• 한국환경과학회지
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• 제23권5호
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• pp.801-806
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• 2014

Long-term change in sea level along the eastern coast of Korea was illustrated using four tide-gauge station (Pohang, Mukho, Sokcho, Ulleung) data, water temperature and salinity. Seasonal variation in the sea level change was dominant. The sea level change by steric height derived from water temperature and salinity was relatively lower than that measured from the tide-gauge stations. Sea level rising rate per year by steric height increased with latitude. The effect of salinity(water temperature) on the sea level change is greater in winter(in summer).

• 한국토양비료학회지
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• 제47권5호
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• pp.313-318
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• 2014

The remote monitoring system of water salinity was assessed in Wando reclaimed land lake during a farming season in 2009. Increasing of water salinity in this lake used to bring about salt damage on rice plant occasionally. At the early stage of the rice growing period, rice growth was not damaged due to enough rainfall with more than 120 mm from the mid-May to the first ten days of June. Data collection using on-site water salinity measuring sensors every 2 hours and real-time transmission in system were carried out for the experiment. We compared the transmitted values from the sensor system with water sample values collected and analyzed by a local technical office. Salt concentrations measured by sensor in real-time monitoring system were available data. The regression equation between rainfall and water salinity was presented as (water salinity after rainfall) = $0.621{\times}$(water salinity before rainfall)${\times}exp(-0.0139{\times}rainfall)$, ($r^2=0.579$, p<0.01). It is suggested that the system is useful for stable farming in the area where farmer use water in reclaimed lakes as an irrigation source.

• Ocean and Polar Research
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• 제33권spc3호
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• pp.371-383
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• 2011

To investigate the physical characteristics and variations of oceanic parameters in the tropical central North Pacific, oceanographic surveys were carried out in summer of 2006 and 2007. The survey periods were classified by Oceanic Ni$\tilde{n}$o Index as a weak El Ni$\tilde{n}$o in 2006 and a medium La Ni$\tilde{n}$a in 2007. The survey instruments were used to acquire data on CTD (Conductivity Temperature and Depth), XBT (Expendable Bathythermograph), and TSG (Thermosalinograph). The dominant temporal variation of surface temperature was diurnal. The diurnal variation in 2007, when the La Ni$\tilde{n}$a weather pattern was in place, was stronger than that in 2006. Surface salinity in 2006 was affected by a northwestward branch of North Equatorial Current, which implies that the El Ni$\tilde{n}$o affects surface properties in the North Equatorial Current region. Two salinity minimum layers existed at stations east of Chuuk in both year's observations. The climatological vertical salinity section along $180^{\circ}E$ shows that the two salinity minimum layers exist in $2^{\circ}N{\sim}12^{\circ}N$ region, consistent with our observations. Analysis of isopycnal lines over the salinity section implies that the upper salinity minimum layer is from intrusion of the upper part of North Pacific Intermediate Water into the lower part of South Pacific Subtropical Surface Water and the lower salinity minimum layer is from Antarctic Intermediate Water.

• 한국양식학회지
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• 제16권1호
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• pp.31-36
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• 2003

사육 염분의 급성교환 실험에서, 해수의 담수화가 1시간 이내에 이루어졌을 경우 농어, 유어들은 다소의 스트레스 반응과 이온의 변화가 있었으며. 24시간 뒤에도 정상 회복이 더딘 것으로 나타났다. 그러나 5시간에 걸친 담수화 과정 중에 스트레스 반응은 담수화 직후 높게 나타났지만, 24시간 후 빠르게 정상으로 회복되는 것을 알 수 있다. 장기간 염분별 사육실험 결과, 20 ppt가 가장 높은 사료섭식량을 나타내었고, 2 ppt구가 가장 낮았다. 사료효율 또한 2 ppt구이 가장 낮게 나타났고, 10 ppt구가 가장 높았으며, 실험구별 유어의 성장은 실험 종료시 10, 20 및 30 ppt구가 2 ppt보다 유의하게 높은 길이 성장을 보였다. 무게 성장은 실험 종료시 20 ppt가 가장 빠른 무게 성장을 나타내었고, 다음으로 30 ppt, 10 ppt. 2 ppt순으로 나타났다. 염분별 사육유어의 혈액 성상은 2 ppt~30 ppt 사육수에 있어 농어 유어들의 혈액 조성은 큰 차이가 없는 것으로 나타났다.

• 한국어류학회지
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• 제17권1호
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• pp.43-48
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• 2005

단계적인 방법에 의해 해수에서 담수로의 염분 하강과 담수에서 해수로의 염분 상승에 대한 잡종 striped bass (Morone chrysops ♀ ${\times}$ M. saxatilis ♂)의 생리적 반응을 조사하였다. 단계적인 염분 변화는 혈중 cortisol 농도의 상승을 동반하지 않았으나, 혈중 glucose 농도는 상승하였다. 혈장의 삼투질 농도와 $Na^+$, $Cl^-$ 농도는 염분상승과 함께 유의하게 증가하였으나, 염분 하강 때는 차이를 보이지 않았다. 이상의 실험 결과들은 잡종 striped bass는 단계적인 염분변화에 매우 효과적으로 적응하고 있음을 보여주고 있으며, 염분 스트레스에 강한 광염성 어종임을 입증하였다.

