114200 eng eng 포항공과대학교 OAK-2015-09653 http://postech.dcollection.net/common/orgView/200000506926 https://oasis.postech.ac.kr/handle/2014.oak/114200 Thesis 2021 ftponangunivst 2022-11-04T01:29:45Z Doctor Atmospheric new particle formation and growth significantly influence climate by supplying new seeds for cloud condensation. Thus, observations of chemical processes in the atmosphere are crucial to understanding and predicting climate change. There is still a lack of knowledge on whether and how marine biota emissions affect aerosol-cloud-climate interactions in the Arctic. Among many naturally produced gases, dimethyl sulfide (DMS) plays an important role in atmospheric sulfur budgets and radiative balance, having potentially climate-cooling effects. Especially during the bloom and post-bloom period when the anthropogenic influence is limited and biological activity is high, the marine biological DMS is of great importance for cloud formation. The harsh environment of the Arctic makes it difficult to perform in situ measurements of atmospheric DMS and related aerosols. But more measurements in the Arctic need to be successfully accomplished because the Arctic is the best place for evaluating the impact of DMS and its oxidation products (e.g. H2SO4 and MSA) on particle formation and growth, further radiative forcing. For this dissertation study, I conducted research that developing an analytical system capable of continuous measurement of atmospheric DMS and proving the robustness of the system (Chapter 2). And I collected aerosol samples (PM 2.5) to quantify the concentration of oxidation products of DMS in the Arctic atmosphere and elucidate the factors controlling the seasonal- and interannual variability of them (Chapter 3). By applying stable S isotope measurement technique, source apportionment of sulfate aerosols and the relationship between biogenic sulfate and fine aerosol particles were investigated (Chapter 4). First, I developed an analytical system capable of continuous measurement of atmospheric DMS at pptv levels. The system uses customized devices for detector calibration and for DMS trapping and desorption that are controlled using a data acquisition system designed to maximize the ... Thesis Arctic Climate change Pohang University of Science and Technology (POSTECH): Open Access System for Information Sharing (OASIS) Arctic
institution Open Polar
collection Pohang University of Science and Technology (POSTECH): Open Access System for Information Sharing (OASIS)
op_collection_id ftponangunivst
language English
description Doctor Atmospheric new particle formation and growth significantly influence climate by supplying new seeds for cloud condensation. Thus, observations of chemical processes in the atmosphere are crucial to understanding and predicting climate change. There is still a lack of knowledge on whether and how marine biota emissions affect aerosol-cloud-climate interactions in the Arctic. Among many naturally produced gases, dimethyl sulfide (DMS) plays an important role in atmospheric sulfur budgets and radiative balance, having potentially climate-cooling effects. Especially during the bloom and post-bloom period when the anthropogenic influence is limited and biological activity is high, the marine biological DMS is of great importance for cloud formation. The harsh environment of the Arctic makes it difficult to perform in situ measurements of atmospheric DMS and related aerosols. But more measurements in the Arctic need to be successfully accomplished because the Arctic is the best place for evaluating the impact of DMS and its oxidation products (e.g. H2SO4 and MSA) on particle formation and growth, further radiative forcing. For this dissertation study, I conducted research that developing an analytical system capable of continuous measurement of atmospheric DMS and proving the robustness of the system (Chapter 2). And I collected aerosol samples (PM 2.5) to quantify the concentration of oxidation products of DMS in the Arctic atmosphere and elucidate the factors controlling the seasonal- and interannual variability of them (Chapter 3). By applying stable S isotope measurement technique, source apportionment of sulfate aerosols and the relationship between biogenic sulfate and fine aerosol particles were investigated (Chapter 4). First, I developed an analytical system capable of continuous measurement of atmospheric DMS at pptv levels. The system uses customized devices for detector calibration and for DMS trapping and desorption that are controlled using a data acquisition system designed to maximize the ...
author2 환경공학부
format Thesis
author 장세현
spellingShingle 장세현
해양 생물기원 DMS에 의한 북극 대기 미세입자 형성 관측
author_facet 장세현
author_sort 장세현
title 해양 생물기원 DMS에 의한 북극 대기 미세입자 형성 관측
title_short 해양 생물기원 DMS에 의한 북극 대기 미세입자 형성 관측
title_full 해양 생물기원 DMS에 의한 북극 대기 미세입자 형성 관측
title_fullStr 해양 생물기원 DMS에 의한 북극 대기 미세입자 형성 관측
title_full_unstemmed 해양 생물기원 DMS에 의한 북극 대기 미세입자 형성 관측
title_sort 해양 생물기원 dms에 의한 북극 대기 미세입자 형성 관측
publisher 포항공과대학교
publishDate 2021
url http://postech.dcollection.net/common/orgView/200000506926
https://oasis.postech.ac.kr/handle/2014.oak/114200
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
genre_facet Arctic
Climate change
op_relation OAK-2015-09653
http://postech.dcollection.net/common/orgView/200000506926
https://oasis.postech.ac.kr/handle/2014.oak/114200
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