• 대한원격탐사학회지
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• 제27권3호
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• pp.235-258
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• 2011

The purpose of this study is to investigate climatological variations from the temporal and spatial surface particulate organic carbon (POC) estimates based on SeaWiFS spectral radiance, and to determine the physical mechanisms that affect the distribution of pac in the Gulf of Mexico. 7-year monthly mean values of surface pac concentration (Sept. 1997 - Dec. 2004) were estimated from Maximum Normalized Difference Carbon Index (MNDCI) algorithm using SeaWiFS data. Synchronous 7-year monthly mean values of remote sensing data (sea surface temperature (SST), sea surface wind (SSW), sea surface height anomaly (SSHA), precipitation rate (PR)) and recorded river discharge data were used to determine physical forcing factors. The spatial pattern of POC was related to one or more factors such as river runoff, wind-derived current, and stratification of the water column, the energetic Loop Current/Eddies, and buoyancy forcing. The observed seasonal change in the POC plume's response to wind speed in the western delta region resulted from seasonal changes in the upper ocean stratification. During late spring and summer, the low-density river water is heated rapidly at the surface by incoming solar radiation. This lowers the density of the fresh-water plume and increases the near-surface stratification of the water column. In the absence of significant wind forcing, the plume undergoes buoyant spreading and the sediment is maintained at the surface by the shallow pycnocline. However, when the wind speed increases substantially, wind-wave action increases vertical motion, reducing stratification, and the sediment were mixed downward rather than spreading laterally. Maximum particle concentrations over the outer shelf and the upper slope during lower runoff seasons were related to the Loop Current/eddies and buoyancy forcing. Inter-annual differences of POC concentration were related to ENSO cycles. During the El Nino events (1997-1998 and 2002-2004), the higher pac concentrations existed and were related to high runoffs in the eastern Gulf of Mexico, but the opposite conditions in the western Gulf of Mexico. During La Nina conditions (1999-2001), low Poe concentration was related to normal or low river discharge, and low PM/nutrient waters in the eastern Gulf of Mexico, but the opposite conditions in the western Gulf of Mexico.

• 한국지구과학회지
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• 제39권5호
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• pp.419-435
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• 2018

본 연구의 목적은 서산 태안 지역에서 마늘 생산량에 영향을 주는 기상 및 기후 인자를 파악하고 농가의 기후정보이용에 따른 경제적 가치를 분석하는 것이다. 이 지역에서 기후 특성과 경향이 1984-2013년의 서산지방기상청 기상자료, 1989-2013년의 마늘 생산량 국가통계자료, 2001-2100년간의 기후변화 시나리오 자료(RCP 4.5, 8.5)와 함께 분석되었다. 연구 결과는 다음과 같다. 첫째, 서산 태안 지역에서 겨울철 평균기온과 평균풍속이 다른 마늘 재배 지역에 비해 낮고 강하여 마늘 성장을 위한 저온 조건을 만족하였고, 5월의 누적강수량이 감소하여 한지형 마늘이 생육하기에 적합한 것으로 나타났다. 하지만 마늘의 수확기 때 평균기온, 누적강수량 및 평균풍속 등의 증가추세로 인해 미래 한지형 마늘 재배지는 줄어들 것이다. 둘째, 서산 태안 지역에서 기후변화 시나리오(RCP 4.5, 8.5)를 이용한 한지형과 난지형 마늘 모두 파종적기는 현재보다 늦어지고 수확적기는 빨라지며, 추후 100년 동안 재배기간이 50-90일 정도 짧아지는 것으로 나타난다. 셋째, 마늘 흑색썩음균핵병과 고자리파리의 발생 시작 일이 평균기온($^{\circ}C$)과 토양습도(%)를 이용한 기상 알고리즘을 적용함으로서 산출되었다. 특별히 RCP 4.5와 RCP 8.5 시나리오에서 미래 마늘 흑색썩음균핵병 발생일은 모두 현재보다 앞당겨 지는 것으로 나타났다. 넷째, 서산 태안지역에서 마늘 생산량(ka/10a)은 월동기 최저기온, 추대기 누적강수량, 월동기 평균풍속, 그리고 추대기 평균상대습도와 높은 상관을 나타내었다. 한편 마늘 재배에 있어 기후정보이용에 따른 마늘 생산량은 총생산량의 약 9%로 경제적 가치가 증가하는 것으로 나타났다.

