• Proceedings of the Korea Water Resources Association Conference
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• 1983.07a
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• pp.84-88
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• 1983

• Journal of Korean Society for Atmospheric Environment
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• v.24 no.2
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• pp.196-205
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• 2008

Variability in vertical ozone and meteorological profiles was measured by 2Z electrochemical concentration cells (ECC) ozonesonde at Bangyi in Seoul ($37.52^{\circ}N$, $127.13^{\circ}E$) during June $6{\sim}9$, 2003 in odor to identify the vertical distribution of ozone and its relationship with the lower-atmospheric structure resulted in the high ozone concentrations near the surface. The eight profiles obtained in the early morning and the late afternoon during the study period clearly showed that the substantial change of ozone concentrations in lower atmosphere(${\sim}5\;km$), indicating that it is tightly coupled to the variation of the planetary boundary layer (PBL) structure as well as the background synoptic flow. All profiles observed early in the morning showed very low ozone concentrations near the surface with strong vertical gradients in the nocturnal stable boundary layer due to the photochemical ozone loss caused by surface NO titration under very weak vertical mixing. On the other hand, relatively uniform ozone profiles in the developed mixing layer and the ozone peaks in the upper PBL, were observed in the late afternoon. It was noted that a significant increase in ozone concentrations in the lower atmosphere occurred with the corresponding decrease of the mixing height in the late afternoon on June 8. Ozone in upper layer did not vertically vary much compared to that in PBL but changed significantly on June 6 that was closely associated with the variation of synoptic flows. Interestingly, heavily polluted ozone layers aloft (a maximum value of 115 ppb around 2 km) were formed early in the morning on 6 through 7 June under dominant westerly synoptic flows. This indicates the effects of the transport of pollutants on regional scale and consequently can give a rise to increase the surface ozone concentration by downward mixing processes enhanced in the afternoon.

• Journal of the Korean Society of Hazard Mitigation
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• v.6 no.1 s.20
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• pp.83-95
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• 2006

This study aims to analysis of suspended-load concentration in related to those data by measuring vertical sediments distribution with rainfall using the ASM (Argus Surface Meter)- IV at the channel reach of a upstream and a downstream in small river. The watershed, small river basin where had taken for experimental study was selected, which is a drainage area lied at Walha in Yunkee-Gun, Chungnam Province. Measured data of suspended-load concentration consists of two groups with 2,145 data during 1hr 11min 30sec and 1,216 data during 40min 32sec for measuring time of 2 second in the study reaches at river, respectively. In order to analyze of the vertical concentration distribution, using the data sets are selected the measuring time 16 sets one of these data by random in the study reaches. As a results, the Rouse number of a measured and a calculated value show that a rang of $0.00129{\sim}0.02394$, averaged value of 0.01129 md, a rang of $0.00118{\sim}0.00822$, averaged value of 0.00436 in upstream reaches, and also a rang of $0.065115{\sim}0.065295$, averaged value of 0.06521, and a rang of $0.057315{\sim}0.059109$, averaged value of 0.05795 in downstream reaches, respectively. These difference show that measured Rouse number compared with downstream reach errors of less than in upstream reach, but between measured and calculated of the Rouse number compared with downstream reach errors of more than in upstream reach, respectively. It seems to will be included one of the occurrence errors of variable estimations when Rouse number of calculated value to be made computed by the fall velocity with a high temperature of water using equation of empirical kinematic viscosity was derived in this study.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2001.11a
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• pp.73-74
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• 2001

도시지역의 오존농도는 배출원 환경 및 지형과 국지 기상조건에 의해 크게 영향을 받게 된다. 일반적으로 도시내 공단과 교통량이 많은 지역에서는 다량의 NO 배출에 의한 오존의 감소가 일어나는 반면 도시플륨의 풍하측의 지역에서는 오존의 축적과 함께 고농가 발생하게 된다 (Wang et al., 2001; Bower et al., 1994; Mckendry). 특히 연안도시의 경우 여름철 주로 발생하는 국지순환인 해풍에 의한 고농도를 경험하게 되는데, 이는 수면의 낮은 오존침적으로 인해 소멸의 영향이 적고 (Entwistle, 1997), 해풍역전으로 인한 연직혼합의 제한으로 인해 발생한다고 볼 수 있다 (Lu and Turco, 1994). (중략)

• Proceedings of The Korean Society of Agricultural and Forest Meteorology Conference
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• 2019.08a
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• pp.201-202
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• 2019

• Korean Journal of Remote Sensing
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• v.31 no.5
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• pp.409-419
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• 2015

The Atmospheric Emitted Radiance Interferometer (AERI) which is the Fourier Transform InfraRed (FTIR) spectrometer has been operated by the National Institute of Meteorological Research (NIMR) in Anmyeon island, South Korea since June 2010. The ground-based AERI with similar hyper-spectral infrared sensor to satellite could be an alternative way to validate satellite-based remote sensing. In this regard, the NIMR has focused on the improvement of Cloud data Filtering Method (CFM) which employed only one reference spectrum of clear sky in winter season. This study suggests Seasonal-Cloud data Filtering Method (S-CFM) which applied seasonal AERI reference spectra. For the comparison of applied S-CFM and CFM, the methane retrievals (surface volume mixing ratio) from AERI spectra are used. The quality of AERI methane retrieval applied S-CFM was significantly more improved than that of CFM. The positive result of S-CFM is similar pattern with the seasonal variation of methane from ground-based in-situ measurement, even if the summer season's methane is retrieved over-estimation. In addition, the comparison of vertical total column of methane from AERI and GOSAT shows good result except for the summer season.

