• 대기
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• 제29권1호
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• pp.41-51
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• 2019

The characteristics of the sea breeze were investigated using the wind and temperature data collected from 300-m tower at Boseong from May 2014 to April 2018. Sea breeze day was detected using following criteria: 1) the presence of a clear change in wind direction near sunrise (between 1 hour after sunrise and 5 hours before sunset) and sunset (from 1500 LST to midnight), 2) presence of thermal forcing of sea breeze and 3) no heavy precipitation (rain < $10mm\;d^{-1}$). Sea breeze days occurred on 569 days for 4 years. The monthly distribution of sea breeze day occurrence shows maxima in May and September and minimum in December. The average onset and cessation times of the sea breeze are 0942 LST and 1802 LST, respectively. Although the 10-m wind shows clockwise rotation with time in the afternoon, the observed hodograph does not show an ideal elliptical shape and has different characteristics depending on the upper synoptic wind direction. Vertical structure of sea breeze shows local maximum of wind speed and local minimum of virtual potential temperature at 40 m in the afternoon for most synoptic conditions except for southeasterly synoptic wind ($60^{\circ}{\sim}150^{\circ}$) which is in the same direction as onshore flow. The local minimum of temperature is due to cold advection by sea breeze. During daytime, the intensity of inversion layer above 40 m is strongest in westerly synoptic wind ($240^{\circ}{\sim}330^{\circ}$) which is in the opposite direction to onshore flow.

• 한국환경과학회지
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• 제14권1호
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• pp.41-51
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• 2005

Using three-dimensional non-hydrostatical numerical model with one way double nesting technique, atmo­spheric circulation in the mountainous coastal region in summer was investigated from August 13 through 15, 1995. During the day, synoptic westerly wind blows over Mt. Mishrung in the west of a coastal city, Sokcho toward the East Sea, while simultaneously, easterly upslope wind combined with both valley wind from plain (coast) toward mountain and sea-breeze from sea toward inland coast blows toward the top of the mountain. Two different directional wind systems confront each other in the mid of eastern slope of the mountain and the upslope wind goes up to the height over 2 km, becoming an easterly return flow in the upper level over the sea and making sea-breeze front with two kinds of sea-breeze circulations of a small one in the coast and a large one in the open sea. Convective boundary layer is developed with a thickness of about 1km over the ground in the upwind side of the mountain in the west and a thickness of thermal internal boundary layer from the coast along the eastern slope of the mountain is only confined to less than 200 m. On the other hand, after sunset, no prohibition of upslope wind generated during the day and downward wind combined with mountain wind from mountain towardplain and land-breeze from land toward under nocturnal radiative cooling of the ground surfaces should intensify westerly downslope wind, resulting in the formation of wind storm. As the wind storm moving down along the eastern slop causes the development of internal gravity waves with hydraulic jump motion in the coast, bounding up toward the upper level of the coastal sea, atmospheric circulation with both onshore and offshore winds like sea-breeze circulation forms in the coastal sea within 70 km until midnight and after that, westerly wind prevails in the coast and open seas.

• 한국환경과학회:학술대회논문집
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• 한국환경과학회 2003년도 International Symposium on Clean Environment
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• pp.177-184
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• 2003

Numerical simulation on marine wind and sea surface elevation was carried out using both three-dimensional hydrostatic and non-hydrostatic models and a simple oceanic model from 0900 LST, August 13 to 0900 LST, August 15, 1995. As daytime easterly meso-scale sea-breeze from the eastern sea penetrates Kangnung city in the center part as basin and goes up along the slope of Mt. Taegullyang in the west, it confronts synoptic-scale westerly wind blowing over the top of the mountain at the mid of the eastern slope and then the resultant wind produces an upper level westerly return flow toward the East Sea. In a narrow band of weak surface wind within 10km of the coastal sea, wind stress is generally small, less than l${\times}$10E-2 Pa and it reaches 2 ${\times}$ 10E-2 Pa to the 35 km. Positive wind stress curl of 15 $\times$ 10E-5Pa $m^{-1}$ still exists in the same band and corresponds to the ascent of 70 em from the sea level. This is due to the generation of northerly wind driven current with a speed of 11 m $S^{-1}$ along the coast under the influence of south-easterly wind and makes an intrusion of warm waters from the southern sea into the northern coast, such as the East Korea Warm Current. On the other hand, even if nighttime downslope windstorm of 14m/s associated with both mountain wind and land-breeze produces the development of internal gravity waves with a hydraulic jump motion of air near the coastal inland surface, the surface wind in the coastal sea is relatively moderate south-westerly wind, resulting in moderate wind stress. Negative wind stress curl in the coast causes the subsidence of the sea surface of 15 em along the coast and south-westerly coastal surface wind drives alongshore south-easterly wind driven current, opposite to the daytime one. Then, it causes the intrusion of cold waters like the North Korea Cold Current in the northern coastal sea into the narrow band of the southern coastal sea. However, the band of positive wind stress curl at the distance of 30km away from the coast toward further offshore area can also cause the uprising of sea waters and the intrusion of warm waters from the southern sea toward the northern sea (northerly wind driven current), resulting in a counter-clockwise wind driven current. These clockwise and counter-clockwise currents much induce the formation of low clouds containing fog and drizzle in the coastal region.