• 한국기후변화학회지
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• 제2권4호
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• pp.317-331
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• 2011

보리 생육모형인 DSSAT의 CERES-Barley를 적용하여, 한반도 A1B 기후변화시나리오에 따른 겉보리의 잠재생산량을 평가하였다. 생육 모의 지역은 30년 평년의 기상자료가 구축되어 있는 56개 지역으로 하였고, 생육 모의 연도는 기준연도(1971~2000년)와 3가지 미래 30년 평년(2011~2040년, 2041~2070년, 2071~2100년)으로 하였다. 그리고 온도효과 분석(온도 변화, $CO_2$ 농도 고정), $CO_2$효과 분석(온도 고정, $CO_2$ 농도 변화), 온난화효과 분석(온도 및 $CO_2$ 농도 변화) 등 3가지 생육모의 환경으로 구분하여 기후변화에 따른 겉보리의 잠재생산성 영향을 평가하였다. CERES-Barly 모형은 국내 겉보리의 발육단계뿐 아니라 수량을 실제 관측값과 아주 유사하게 모의하여($R^2=0.84$), 기후변화에 따른 겉보리의 잠재생산성 변화 예측에 활용하는데 무리가 없다고 판단되었다. 생육 모의 조건별 결과를 나타내면, (1) 온도효과 분석에서, 미래의 온도상승이 상대적으로 낮은 2011~ 2040년 생육 모의 연도의 잠재수량은 기준년도와 비슷한 반면에, 온도상승 정도가 큰 2041~2070, 2071~2100년의 미래 기후조건에서는 잠재수량이 기준년도에 비해 각각 6, 20%씩 감소하였다. 다음으로, (2) $CO_2$ 효과 분석에서, 3가지 미래 기후조건(2011~2040년, 2041~2070년, 2071~2100년)에서 겉보리의 평균 잠재수량이 기준년도에 비해 각각 12, 28, 43%씩 증가하였다. 마지막으로 (3) 온난화효과 분석에서, 미래 생육 모의 연도별(2011~2040년, 2041~2070년, 2071~2100년) 잠재수량은 기준년도에 비해 각각 13, 21, 19%씩 증가하였다.

• 환경영향평가
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• 제4권3호
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• pp.73-86
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• 1995

This paper demonstrates Environmental Impact Assessment (EIA) has to be applied for development projects with regard to the ecological, economical and social aspects before any decisions made in the project. Korea has confronted various environmental problems during the last fifteen years, even though EIA has been enacted since 1981. The role of impact assessment in planning and policy processes should be emphasized to investigate the magnitude and intensity of the adverse influences of economic development. In the Seoul Metropolitan Region, it is necessary to apply EIA all urban projects to reduce the adverse effects of urbanization. Special attention should be given to the climatological effects throughout the urbanization process in Korea to keep the urban area energy-efficient. This study intends not only to establish basic data for national-and regional-based land-use policy in the environmental aspects, but also to provide the basic data for the possible climate model (scenarios) that may provide spatial and temporal variability by analyzing the actual climatic record. There is a noticeable impact of urbanization on the atmospheric environment in the Seoul Metropolitan Region. In this sense, the climatic aspect must be taken into consideration in the process of EIA to mitigate the well-known climatic alterations of urbanization. Moreover, the techniques of assessment should be improved by developing geo-reference data sets to build models of the global climate in response to the man-made environmental change.

• 한국지구과학회지
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• 제29권5호
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• pp.428-436
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• 2008

This study observed the upper tropospheric ozone enhancement in the northern Atlantic for the Aerosols99 campaign in January-February 1999. To find the origin of this air, we have analyzed the horizontal and vertical fields of Isentropic Potential Vorticity (IPV) and Relative Humidity (RH). The arch-shaped IPV is greater than 1.5 pvus indicating stratospheric air stretches equatorward. These arch-shaped regions are connected with regions of RH less than 20%. The vertical fields of IPV and RH show the folding layer penetrating into the upper troposphere. These features support the idea that the upper tropospheric ozone enhancement originated from the stratosphere. Additionally, we have investigated the climatological frequency of stratospheric intrusion over the tropical north Atlantic using IPV and RH. The total frequency between the equator and $30^{\circ}N$ over the tropical north Atlantic exhibits a maximum in northern winter. It suggests that the stratospheric intrusion plays an important role in enhancing ozone in the upper troposphere over the tropical north Atlantic in winter and early spring. Although the tropospheric ozone residual method assumed zonally invariant stratospheric ozone, stratospheric zonal ozone variance could be caused by stratospheric intrusions. This implies that stratospheric intrusion influences ozone variance over the Atlantic in boreal winter and spring, and the intrusion is a possible source for the tropical north Atlantic paradox.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 1999년도 Proceedings of International Symposium on Remote Sensing
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• pp.237-242
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• 1999

