• 한국지하수토양환경학회지:지하수토양환경
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• 제16권3호
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• pp.38-47
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• 2011

Groundwater monitoring data from the National Groundwater Monitoring Stations, a total of 320 stations, were analyzed to identify the response of water level and quality to the Odaesan earthquake (M4.9) occurred in January 2007. Among the total of eight stations responded to the earthquake, five wells showed water-level decline, and in three wells, water level rose. In terms of recovery, water levels in four stations had recovered to the original level in five days, but not in the rest four wells. The magnitude of water-level change shows weak relations to the distance between the earthquake epicenter and the groundwater monitoring station. However, the relations to the transmissivities of monitored aquifer in the station with the groundwater change were not significant. To implement the earthquake monitoring system through the groundwater monitoring network, we still need to accumulate the long-term monitoring data and geostatistically analyze those with hydrogeological and tectonic factors.

• 한국환경과학회지
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• 제23권3호
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• pp.503-510
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• 2014

To estimate the benefit of high-resolution meteorological data for building energy estimation, a building energy analysis has been conducted over Busan metropolitan areas. The heating and cooling load has been calculated at seven observational sites by using temperature, wind and relative humidity data provided by WRF model combined with the inner building data produced by American Society of Heating Refrigeration and Air-conditioning Engineers (ASHRAE). The building energy shows differences 2-3% in winter and 10-30% in summer depending on locations. This result implicates that high spatiotemporal resolution of meteorological model data is significantly important for building energy analysis.

• 한국대기환경학회지
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• 제25권1호
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• pp.57-74
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• 2009

In order to clarify the vertical ozone distribution in planetary boundary layer of coastal area with complex terrain, an observation campaign was carried out around Gwangyang Bay with dense pollutant emission sources during two days from June, 4 2007. For this observation are Radiosonde, SODAR(SOnic Detection And Ranging) and Tethered ozone sonde were employed. The surface meteorological and photochemical observation data provided by AWS (Automatic Weather System) and AQMS (Air Quality Monitoring System) were also applied for analysis. Synoptic condition is strongly associated with lower level ozone distribution in complex terrain coastal area. Since mesoscale circulation induced by difference of characteristics of land and sea and orographic forcing is predominant under calm synoptic condition, vertical distribution of ozone is complicate and vertical ozone concentration greatly fluctuated. However in second day when synoptic influence become strong, ozone concentration in lower levels is vertically uniform regardless of observation level. This results in vertical observation indicates that vertical ozone distribution is often determined by synoptic condition and also affects surface ozone concentration.

• 천문학논총
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• 제19권1호
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• pp.55-63
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• 2004

Observation environment of the Bohyunsan Optical Astronomy Observatory(BOAO) has been examined using various statistical data including real observation times versus allocated times and seeing statistics. The data have been collected from the observation logs of the 1.8m telescope in the period 1998 - 2004. New criteria have been set up to calculate a more realistic observation efficiency of the observatory. The new statistical analysis based on the new criteria gives the overall observation efficiency of BOAO as $38.6\%$, that is equivalent to 115.8 observable nights out of 300 allocatable nights. The seeing statistics shows that the mean seeing measured at the focal images is 2".3. The present study of the observation environment of BOAO suggests that differential photometry and spectroscopy should be preferred modes of observation to maximize the productivity of BOAO.

• 한국지구과학회지
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• 제23권3호
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• pp.270-279
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• 2002

주요 온실기체인 이산화탄소와 메탄의 농도를 난지도 매립장에 위치한 42개의 배출공으로부터 측정하였다. 그 결과에 의하면, 배출공의 출구에서 관측된 메탄은 부피기준으로 절반 그리고 이산화탄소는 28%에 가까운 수준으로 높은 농도를 유지하였다. 그러나 이들의 환경거동은 배출공의 위치 등과 같은 차이 외에도 가스성분에 따라 여러 가지차이를 보여 주었다. 본 연구의 결과는 이들 성분의 분포가 수은과 같은 미량성분의 분포특성과는 달리 대체로 균질한편이라는 것을 확인해 주었다.

