• 한국항행학회논문지
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• 제1권1호
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• pp.81-94
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• 1997

우리나라의 급증하는 항공수요 처리와 동북아 지역 허브 공항 역할을 하기 위한 목적으로 인천국제공항이 건설되고 있다. 그러나 동북아지역 각국에서는 대규모 공항건설 및 수용능력 확장 사업이 추진되고 있어 인천국제공항이 성공적인 허브 공항으로 자리매김하기는 쉬운 일이 아니다. 특히 일본은 우리나라에 비해 월등히 많은 항공수요량을 바탕으로 신동경국제공항(나리타 공항)에 이어 오오사카 간사이 공항을 새로운 허브 공항으로 발전시키기 위한 계획을 추진하고 있다. 따라서 인천국제공항은 일본의 공항들과 동북아지역 허브 공항 경쟁을 하여야 한다. 공항의 허브 기능은 배후지형(hinterland) 허브 기능과 모래시계형(hourglass) 허브 기능이 있다. 성공적인 배후지형 허브 공항이 되기 위해서는 근거리 국내, 국제노선에 대한 풍부한 비행편이 존재해야만 한다. 인천국제공항운영자는 동 공항과 중국, 일본, 근거리 동남아 지역 주요 도시간의 비형편이 일본의 경쟁 공항을 이용하는 것보다 유리하도록 해야 할 것이다. 모래시계형 허브 기능으로서는 지리적 위치상 원거리 동남아 지역과 미주지역을 연결시켜주는 징검다리로서의 역할이 가능하다. 여기서도 경쟁 공항과 비행편 스케쥴링 전략에서 이겨야 하는데, 공항당국과 국적 항공사의 긴밀한 협조에 의한 수요개발과 외국(미국, 동남아) 항공사들과 국적항공사(대한항공, 아시아나 항공)간의 운항 제휴 등이 효과적 스케쥴링으로 결과될 수 있을 것이다. 정부의 항공당국도 외국과의 항공협정이나 국가 항공정책 수립시 일본의 정책을 고려하고 공항 당국 및 국척항공사의 의견을 수렴하여 인천국제공항이 동북아 허브 공항으로서 성공할 수 있도록 해야할 것이다.

• 한국지구과학회지
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• 제25권6호
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• pp.418-427
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• 2004

최근 도시기후를 고려한 도시계획이 많은 나라에서 실용화되고 있다. 도시기후의 고려는 주로 도시의 바람 길 조성이라는 개념으로 구체화되고 있다. 도시의 바람 길 조성은 주로 하계에 도시지역의 열적 쾌적성을 개선하는 것을 목표로 한다. 아울러, 과학적 조사에 근거하여 도시의 단지계획을 합리적으로 함으로써 청정한 냉기류의 도심유입을 원활히 하여 도심의 대기오염을 저감하고자 하는 것도 목적으로 한다. 이 연구에서는, 수치실험을 통하여 전형적인 난후기일을 대상으로 대구지역의 국지순환풍이 지나는 바람의 길을 조사하였다. 그리고 이 바람에 의한 대기오염의 수송도 조사하였다. 수치실험에 사용한 모형은 RAMS(지역규모 대기모델)이다. 수치실험의 관심지역은 대구광역시 일대(약900$km^2$)이다. 수평규모는 약 30km이다. 수치실험은 일반풍이 약하고 쾌청한 일기조건을 갖는 늦봄의 기상조건 하에서 수행되었다. 수치실험의 결과 다음과 같은 3가지 결과를 얻었다: (1) 대구의 대표적 산지인 팔공산과 앞산에서 야간에 산정에서 복사냉각으로 생성된 국지풍이 지나는 길을 발견할 수 있었다. 그 바람은 대구의 동쪽 지역에서 중력류의 형태로 계곡을 따라서 흘러내렸다. (2) 평지에서는, 그 바람이 대구의 중심지를 지나 서쪽으로 흘러갔다. (3) 그 결과로, 대기오염물질은 야간에 국지풍에 의해 서쪽지역으로 수송되어졌다.

