Acknowledgement
본 연구는 한국해양과학기술원 부설 극지연구소에서 해양수산부의 재원으로 수행하는 극지 해양환경 및 해저조사 연구사업(KIMST Grant 20210632)과 과학기술 정보통신부의재원으로 한국연구재단에서 지원하는 신진 연구 및 기초연구실 지원과제(NRF-2022R1C1C1003385 및 NRF-2022R1A4A3027001)의 지원을 받아 수행되었습니다. 본 논문의 발전을 위하여 사독을 해주신 박성준 박사님과 김창성 박사님께 깊이 감사드립니다.
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