• 한국해양학회지:바다
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• 제9권3호
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• pp.137-152
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• 2004

한반도 남서해안에서 연안지대의 기후학적 특성을 조사하기 위해 AWS(automatic weather system)와 4개 지점의 부이자료를 사용하였다. 연안지대를 기후학적으로 정의하였는데 해안선을 가로지르는 풍속과 온도의 기울기에 있어서 뚜렷이 대비가 나타나는 지대로 정의하였고, 연안지대가 고정적인 것이 아니라 종관풍에 따라 변동될 수 있다는 것을 보였다. 한반도의 남해와 서해에서 부이와 나란한 AWS지점으로 구성된 4개의 단면도선을 거제도부이라인, 거문도부이라인, 칠발도부이라인, 덕적도부이라인으로 선택하였다. 일주기와 월변동의 분석에서 월별평균과 극값, 부이와 각 지점간의 온도경도와 풍속의 누적빈도수가 연안의 범위와 특징을 조사하는데 응용되었다. 그 결과 연안지대의 최대범위는 거제도부이라인은 offshore에서 생림(해안선에서 약 34 km), 거문도부이라인은 순천(약 52 km), 칠발도부이라인은 자은도(약 27 km), 덕적도부이라인은 용인(약 65 km)으로 분석되었다. 종관풍에 따른 연안지대의 변동을 onshore, offshore, calm에 대해 조사하였다. 그 결과 onshore 일 때 연안지대의 범위는 65∼90 km로 변화한다. 더욱 우리는 태풍(MAEMI)에 의해 영향을 받은 2003년 9월 12일∼13일 동안에 거제도부이라인에 대한 풍속과 온도의 변화와 해상과 육상의 풍속비를 알기 위해 조사하였다.

• 해양환경안전학회지
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• 제27권6호
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• pp.721-730
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• 2021

본 연구에서는 국내 서로 다른 지리적 특성을 갖는 지역에서 발생되는 해륙풍에 의한 항만 내 선박 대기오염물질의 항구도시 확산 범위를 규명하고자 하였다. 연구 대상 지역은 서해안(인천항 및 평택·당진항), 다도해 지역(목포항), 남해 및 동해(부산항 및 마산항), 동해 산간 지역(동해·묵호항)으로 선정하였다. 해륙풍 발생과 그로 인한 항만 내 선박에서 기인하는 대기오염물질의 확산 모사를 위하여 비선형(Non-linear) 및 비정상(Unsteady) 거동의 국지 순환풍 모사가 가능한 HOTMAC-RAPTAD 프로그램을 활용하였으며, 모사 기간은 전형적인 여름 날씨인 7월 중순으로 하였다. 그 결과, 해륙풍의 발생 특성과 항만에서 발생되는 대기오염물질의 주변 지역 확산 거동이 지역마다 서로 다르게 나타났는데 연구 대상 항만인 인천항, 목포항, 부산항, 동해·묵호항에서 배출되는 대기오염물질은 항구로부터 각각 27~31km(서울 서쪽 일부 지역), 21~24km(무안 남부), 20~26km(김해 및 양산 인근), 22~25km(태백산맥 능선 지역)까지 영향을 끼치는 것으로 분석되었다. 따라서 본 연구에서 도출된 결과는 향후 효과적인 항만 지역 대기질과 선박 대기오염물질 관리에 있어 매우 중요한 기초 수단으로 활용 가능할 것으로 기대된다.