As one of the key parameters to determine $CO_2$ flux between air - sea interface, it is quite important to know p$CO_2$, which has involved much uncertainty, mainly due to the complex variations of sea surface p$CO_2$ and the paucity of samples, made in ocean. In order to improve the interrelationship between partial pressure (p$CO_2$) and different physical and biochemical parameters in global sea surface water, a new empirical relation is established to correlate and parameterize p$CO_2$ in the mixed layer using the data from recent WOCE cruises. Meanwhile, by new empirical relation, abundant historical hydrographic and nutrients ship data, Levitus data set and NOAA/AVHRR(SST), p$CO_2$ have been accumulated and applied. Then effort has to be made fur promotion of this study to correlate and parameterize p$CO_2$ in the mixed Layer with different physical and biochemical parameters. and further attribute this huge historical data sets and NOAA/AVHRR(SST) data to estimate p$CO_2$. In this paper we analyzed more interrelationship between the model and ship/satellite data set. Finally, the inter-annual variations of p$CO_2$ in sea are presented and discussed.

• 대기
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• 제20권4호
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• pp.505-518
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• 2010

We investigated the impacts of the diabatic heating location, vertical profile and basic state on the Rossby wave propagation. To examine the dynamical process of individual responses on the regional heat source, a dry version of the linear baroclinic model was used with climatological summertime (JJA) mean basic state and vertical structure of the diabatic heating for 1979-2008. Two sets of diabatic heating were constructed of those positioned in the mid-latitudes (Tibetan Plateau, eastern Mediterranean Sea, and the west-central Asia) and the tropics (the southern India, Bay of Bengal, and western Pacific). It was found that using the principal component analysis, atmospheric response to diabatic heating reaches to the steady state in 19th days in time. The prescribed mid-latitude forcing forms equivalent barotropic Rossby wave propagation along the westerly Asia jets, whereas the tropical forcing generates the Rossby wave train extending from the tropics to mid-latitudes. In relation to the maximum vertical profile, the mid-level forcing reveals a stronger response than the lower-level forcing, which may be caused by more effective Rossby wave response by the upper-level divergent flow. Under the different sub-seasonal mean state, both of the tropical and mid-latitude forcing induce the different sub-seasonal response intensity, due to the different basic-state wind.

• Corrosion Science and Technology
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• 제8권3호
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• pp.116-118
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• 2009

Korea Institute of Construction Materials founded Seosan Outdoor Exposure Test Site 2005 at Korea, which is a part of Worldwide Exposure Network (WEN). To evaluate the test site along with other exposure test sites, three different types of paints have been under real time weathering conditions at three major weathering test facilities around the world. Using these test specimens several spectroscopic experiments along with physical tests have been performed. Also acceleration tests have been performed using the same paints. The correlation of weathered paints among three different test facilities and accelerated test results has been compared. From the results the reliability of Seosan Weathering Test Facility and reasonable life time prediction tests are discussed.

• 한국환경과학회지
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• 제16권5호
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• pp.583-591
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• 2007

In this study, meteorological characteristics concerning the occurrence of fog are analyzed using 4-years (2000-2003) data at Chuncheon. From the analysis of meteorological characteristics, the fog at Chuncheon occurred before sunrise time and disappeared after that time and lasted for 2-4 hours. When fog occurred, on the whole, wind direction was blew the northerly and wind speed was below 2.1 m/s. Especially, about 42 % of foggy day fell on the calm($0{\sim}0.2m/s$) conditions. The difference between air temperature and dew point temperature near the surface were mainly less than $2^{\circ}C$. For the lack of water surface temperature, the water sur-face temperature was calculated by using Water Quality River Reservoir System (WQRRS). In Chuncheon, there is close correlation between the frequency of fog day and outflow from Soyang reservoir and high frequency of occurrence due to the difference between air and cold outlet water temperature.

• 한국GIS학회:학술대회논문집
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• 한국GIS학회 2003년도 공동 춘계학술대회 논문집
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• pp.517-522
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• 2003

증발산량의 정확한 산정은 자연현상과 인문현상을 이해하는데 있어 중요하다. 증발산량의 점추정이 갖는 한계를 극복하기 위해 원격탐사를 이용하여 증발산량을 추정하는 방법이 활발히 연구되고 있다. 이 중 SEBAL 모형은 원격탐사 자료를 이용하는 기존의 방법에 비해 소요되는 자료가 적으면서도, 증발산량을 정확하게 추정하는 방법으로 알려지고 있다. 이 연구에서는 우리나라 지형에서 SEBAL 모형의 적용 가능성을 검증하였고, 증발산량 분포의 시공간적 특성을 살펴보았다. 연구 지역은 금강 상류의 보청천 유역이며, Landsat 5 TM영상(1995년 1월 11일, 4월 1일, 5월 3일, 10월 10일, 11월 27일)을 이용하였다.