• International Union of Geodesy and Geophysics Korean Journal of Geophysical Research
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• 제25권1호
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• pp.57-81
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• 1997

Numerical prediction of nocturnal thermal high in summer of the 1995 near Taegu city located in a basin has been carried out by a non-hydrostatic numerical model over complex terrain through one-way double nesting technique in the Z following coordinate system. Under the prevailing westerly winds, vertical turbulent fluxes of momentum and heat over mountains for daytime hours are quite strong with a large magnitude of more than $120W/\textrm{m}^2$, but a small one of $5W/\textrm{m}^2$ at the surface of the basin. Convective boundary layer (CBL) is developed with a thickness of about 600m over the ground in the lee side of Mt. Hyungje, and extends to the edge of inland at the interface of land sea in the east. Sensible heat flux near the surface of the top of the mountain is $50W/\textrm{m}^2$, but its flux in the basin is almost zero. Convergence of sensible heat flux occurs from the ground surface toward the atmosphere in the lower layer, causing the layer over the mountain to be warmed up, but no convergance of the flux over the basin results from the significant mixing of air within the CBL. As horizontal transport of sensible heat flux from the top of the mountain toward over the basin results in the continuous accumulation of heat with time, enhancing air temperature at the surface of the basin, especially Taegu city to be higher than $39.3^{\circ}C$. Since latent heat fluxes are $270W/\textrm{m}^2$ near the top of the mountain and $300W/\textrm{m}^2$ along the slope of the mountain and the basin, evaporation of water vapor from the surface of the basin is much higher than one from the mountain and then, horizontal transport of latent heat flux is from the basin toward the mountain, showing relative humidity of 65 to 75% over the mountain to be much greater than 50% to 55% in the basin. At night, sensible heat fluxes have negative values of $-120W/\textrm{m}^2$ along the slope near the top of the mountain and $-50W/\textrm{m}^2$ at the surface of the basin, which indicate gain of heat from the lower atmosphere. Nighttime radiative cooling produces a shallow nocturnal surface inversion layer with a thickness of about 100m, which is much lower than common surface inversion layer, and lifts extremely heated air masses for daytime hours, namely, a warm pool of $34^{\circ}C$ to be isolated over the ground surface in the basin. As heat transfer from the warm pool in the lower atmosphere toward the ground of the basin occurs, the air near the surface of the basin does not much cool down, resulting in the persistence of high temperature at night, called nocturnal thermal high or tropical night. High relative humidity of 75% is found at the surface of the basin under the moderate wind, while slightly low relative humidity of 60% is along the eastern slope of the high mountain, due to adiabatic heating by the srong downslope wind. Air temperature near the surface of the basin with high moisture in the evening does not get lower than that during the day and the high temperature produces nocturnal warming situation.

• Environmental Analysis Health and Toxicology
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• 제30권
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• pp.10.1-10.14
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• 2015

Recent cohort studies have relied on exposure prediction models to estimate individual-level air pollution concentrations because individual air pollution measurements are not available for cohort locations. For such prediction models, geographic variables related to pollution sources are important inputs. We demonstrated the computation process of geographic variables mostly recorded in 2010 at regulatory air pollution monitoring sites in South Korea. On the basis of previous studies, we finalized a list of 313 geographic variables related to air pollution sources in eight categories including traffic, demographic characteristics, land use, transportation facilities, physical geography, emissions, vegetation, and altitude. We then obtained data from different sources such as the Statistics Geographic Information Service and Korean Transport Database. After integrating all available data to a single database by matching coordinate systems and converting non-spatial data to spatial data, we computed geographic variables at 294 regulatory monitoring sites in South Korea. The data integration and variable computation were performed by using ArcGIS version 10.2 (ESRI Inc., Redlands, CA, USA). For traffic, we computed the distances to the nearest roads and the sums of road lengths within different sizes of circular buffers. In addition, we calculated the numbers of residents, households, housing buildings, companies, and employees within the buffers. The percentages of areas for different types of land use compared to total areas were calculated within the buffers. For transportation facilities and physical geography, we computed the distances to the closest public transportation depots and the boundary lines. The vegetation index and altitude were estimated at a given location by using satellite data. The summary statistics of geographic variables in Seoul across monitoring sites showed different patterns between urban background and urban roadside sites. This study provided practical knowledge on the computation process of geographic variables in South Korea, which will improve air pollution prediction models and contribute to subsequent health analyses.

