• Proceedings of the Korean Society of Fisheries Technology Conference
• /
• 2002.05a
• /
• pp.471-471
• /
• 2002

• 한국석유지질학회:학술대회논문집
• /
• spring
• /
• pp.1-111
• /
• 1998

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
• /
• v.7 no.3
• /
• pp.218-220
• /
• 2002

현재 국립수산과학원에서 실시하고 있는 해양조사는 크게 연안 정지 해양관측, 정선 해양관측, 해양오염측정망관측, 적조예찰 및 조사 등이 있다. 수집된 조사자료는 국립수산과학원 홈페이지(http://www.nfrdi.re.kr/)에 제공하고 있다.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
• /
• v.7 no.3
• /
• pp.207-210
• /
• 2002

국립해양조사원은 우리나라 전 해역을 대상으로 해양교통안전, 해양자원 개발, 군 작전 지원, 해양수산 발전에 필요한 정보를 제공하고자 조석, 조류, 해류관측에 의해 수집된 각종 해양자료를 처리·분석하고 DB화하고 있다.

• 한국석유지질학회:학술대회논문집
• /
• spring
• /
• pp.47-56
• /
• 1997

• Proceedings of the KSRS Conference
• /
• 2003.11a
• /
• pp.662-662
• /
• 2003

• Proceedings of the Zoological Society Korea Conference
• /
• 1999.10b
• /
• pp.88.2-88
• /
• 1999

No Abstract, See Full Text

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
• /
• v.11 no.4
• /
• pp.172-178
• /
• 2006

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
• /
• v.13 no.3
• /
• pp.165-167
• /
• 2008

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
• /
• v.8 no.3
• /
• pp.295-306
• /
• 2003

Recently efforts are underway to analyze the impacts of anthropogenic $CO_2$ on the global environments and the amount of oceanic uptake increase. The East Sea is now viewed as a miniature ocean because its circulation pattern is similar to the ocean conveyer belt. The biological pump of the East Sea is a vital component to understand the carbon cycle quantitatively. In this paper, the biological pump is estimated utilizing the stoichiometric ratio between carbon and phosphorus. A simple phosphate budget model is constructed based on the seawater and dissolved oxygen box model that can simulate the recent structural change in deep water circulation of the East Sea. A model run from you 1952 to 2040 shows the steadily intensifying biological pump. Currently it exports about 0.016 Pg C yr$^{-1}$ , which corresponds to 35％ of the carbon introduced into the seawater by the air-sea exchange. An increased oxygen supply to the central water mass as a result of from the transition in the ventilation system might enhance the remineralization of sinking biogenic particles. This should strengthen the upward nutrient flux into the surface layer. Consequently, the biological sequestration of anthropogenic carbon is expected to increase with time. The estimated biological uptake of the anthropogenic carbon in the East Sea since the Industrial Revolution is estimated as 0.025 Pg C.