• 한국지구과학회지
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• 제32권2호
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• pp.180-189
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• 2011

엘니뇨/라니냐의 강도 변화에 따른 한반도의 풍력자원 변동성을 확인하기 위하여 20년간 장기 지상관측자료를 바탕으로 해석적인 분석을 실시하였다. 장기적으로 유라시아 대륙의 풍속 약화경향에도 불구하고 한반도는 최근 10년간 풍속 증가가 약하게 나타났다. 그리고 엘니뇨와 라니냐에 따른 한반도 풍속은 계절적으로 다양한 형태를 나타낸다. 지역적으로 음의 해수면 온도 아노말리를 나타내는 라니냐가 발생하면 한반도내 지상풍속이 빨라지는 경향을 가진다. 그리고 기후변화에 대한 풍속은 중규모의 강제력이 가장 미약한 산악지역에서 가장 민감하게 나타난다.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2003년도 Proceedings of ACRS 2003 ISRS
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• pp.840-842
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• 2003

Recent satellite data have revealed a correlation between the Sun’s activities and the Earth’s atmosphere . Many scientists have been conjectured a more direct connections between solar variability and the Earth’s atmosphere from satellite data analysis. During solar storms, more energetic particles reach the Earth’s atmosphere and this phenomenon have effects on the Earth’s atmospheric environment. Consequently, scientists suggest that these variations will affect a global climate change. In this study, we investigate the confirmative research results of atmospheric effects due to solar activities, especially solar storms.

• 한국산업정보학회논문지
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• 제28권6호
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• pp.45-52
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• 2023

최근 일상생활 속 보행의 중요성이 강조되면서 보행권 보장 및 보행환경 조성을 위한 사업이 지역 곳곳에서 추진되고 있다. 선행 연구에서는 전주시 도로 이미지를 사용하여 보행환경 평가를 진행하고, 이미지 비교 쌍 데이터 세트를 구축하였다. 하지만 숫자로 표현된 데이터 세트는 보행환경 평가자들의 판단 기준을 일반화하거나 보행자가 선호하는 보행환경을 시각적으로 파악하기에 어려움이 존재한다. 따라서 본 연구는 웹 애플리케이션을 구축하여 데이터 시각화를 통해 보행환경 평가의 결과를 해석하는 방법을 제안한다. 의미론적 분할 결과를 활용하여 보행환경 평가자에게 영향을 미치는 보행환경 구성 요소를 분석한 결과, 보행자는 주로 'earth'와 'grass'가 많은 환경을 선호하지 않았고, 'signboard'와 'sidewalk'를 가진 환경을 선호하는 것으로 확인하였다. 제안된 연구는 향후 보행환경 평가의 참여자가 임의로 선택한 결과를 파악하고 분석할 수 있을 것으로 기대하며, 데이터에 대한 정제과정을 전처리로 수행함으로써 좀 더 향상된 정확도를 얻을 수 있을 것으로 판단한다.

• 천문학논총
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• 제15권spc2호
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• pp.1-13
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• 2000

Through the coupling between the near-earth space environment and the polar ionosphere via geomagnetic field lines, the variations occurred in the magnetosphere are transferred to the polar region. According to recent studies, however, the polar ionosphere reacts not only passively to such variations, but also plays active roles in modifying the near-earth space environment. So the study of the polar ionosphere in terms of geomagnetic disturbance becomes one of the major elements in space weather research. Although it is an indirect method, ground magnetic disturbance data can be used in estimating the ionospheric current distribution. By employing a realistic ionospheric conductivity model, it is further possible to obtain the distributions of electric potential, field-aligned current, Joule heating rate and energy injection rate associated with precipitating auroral particles and their energy spectra in a global scale with a high time resolution. Considering that the ground magnetic disturbances are recorded simultaneously over the entire polar region wherever magnetic station is located, we are able to separate temporal disturbances from spatial ones. On the other hand, satellite measurements are indispensible in the space weather research, since they provide us with in situ measurements. Unfortunately it is not easy to separate temporal variations from spatial ones specifically measured by a single satellite. To demonstrate the usefulness of ground magnetic disturbance data in space weather research, various ionospheric quantities are calculated through the KRM method, one of the magneto gram inversion methods. In particular, we attempt to show how these quantities depend on the ionospheric conductivity model employed.

• 한국지하수토양환경학회지:지하수토양환경
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• 제15권6호
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• pp.46-52
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• 2010

Derivative analysis, based on the derivative of the drawdown as a function of time (i.e., rate of drawdown change), was applied to the evaluation of hydraulic parameters of the aquifer as an aid of the aquifer test interpretation based on the Theis solutions. Pumping tests were conducted at a coastal fractured aquifer in Muan county, Korea, of which the drawdown data, measured at the two observation wells, were used for derivative analysis. Wellbore storage and transition period were hard to identify at conventional log-log and semi long plots, but was easily recognized by distinctive curves of positive unit slope, hump and negative unit slope in the derivative plot. For the observation well of OW-2 at which wellbore storage and transition lasted over an hour, conventional aquifer analysis would suffer from the uniqueness problems and in further result in erroneous hydraulic parameters. Derivative analysis was found to be effective for distinguishing the drawdown data directly reflecting the aquifer property from those reflecting non aquifer effects such as wellbore storage and transition, which offers a unified methodology to yield correct hydraulic parameters from aquifer test data.