• Journal of the korean society of oceanography
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• 제37권3호
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• pp.117-124
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• 2002

Anthropogenic changes have been made to the water budget for the Mediterranean Sea as a result of river diversion projects. The decrease in freshwater inflow to the Mediterranean represents an effective increase in the overall net evaporation over the basin. Hydraulic control models for the exchange between the Mediterranean and Atlantic through the Strait of Gibraltar predict that the salinity of the Mediterranean should increase if the net evaporation over the Mediterranean increases. Increases in the salinity of the deep waters in both the western and eastern Mediterranean basins have been observed. The causes of such higher deep water salinity are attributed to increases in intermediate water salinity which are ultimately mixed down into the deep sea during wintertime buoyancy loss events. The pattern of the Mediterranean salinity increase is instructive for understanding how the water mass properties in a basin change over time as a result of anthropogenic changes.

• 한국양식학회지
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• 제18권1호
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• pp.45-51
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• 2005

황복 치어를 대상으로 염분과 수온이 변화되었을 때 나타나는 생리적 변화를 대사지표인 산소 소비율과 암모니아 질소 배설률을 측정하여 그 영향정도를 알아보고자 하였다. 염분 2, 12, 22 및 32 psu에서 2 개월간 순치 사육한 황복(체장 9.5$\pm$0.9 cm, 체중 18.7$\pm$5.4g)의 산소소비율과 암모니아 질소 배설률은 사육염분에 대하여 포물선식으로 나타낼 수 있어서 각각 $Y=-0.0873X^2+0.6384X-0.690$ 와 $Y=-2.1667X^2+7.1672X+31.999$로 표시할 수 있었다. 산소소비율과 질소배설률은 사료섭취과 관련하여 일주기성을 나타내어 산소소비는 사료섭취 3시간 후에, 암모니아 질소 배설은 사료섭취 4시간 후에 각각 높은 값을 나타내었다. 염분 2, 12, 22 및 32 psu에서 사육하던 황복을 갑자기 염분을 달리하였을 때 산소소비율과 암모니아 질소 배설률은 저염분(2. 12 psu)으로 옮긴 경우가 정상염분(32 psu)으로 옮긴 경우 보다 각 염분별 사육군간에 유의적인 차이를 보였다. 염분변화에 대한 생리적 보상으로 에너지 소비 경향을 산소소비량 대 암모니아 질소 배설량간의 원자비(O:N비)로 대사 기질을 판단할 때 많은 에너지를 소비하지 않는 것으로 나타났다. 사료효율 및 성장으로 본 황복에 적정 염분은 22 psu로 나타났다.

• 수산해양교육연구
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• 제28권4호
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• pp.1068-1075
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• 2016

The suitable temperature and salinity for the long-distance transportation for the rockfish were investigated by assessing survival rate, metabolism, histological change. All experimental groups showed survival rates of 100%. Daily Oxygen consumption rhythm was decreased during nights and increased during days. Average oxygen consumption was significantly decreased as temperature and salinity were decreased. Ammonia excretion was significantly increased as temperature and salinity were decreased. Histological changes were observed in the skin and gill of the rockfish exposed to 10 psu under all the temperature conditions, with larger changes at $4^{\circ}C$. Further, nucleus deformation and uniformity in the cytoplasm were also observed.

• 한국해양학회지
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• 제7권1호
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• pp.15-18
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• 1972

1968년 8월부터 1969년 7월까지 1년간 대한해협에서 수온 염분의 시간적 변동에 대해 조사한 결과를 요약하면 다음과 같다. 1. 수온 염분의 시간적 변동범위는 년중 8월이 가장 크고 4월이 가장 작았다. 2. 8월의 수온은 125m 층에서 5.67-15.75$^{\circ}C$로 10.08$^{\circ}C$의 최고 변동범위를 보였으며, 염분은 20m 층에서 32.09-34.32 로 2.23 의 최고 변동범위를 보였다. 3. 이렇게 수온, 염분의 시간적 변동범위가 계절에 따라 수층에 따라 큰 차이를 보이는 것은 대한해협에는 수평, 수직적으로 이질적인 다양한 수괴들이 있어 이들이 게절에 따라 분포구조가 변화할 뿐 아니라, 이곳을 통과하는 대마난류가 조석의 영향으로 시시각각 그 유향과 유속이 변동됨에 따라 이들 수괴들이 상호 수직, 수평으로 유동하기 때문인 것으로 보인다.

• 수산경영론집
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• 제46권3호
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• pp.63-72
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• 2015

This study aims to empirically analyze the relationship between climate change elements and catch amount of coastal fisheries, which is predicted to be vulnerable to climate change since its business scale is too small and fishing ground is limited. Using panel data from 1974 to 2013 by region, we tested the relationship between the sea temperature, salinity and the coastal fisheries production. A spatial panel model was applied in order to reflect the spatial dependence of the ocean. The results indicated that while the upper(0-20m) sea temperature and salinity have no significant influence on the coastal fisheries production, the lower(30-50m) sea temperature has significant positive effects on it and, by extension, on the neighboring areas's production. Therefore, with sea temperature forecast data derived from climate change scenarios, it is expected that these results can be used to assess the future vulnerability to the climate change.