• Journal of Environmental Science International
• /
• v.5 no.4
• /
• pp.441-451
• /
• 1996

The surface meteorological and upper layer meteorological observation carried out to investigate influences of sea breeze effect on lower layer atmosphere at Gori nuclear power plant for 29∼30 July, 1996. According to surface meteorological data, the inflow of sea breeze was occurred 11:30 on 29 July, 10:30-on 30 July, respectively, at observation site. And the meteorological tower data showed that wind direction of sea breeze was identified as south-westerly, and wind speed of 58 m was 2 times stronger than that of 10 m. It is notworthy that surface inversion layer which built from the night time to daybreak of next day was not broken off by seab reeze's inflow for daytime, and strong inversion layer observed at 47∼243 m with moderately stable class (F) by URC. It was found that strong stable layer of potential temperature appeared at that layer, maximum relative humidity observed at the bottom of inversion layer and maximum mixing ratio observed in the low of inversion layer.

• Landscaping Tree
• /
• s.84
• /
• pp.16-18
• /
• 2005

전국 어디서나 쉽게 볼 수 있는 사철나무는 노박덩굴과 식물로 해풍과 염기에 강하며 해수와 접하여도 잘 죽지 않고, 또한 내음력이 강하며, 습지와 건조지에서도 강하며 맹아력이 좋고 공해에도 강하여 정원수나 조경수로는 적격인 수종이라 할 수 있겠다. 이러한 까닭에 도심지의 조경수, 관상수, 정원수로 많이 식재되고 있고 잘 정돈된 사철나무 울타리는 도시인의 마음을 한결 깔끔하게 하고 화려하지는 않지만 은은하여 도시에서 느낄 수 없는 소박한 시골 아낙네 같은 청초한 느낌을 준다. 봄과 여름에는 다른 수종들과 어울러져 남들을 더욱 돋보이게 하고 가을과 겨울에는 혼자만이 꿋꿋이 녹색을 띠면서 적막한 도시의 거리를 조금이나마 부드럽게 하는 현대인이 배우고 갖추어야 할 덕목을 일러주는 나무인 것이다. 이러한 사철나무를 가해하는 해충으로 깍지벌레류와 진딧물류의 피해가 심하고, 기타 잎을 가해하는 왕물결나방, 차주머니나방이 피해를 주고 있어 이들에 대한 생태 및 방제법을 간략하게 소개하고자 한다.

• Proceedings of the Korean Environmental Sciences Society Conference
• /
• 2007.05a
• /
• pp.149-156
• /
• 2007

부산의 대표적 큰 계곡인 성지곡수원지는 남쪽으로 부산의 최대 도심인 서면을 향해 열려 있고, 그 이외의 삼면은 높은 산지로 둘러싸여 있다. 그래서 성지곡-서면-남항 일대는 낮에는 해풍이 곡풍(남풍)의 형태로 불고, 야간에는 산풍이 육풍(북풍)의 형태로 불고 있다. 이렇게 형성된 국지풍 순환의 규모와 특성을 평가하기 위하여, 계곡 입구와 도심인 서면 부근에 자동기상관측장치를 설치하여 특별 관측을 수행하였다. 관측결과 주간에는 서면 부근의 기온이 성지곡 입구보다 낮았고, 야간에는 이와 반대로 나타났으며 그 차이는 대체로 $3^{\circ}C$ 내외였다. 이것은 주로 지표면 가열의 의한 기단변질의 결과로 판단된다. 관측 일에 확인된 도로표면온도는 낮에 약 65도까지 상승하였으며 야간에도 30도 정도의 고온이 유지되었다. 이 연구에서는 현장관측으로 확인된 기단변질과정을 이해하기 위하여 2차원 대류모델을 이용한 수치실험을 수행하였다. 수치실험의 결과 낮에는 지표로부터 약 $150W/m^2$이상의 현열이 보급됨이 확인되었다. 야간에도 $10W/m^2$ 내외의 현열이 대기 중으로 보급되어 성지곡 수원지에서 발원된 냉기류를 가열시키고 있음이 확인되었다.

• Proceedings of the KIEE Conference
• /
• 1990.07a
• /
• pp.529-531
• /
• 1990

Because Filters do both the sampling or Sampled-and-Hold(S/H) operations, it result in the replication of the spectrum of input signal and (unless Nyquist's criterion is satisfied) induce aliasing distortion. In this paper, therefore, we designed AAF(Analog Anti-aliasing Filers) so as to remove high-frequency components from input signal for aliasing distortion prevention before input signal had been processed frequency seletion by filters. and then, researched characteristics of it.

• Journal of Environmental Science International
• /
• v.11 no.4
• /
• pp.289-295
• /
• 2002

We would like to investigate the strong wind phenomenon effecting to the onset of a sea breeze. It is general the fact that the onset time of a sea breeze is mainly affected according to the distance from the coastline but we find the reversal fact. The onset time at Suyoung is faster than that at Haeundae in spite of the observation site of Suyoung is 5 m and that of Haeundae is 1 km away from the coastline. This is the reason that the nighttime air is converged the lower area by surface cooling and then it is strongly drained onto the lowest area, Suyoung river until the sunrise. it is proved by observation data at Suyoung and Haeundae.

