• 한국해안해양공학회지
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• 제16권2호
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• pp.92-102
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• 2004

본 논문은 조류의 대ㆍ소조 변동이 존재하는 해역에서의 점열원에 대한 초과수온 분포를 예측하는 해석해를 다룬다. 해석해는 Jung et al.(2003)이 제시한 2차원 해석해를 기본으로 하여 조류의 대ㆍ소조 변동과 수평 확산계수의 대ㆍ소조 변화를 반영할 수 있는 형태로 확장되었다. 일련의 해석모형 실험을 통해 조류 및 난류확산의 변동에 따른 열오염의 이동ㆍ확산 변화를 검토하였다. 실험결과 열오염의 이동ㆍ확산은 tidal excursion 거리 이내에서는 조류의 크기에 좌우되며 tidal excursion 거리를 벗어난 해역에서는 주로 수평 확산에 의해 결정되는 것으로 나타났다. 특히 tidal excursion 거리 이내 해역에서 초과수온 분포는 수평 확산계수의 대ㆍ소조 변동에 큰 영향을 받는 것으로 나타났다. 즉, 1$^{\circ}C$이상의 비교적 높은 초과수온이 발생하는 범위는 수평 확산계수의 대ㆍ소조 변동을 고려하는 경우가 상대적으로 더 멀리 확장하는 경향을 보여주었다.

• Ocean and Polar Research
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• 제25권1호
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• pp.63-74
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• 2003

The build-up of the heat field in shallow coastal water due to a point source has been investigated using an analytical solution of a time-integral form derived by extending the solutions by Holley(1969) and also presented in Harleman (1971). The uniform water depth is assumed with non-isotropic turbulent dispersion. The alongshore-flow is assumed to be uni-directional, spatially uniform and oscillatory. Due to the presence of the oscillatory alongshore-flow, the heat build-up occurs in an oscillatory manner, and the excess temperature thereby fluctuates in that course and even in the quasi-steady state. A series of calculations reveal that proper choices of the decay coefficient as well as dispersion coefficients are critical to the reliable prediction of the excess temperature field. The dispersion coefficients determine the absolute values of the excess temperature and characterize the shoreline profile, particularly within the tidal excursion distance, while the decay coefficient determines the absolute value of the excess temperature and the convergence rate to that of the quasi-steady state. Within the e-folding time scale $1/k_d$ (where $k_d$ is the heat decay coefficient), heat build-up occurs more than 90% of the quasi-steady state values in a region within a tidal excursion distance (L), while occurs increasingly less the farther we go to the downstream direction (about 80% at 1.25L, and 70% at 1.5L). Calculations with onshore and offshore discharges indicate that thermal spreading in the direction of the shoreline is reduced as the shoreline constraint which controls the lateral mixing is reduced. The importance of collecting long-term records of in situ meteorological conditions and clarifying the definition of the heat loss coefficient is addressed. Interactive use of analytical and numerical modeling is recommended as a desirable way to obtain a reliable estimate of the far-field excess temperature along with extensive field measurements.