• Proceedings of the Korea Air Pollution Research Association Conference
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• 2003.05b
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• pp.303-304
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• 2003

연안도시의 경우 해양 배경농도의 영향과 내륙과 비교해 강한 풍속조건이 형성됨으로 오존농도의 일변화 폭이 적으며 야간에 농도상승 현상이 빈번히 나타난다. 또한 일반적으로 여름철 주로 발생하는 해풍에 의해 고농도를 경험하게 되는데, 이는 해풍역전으로 인한 연직혼합의 억제와 (Lu and Turco, 1994) 해풍전선의 이동 (McElroy and Smith, 1991), 해풍의 내륙침투 시 생기는 Fumigation 효과(Entwistle, et al., 1997; Zhang et al., 1998) 등으로 설명되어 진다. 아울러 해륙풍순환으로 생기는 오전의 대기정체현상은 오후의 오존의 광화학 생성과 축적에 기여하게 되며 (Liu et al., 1994), 해풍 발달 시에는 오존 및 전구물질이 내륙 수송되어 풍하측 지역에 고농도가 나타나게 된다(Zhang et al., 1998). (중략)

• Proceedings of the Korea Water Resources Association Conference
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• 2005.05b
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• pp.469-473
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• 2005

수질모형의 지배방정식에서 정의되는 대표적인 수질매개변수는 유역 및 대기로부터의 오염부하량 퇴적물로부터의 오염물질 용출부하량, 확산계수. 반응계수 등으로 직접적인 관측이 곤란할 뿐만 아니라 많은 관측비용을 필요로 한다. 본 연구에서는 매개변수를 포함한 오염물질 수지방정식을 구성하고, 구성된 선형 연립방정식을 이용함으로써 계산된 농도분포자료와 관측된 시계열 농도분포자료를 이용하여 계산한 질량변화량의 차이를 최소화하는 역산문제를 구성하여 모형의 매개변수를 추정하는 방법을 제시하였다. 이 방법을 이용하여 천수만, 울산만(울산항) 해역에서 관측된 연직방향 농도분포 자료를 이용하여 확산계수 및 대기로부터의 오염부하량, 퇴적물로부터의 오염물질 용출율, 확산$\cdot$반응에 의한 오염물질 변화량 등을 추정하였으며, 추정 매개변수는 시기적으로 변동이 크게 나타났다. 반면, 추정매개변수를 이용한 관측자료와 계산결과를 비교한 결과, RMS 오차는 관측자료 범위의 $5.0\% 이하, 일치지수는 0.95 이상으로 본 방법을 이용한 매개변수 추정결과의 신뢰성은 우수한 것으로 파악되었다.

• The Sea:JOURNAL OF THE KOREAN SOCIETY OF OCEANOGRAPHY
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• v.24 no.1
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• pp.1-17
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• 2019

In this study, the surveys were carried out from October (2016) to October (2017) along the tidal flat of Geunso Bay, Taean Peninsula of the western edge of Korea. The sampling trips were carried out for a total of 16 times, once or twice a month. In order to investigate the monthly variation of the microphytobenthos (MPB) biomass, community composition and photo-physiology were analyzed by HPLC (High performance liquid chromatography). The total chlorophyll a (TChl a) concentrations used as an indicator of biomass of MPB in the upper 1 cm sediment layer ranged from 40.4 to $218.9mg\;m^{-2}$ throughout the sampling period. TChl a concentrations showed the maximum level on $24^{th}$ of February and remained high throughout March after which it started to declined. The biomass of MPB showed high values in winter and low values in summer. The monthly variations of Phaeophorbide a concentrations suggested that the low grazing intensity of the predator in the winter may have partly attributed to the MPB winter blooming. As a result of monthly variations of the MPB community composition using the major marker pigments, the concentrations of fucoxanthin, the marker pigment of benthic diatoms, were the highest throughout the year. The concentrations of most of the marker pigments except for chlorophyll b (chlorophytes) and peridinin (dinoflagellates) increased in winter. However, the concentrations of fucoxanthin increased the highest, and the relative ratios of the major marker pigments to TChl a except fucoxanthin decreased during the same period. The vertical distribution of Chl a and oxygen concentrations in the sediments using a fluorometer and an oxygen micro-optode Chl a concentrations decreased with oxygen concentrations with increasing depth of the sediment layers. Moreover, this tendency became more apparent in winter. The Chl a was uniformly vertical down to 12 mm from May to July, but the oxygen concentration distribution in May decreased sharply below 1 mm. The increase in phaeophorbide a concentration observed at this time is likely to be caused by increased oxygen consumption of zoobenthic grazing activities. This could be presumed that MPB cells are transported downward by bioturbation of zoobenthos. The relative ratios (DT/(DD+DT)) obtained with diadinoxanthin (DD) and diatoxanthin (DT), which are often used as indicators of photo-adaptation of MPB, decreased from October to March and increased in May. This indicated that there were monthly differences in activity of Xanthophyll cycle as well.

• Journal of Korea Water Resources Association
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• v.54 no.8
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• pp.607-616
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• 2021

The purpose of this study is to simulate the transport of nonuniform sediment considering the hiding-exposure effect numerically. In order to calculate the transport of multi-disperse suspended sediment mixtures, the set of advection-diffusion equations for each particle class is solved. The applicability of the numerical model is examined by comparing the simulation results with experimental data. In this study, we calculate the vertical distribution of total concentration of sediment particles using two approaches: (1) by considering the mixture as represented by a single size; and (2) by combining the concentration of the sediment corresponding to several particle size classes; From the simulation results, it is shown that both approaches calculate reasonable results due to the narrow range of size distribution. Under the condition of nonuniform sediment, the critical shear stress of the sediment particle is influenced by the size-selective entrainment, i.e., hiding-exposure effect. It is shown in this study that the effect of hiding-exposure effect on the erosion rates of fine sand is negligibly small.