• Proceedings of the KSRS Conference
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• 2001.03a
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• pp.91-91
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• 2001

현재 진행되고 있다고 여겨지는 지구변화 (Global Change)의 연구는 환경/지구과학의 초미의 관심사로 떠오르고 있다. 특히 온실가스의 분출로 인한 지구 온난화 (Global Warming)는 지구환경에 부정적인 효과가 초래될 것으로 우려되는바, 여러 지구환경 인자들의 변화를 초래할 것으로 예측되고 있다. 가장 직접적인 인자는 대기온도이고 아울러 해수온도/해류, 바람속도/방향, 대기화학 조성, 식생분포, 구름량, 얼음분포 등이 간접적인 인자들이다. 본 연구에서는 EOS 위성군 중 고층대기 연구를 위한 UARS 위성의 HRDI 센서의 자료를 분석하였다. HRDI는 대기성분 중 산소 $O_2$ 발광선의 도플러 변이를 측정하여 바람속도를 측정한다. 이 자료의 분석을 통하여 50~100 km 상공의 바람속도 변화를 지상에서의 OH 발광선 관측치와 비교하였다. 본 연구는 초기 연구로서 정략적이고 보편적인 결과 도출보다는 향후 연구를 위한 기반연구로서의 성격을 갖는다. 지구온난화는 대기의 온도를 상승시키고, 이는 대기 중 에너지의 증가를 불러와 필연적으로 고층대기의 교란 현상이 있을 것으로 예상된다. 앞으로 지구전체 대기의 풍속/풍향의 고도변화가 분석되면 지구온난화에 의한 고층대기 변화가 탐지될 것으로 기대된다.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.28 no.3
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• pp.95-120
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• 2023

Methane (CH₄) is a key greenhouse gas in the atmosphere with 85 times greater greenhouse potent relative to carbon dioxide (CO₂). The atmospheric concentration of CH₄ is rapidly increasing due to the intensive usage of CH₄ and the thawing of the cryosphere. Additionally, with the current warming of ocean water, the dissociation of gas hydrates, an ice-like compound and the largest reservoir of CH₄ on Earth, is expected to occur, resulting in the release of CH₄ from the seafloor into the overlying water and atmosphere. Moreover, bottom water hypoxia is another concern that potentially introduces greenhouse gases into the atmosphere. With ongoing global warming and eutrophication, the size and duration of bottom water hypoxia are rapidly increasing. These low-oxygen conditions would relocate the redox zone shallower in sediment or in the water column, causing the release of CH₄ into the atmosphere and thereby intensifying global warming. However, there exists a gap in the understanding of CH₄ dynamics including its generation in relation to bottom water hypoxia. Therefore, this review article aims to understand the relationship between CH₄ and bottom water hypoxia and to draw attention to CH₄ investigation in Korea.

• Journal of Aquaculture
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• v.8 no.4
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• pp.251-260
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• 1995

Experimental transportations of the olive flounder (Paralichthys olivaceus) seedlings (body weight $2.1\pm0.39g$) with polyethylene vinyl bag were Performed to study the change of dissolved oxygen (DO) during transportation, survival rate and feeding activity of seedlings after transportation. The distance and time required for the transportations were 272 km and 11 hours, respectively. DO was rapidly decreased within 3 hours (P<0.05) during the transportation of seedlings of 40 fish in 10l of sea water at $15.6\~17.8^{\circ}C$ of initial water temperature with 5 ml/l of initial DO. The decreasing tendency of DO (Y) according to elapsed time (X) was expressed an equation of $Y\;=\;2.7444X^{-0.4780}$ (r=0.8071). Feeding activity of the seedlings after transportation supplemented with oxygen and icepack besides above transport conditions was significantly higher than that of fish supplemented with icepack only (P<0.05). It was desirable to starve the seedlings for 36 hours before transportation. Survival rate of seedlings was greatly reduced, when the dissolved oxygen concentration was lowered below the range of $0.7\~0.94ml/l$ just after transportation.

• Journal of the Korean Data Analysis Society
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• v.20 no.6
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• pp.2941-2951
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• 2018

The purpose of this paper is to analyse the effect of ocean weather factors on shipments of swimming crab. We use the data of data portal and ocean weather factors (mean wind velocity, mean atmospheric pressure, mean relative humidity, mean air temperature, mean water temperature, mean maximum wave height, mean significant wave height, maximum significant wave height, maximum wave height, mean wave period, maximum wave period). We did statistical analysis using Poisson regression analysis and negative binomial regression analysis. As the result of study, important factors influential in the shipments of swimming crab turn out to be mean wind velocity, mean atmospheric pressure, mean relative humidity, mean water temperature, maximum wave height, mean wave period and maximum wave period. the shipments of swimming crab increases as mean wind velocity, mean atmospheric pressure, mean relative humidity, mean water temperature increases or mean wave period increase. However, as maximum wave height, maximum wave period decreases, the shipment of swimming crab increases.