• Journal of the korean society of oceanography
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• 제32권4호
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• pp.171-180
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• 1997

Daily mean sea level variability and its response to atmospheric pressure along the coasts of the northwestern Pacific Ocean are investigated. Daily values of sea level and atmospheric pressure covering the period 1976-1986 from 72 stations are analyzed. The sea level and the air pressure in all the data set have a definite seasonal signal, and higher frequency oscillations at time scales of several days to several weeks are also observed. Among the short-period oscillations of sea level with periods shorter than six months, the period of around 3 or 4 months is dominant in most study stations. According to the statistical analysis of sea level and air pressure, the length scale of sea level variability is smaller than that of air pressure for the present study area. The overall variability of sea level is found to be the smallest around Hokkaido, Japan and the largest in the China coasts. Large short-period (< 6 months) sea level variability is found in the southern coasts of China and Hokkaido, and large long-period (> 6 months) variability in the southern coasts of Japan and Korea along Tsushima Current and Kuroshio. The patterns of air pressure are very similar to those of sea level. The air pressure field is found to account for 31% of the overall sea level variability in the study area. Conside.ins the fact that the results (40%) of Pang and Oh (1995) were obtained through monthly sea level, the present result implies that the short-period sea level variability is less affected by air pressure. Generally the sea level response to air pressure are found to be isostatic, but significantly nonisostatic for the periods around 4 months and for those of 2 to 4 days. In particular, nonisostatic response for higher frequencies seem to be due to the restrictions to water transport necessary for barometric responsein the Korea Strait.

• 한국항행학회논문지
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• 제28권4호
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• pp.436-441
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• 2024

도심항공교통(UAM)은 전기동력 수직이착륙기(eVTOL)를 활용하여 도심 지역에서 승객 및 화물을 운송하는 혁신적인 항공교통관리 시스템으로, 회랑은 비행체가 운항하는 네트워크이자 협력적으로 관리해야 하는 공역으로 정의할 수 있다. UAM의 안정적 운용을 위해서는 전략적 분리 기법과 함께 협력적 의사결정체계(CDM)를 통한 이해관계자 간의 협력과 조정이 필수적이다. 본 연구는 전통적인 항공교통흐름관리에서 적용하는 CDM의 시간 기반 마일스톤을 UAM 체계에 적용하여 안전한 교통량 보장과 최적의 항공교통흐름을 확보하는 방안을 검토하였다. 교통흐름관리를 위해 마일스톤 시간정보는 UAM 이동 상태에 따라 총 13개 주요 마일스톤 시간정보로 구분하였고, 각 시간정보를 제공하는 공유 주체와 마일스톤 흐름을 정의하였다. UAM의 교통량과 수용량 균형을 위해 협력적 의사결정체계(CDM)의 필요성을 강조하며, 이를 통해 이해관계자 간의 마일스톤 정보 공유와 관리는 UAM 기체의 출발 흐름 개선과 운영 효율성 향상에 기여할 것으로 기대한다.