• Proceedings of the Korean Society of Coastal and Ocean Engineers Conference
• /
• 1993.07a
• /
• pp.175-177
• /
• 1993

열대성 저기압에 의해 발생되는 태풍 또는 폭풍은 주변해역에 평균수위상승(setup)을 유발하며 진행하게 된다. 우리나라에는 주로 하절기에 남해평양에서 발생한 해풍의 영향을 받아 해일 등의 피해를 입게 되는데, 이러한 해일은 여러가지 수위상승효과가 복합된 결과이다. 즉, 폭풍 도착전 발생하는 초기수위상승(initial setup), 저기압 중심 주변의 급격한 압력경사에 의한 수위상승(pressure setup), 폭풍의 진행속도가 발생된 파의 속도에 근접할 경우 압력차에 의한 수위상승이 더욱 증폭되는 장파수위상승(long wave setup), 바람과 바닥 마찰에 의한 수위상승(wind and bottom stress setup), Coriolis힘에 의한 수면상승(Coriolis setup) 등 여러 가지 효과에 의해 해일이 발생하게 된다. (중략)

• Journal of the Korean Society of Marine Environment & Safety
• /
• v.22 no.2
• /
• pp.195-204
• /
• 2016

In this paper, the applicability and usefulness of windprofiler input data were investigated to generate three dimensional wind field. A logical diagnostic model CALMET with windprofiler data at ten sites and with weather forecasting model WRF output was evaluated by statistically comparing with the radiosonde data at eight sites. The horizontal wind speed from CALMET simulated with hourly windprofiler data is in good agreement with radiosonde observations within 1.5 m/s of the root mean square error, especially local circulation of wind such as sea breeze over the coastal region. The root mean square error of wind direction ranged $50^{\circ}{\sim}70^{\circ}$ is due to the wind direction error from the windprofiler polluted by ground clutters. Since the exact wind can be produced quickly and accurately in most of the altitude with windprofiler data on CALMET, we expect the method presented in this study to be useful for the monitoring of safe environment as well as weather in the coastal zone.

• International Union of Geodesy and Geophysics Korean Journal of Geophysical Research
• /
• v.23 no.1
• /
• pp.18-33
• /
• 1995

Under the synoptic scale strong westerly winds flowing over the large steep mountains in the eastern coastal region, the strong downslope wind storms such as internal gravity waves should be generated in the lee-side of mountain. Int he daytime as sea breeze circulation induced by meso-scale thermal forcing from sea toward inland confines to the offshore side of coastal sites due to the eastward internal gravity waves. Thus, surface winds near the coastal seas were relatively weaker than those in the open sea or the inland sites. Evidently, two different kinds of atmospheric circulations such as an internal gravity wave circulation with westerly wind and a sea breeze circulation with both easterly wind near the sea surface and westerly in the upper level were apparently produced. Under this situation the atmospheric pollutants at Kangnung city should be trapped by two different circulations in the opposite directions and resulted in the high concentrations of Total Suspended Particles (TSP) and ozone (O3). At night a meso-scale land breeze from land toward the more intensification of westerly winds in the coastal regions. The concentrations of TSP controled by the strong surface winds blowing from the mountain side toward the coastal sea were relatively higher at night than those in the daytime case and the concentrations of O3 due to the downward transport of ozone from the upper atmosphere toward the surface were also much higher at night than during the day. Consequently, the atmospheric pollutant concentrations in the mountainous coastal region under the downslope wind storms were higher than those after and before the occurrences of wind storms.

• Korean Journal of Agricultural and Forest Meteorology
• /
• v.15 no.4
• /
• pp.210-218
• /
• 2013

The sea breeze shows different characteristics compared to land breeze, such as high wind speed and more rapider shift period. One of the major factors affecting plant early growth is wind speed. In the early growth stage, tree growth-rates rise with decreasing wind speed. Thus, the study was performed to identify wind break effects on wind characteristics and tree growth. The wind break used in this study was about 130 meters length and 3 meters height, made up with poly-ethylene (with 40% openness). We installed one vane and fifteen anemographs at three different heights (1, 2 and 3 meters) on the inner and outer wind break areas. The wind characteristic and plant growth data were collected from Jun. 2011 to Oct. over 2012. The wind rose of the Saemangum seawall area presented the north (21.5%) and it was followed by north-west (18.1%), east (14.9%) and north-east (13.7%) and the remainder with other directions. Wind speeds at height were different. The tree height was 159.6 cm at inside and 129.6 cm at outside. The diameter at root-collar was 36.9 mm at inside and 32.6 mm at outside from wind break.

• Journal of Environmental Science International
• /
• v.23 no.2
• /
• pp.261-274
• /
• 2014

This work investigates the relationship between the sea breeze circulation and ozone concentrations during cold water events in the southeastern coastal area of the Korean Peninsula, where coastal upwelling frequently occur. This analysis was performed based on the classification of two categories, such as cold water and non-cold water events, over the period of 2000-2009. The low air temperature ($0.5^{\circ}C$), low SST ($5^{\circ}C$) and the wind direction(southerly) are the features of the cold water events in the Southeastern coastal area. Moreover, ozone concentrations in the cases of the sea breeze circulation and cold water events were significantly lower (below 30 ppb) than those (70~100 ppb) in the non-clod water events, because of the low air temperature ($10{\sim}20^{\circ}C$) and high wind speed (3~5 m/s) around the southeastern coastal area.