• Proceedings of the Korean Environmental Sciences Society Conference
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• 2008.11a
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• pp.149-151
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• 2008

• 한국지구과학회:학술대회논문집
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• 2006.02a
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• pp.140-142
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• 2006

• Proceedings of the Korea Air Pollution Research Association Conference
• /
• 2006.10a
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• pp.103-105
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• 2006

• Proceedings of the Korea Air Pollution Research Association Conference
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• 1991.05a
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• pp.53-57
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• 1991

• Proceedings of the Korean Environmental Sciences Society Conference
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• 2004.05a
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• pp.230-231
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• 2004

일출 후 태양복사에 의한 혼합층 발달과 새벽녘의 안정층 형성이 잘 관측되고 있다. 풍향의 경우, 해륙풍에 의한 풍향 일변화를 보이고 있으며, 이는 해안지역의 특징을 잘 반영하는 것이다. 간척지라는 지면특성을 고려하여 지속적인 관측과 분석이 이루어진다면, 지면성질에 따른 대기경계층 특성과 혼합층 고도를 추정할 수 있을 것으로 기대된다.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 1996.10a
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• pp.9-10
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• 1996

• Journal of the Korean Society of Fisheries and Ocean Technology
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• v.27 no.1
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• pp.41-55
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• 1991

A study was done to investigate characteristics of the land and sea breeze over Cheju island on the basis of surface meteorological data collected from 1977 to 1986. The results are summarized as follows: The frequency of the land and sea breze was highest in August followed by September, October, May and November in descending order. This indicates that the frequency of the land and sea breeze is higher in fall than in spring, and lowest in winter. The sea breeze began much earlier than any other regions of Korea all the year round, and it began about 30 minutes earlier and ended one hour later in the northern coast than in the southern coast of Cheju island. Meanwhile, the land breeze began about one hour earlier in the southern coast than in the northern coast and ended almost at the same time in both coasts. The annual mean duration of the sea breeze was about one hour longer in the northern coast than in the southern coast, but the land breeze showed an opposite trend. The duration of the sea breeze was longer in summer than in winter and again the land breeze was opposite. Transition period from the sea to the land breeze was relatively long in summer and shout in winter, but transition period from the land to the sea breeze was not different between seasons. The time for a maximum velocity of the sea breeze came earlier in the southern coast than in the northern coast, but that of the land breeze came almost at the same time in both coasts with no seasonal variations. Monthly mean maximum velocity of the sea breeze was greater than that of the land breeze.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 1999.10a
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• pp.420-421
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• 1999

여천지역은 화학물질 누출사고 등 안전 사고 발생의 잠재적 위험이 높으나 (김영성 등, 1999), 복잡한 해안선의 여수 반도 해안지역에 산을 등지고 있어 해륙풍에 의한 일 변화와 지형 조건에 따른 국지 변화등 복잡한 형태의 바람장이 예상되는 지역이다. 이러한 지역에서의 확산현상은 환경영향평가에서 흔히 이용되고 있는 균일한 바람장 분포를 가정한 대기화산 예측과는 다른 결과를 보이며 (오현선, 김영성, 1999), 따라서 단순한 가우시안 플룸 모델을 이용한 확산 예측은 적용범위가 매우 제한적일 수밖에 없다.(중략)

• Journal of Environmental Science International
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• v.11 no.9
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• pp.933-943
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• 2002

The urban pollution if affected by local environmental, so it is necessary to consider area characteristics such as emission source and meteorological phenomena, in studying urban air pollution. Ulsan is laocated on south-east coast and has many industrial facilities, so many people have concerned about air pollution. This study contain conducting numerical simulation of air pollutant concentration considered land and sea breeze in Ulsan area with the numerical model.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2000.11a
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• pp.183-184
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• 2000

종합적인 오존대책을 구축하기 위해서는 광화학 옥시단트의 생성물리ㆍ화학과정 및 생물기원(자연발생원) 탄화수소의 영향을 고려한 3차원 광화학반응 모델의 구축이 가장 절실하다. 특히, 광화학 옥시단트는 국지적인 순환(해륙풍)및 혼합층에 의해 지배되기 때문에 지형을 고려한 3차원 기상장 수치모델(도시규모)과 광화학을 포함한 농도장(광화학반응 모델) 모델에 의한 대상지역의 시간적, 공간적인 오존농도 분포를 재현할 수 있는 모델 개발이 필요하다. (중략)