• 한국대기환경학회지
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• 제34권1호
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• pp.16-37
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• 2018

In this study, difference in chemical composition of $PM_{2.5}$ observed between the year 2013 and 2015 at six air quality intensive monitoring stations (Bangryenogdo (BR), Seoul (SL), Daejeon (DJ), Gwangju (GJ), Ulsan (US), and Jeju (JJ)) was investigated and the possible factors causing their difference were also discussed. $PM_{2.5}$, organic and elemental carbon (OC and EC), and water-soluble ionic species concentrations were observed on a hourly basis in the six stations. The difference in chemical composition by regions was examined based on emissions of gaseous criteria pollutants (CO, $SO_2$, and $NO_2$), meteorological parameters (wind speed, temperature, and relative humidity), and origins and transport pathways of air masses. For the years 2013 and 2014, annual average $PM_{2.5}$ was in the order of SL ($${\sim_=}DJ$$)>GJ>BR>US>JJ, but the highest concentration in 2015 was found at DJ, following by GJ ($${\sim_=}SJ$$)>BR>US>JJ. Similar patterns were found in $SO{_4}^{2-}$, $NO_3{^-}$, and $NH_4{^+}$. Lower $PM_{2.5}$ at SL than at DJ and GJ was resulted from low concentrations of secondary ionic species. Annual average concentrations of OC and EC by regions had no big difference among the years, but their patterns were distinct from the $PM_{2.5}$, $SO{_4}^{2-}$, $NO_3{^-}$, and $NH_4{^+}$ concentrations by regions. 4-day air mass backward trajectory calculations indicated that in the event of daily average $PM_{2.5}$ exceeding the monthly average values, >70% of the air masses reaching the all stations were coming from northeastern Chinese polluted regions, indicating the long-range transportation (LTP) was an important contributor to $PM_{2.5}$ and its chemical composition at the stations. Lower concentrations of secondary ionic species and $PM_{2.5}$ at SL in 2015 than those at DJ and GJ sites were due to the decrease in impact by LTP from polluted Chinese regions, rather than the difference in local emissions of criteria gas pollutants ($SO_2$, $NO_2$, and $NH_3$) among the SL, DJ, and GJ sites. The difference in annual average $SO{_4}^{2-}$ by regions was resulted from combination of the difference in local $SO_2$ emissions and chemical conversion of $SO_2$ to $SO{_4}^{2-}$, and LTP from China. However, the $SO{_4}^{2-}$ at the sites were more influenced by LTP than the formation by chemical transformation of locally emitted $SO_2$. The $NO_3{^-}$ increase was closely associated with the increase in local emissions of nitrogen oxides at four urban sites except for the BR and JJ, as well as the LTP with a small contribution. Among the meterological parameters (wind speed, temperature, and relative humidity), the ambient temperature was most important factor to control the variation of $PM_{2.5}$ and its major chemical components concentrations. In other words, as the average temperature increases, the $PM_{2.5}$, OC, EC, and $NO_3{^-}$ concentrations showed a decreasing tendency, especially with a prominent feature in $NO_3{^-}$. Results from a case study that examined the $PM_{2.5}$ and its major chemical data observed between February 19 and March 2, 2014 at the all stations suggest that ambient $SO{_4}^{2-}$ and $NO_3{^-}$ concentrations are not necessarily proportional to the concentrations of their precursor emissions because the rates at which they form and their gas/particle partitioning may be controlled by factors (e.g., long range transportation) other than the concentration of the precursor gases.

• 한국연소학회:학술대회논문집
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• 한국연소학회 1997년도 제15회 KOSCO SYMPOSIUM 논문집
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• pp.77-87
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• 1997

The axisymmetric Navier-Stokes model together with detailed chemical kinetics and variable transport properties has been applied to analyze the effects of the multidimensional flow on the flame characteristics in the nitrogen-diluted hydrogen counterflow nonpremixed flame. Computations are performed for two nozzle exit area-averaged velocities. Effects of multidimensional flow and strain rate on the near-extinction structure of the highly diluted hydrogen flames are discussed in detail.

• 한국대기환경학회:학술대회논문집
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• 한국대기환경학회 2007년도 추계학술대회 논문집
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• pp.193-194
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• 2007

• 한국대기환경학회:학술대회논문집
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• 한국대기환경학회 2009년도 추계학술대회 논문집
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• pp.179-181
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• 2009