• 한국해안·해양공학회논문집
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• 제22권1호
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• pp.58-66
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• 2010

본 논문에서는 지상 LiDAR 및 MBES(다중빔 음향측심기)를 이용하여 정밀 지형 및 수심측량을 실시하였고, 조간대 영역의 육도-해도 접합을 통하여 대조차 해안인 만리포에 대한 정밀 지형도를 작성하였다. 제한된 시간내에 조간대 영역의 충분한 지형정보 획득을 위하여 간조시 지상 LiDAR 및 DGPS를 차량지붕에 탑재하여 이동 정지 스캐닝의 해변 전체의 지형정보를 획득하였고, 이와 동시에 만조시 MBES를 통하여 수심측량을 실시하였으며 조위계 설치와 목측을 통한 조위관측의 병행을 통하여 수심보정자료 및 만리포의 평균해면 추산자료로 사용하였다. 조간대 정합을 위해 지형 및 수심자료의 수직좌표계 기준면은 인천 평균해면으로 단일화하였으며, 조간대 평균 중첩오차는 약 2~6 cm 이내로 나타났다. 또한 지상 LiDAR 자료의 정확도 검증을 위해 RTK-DGPS 측량을 동시에 실시하여 수직좌표값을 비교한 결과 평균 제곱근 오차가 약 4~7 cm 이내로 나타났다. 정밀지형도 작성은 GIS 기반 자료처리를 통하여 50 cm 해상도를 갖는 수치표고자료로 생산하였으며, 이는 현재 연안지역 침수범람 예측을 위한 폭풍해일 침수범람 예측모델의 정밀 입력자료로 사용되고 있다. 또한 장기간에 걸친 주기적 측량 자료와 측량시의 인위적 해변 변화량 및 해양환경정보를 함께 고려하여 3차원 공간분석을 실시한다면 침 퇴적양의 정확한 산출을 통하여 연안 모니터링에도 효과적으로 활용될 수 있을 것이다.

• 한국산림과학회지
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• 제95권6호
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• pp.663-671
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• 2006

본 연구는 소나무림과 참나무류림의 공간분포 패턴을 규명하기 위하여 수행하였다. 공간분석을 위한 기초 자료로 수치 임상도와 현존식생도를 활용하여 $100m{\times}100m$ 격자 단위로 전국 단위의 소나무림과 참나무류림 분포도를 제작하였다. 또한 $100m{\times}100m$ 래스터 격자 단위의 지형, 기후, 토양 관련 주제도를 제작하였다. 이상의 소나무림과 참나무류림의 분포도와 주제도간의 GIS 기반 공간 분석을 실시하여 지형, 기후, 토양 등의 환경 인자에 따른 소나무림과 참나무류림의 공간분포 특성을 분석하였으며, 이러한 공간분포 특성을 활용하여 소나무림과 참나무류림의 출현빈도모델을 제시하였다. 소나무림의 경우 참나무류림에 비하여 상대적으로 표고가 낮고 경사도가 완만하며 기온이 높은 지역에 많이 분포하고 있는 것으로 나타났다. 또한, 소나무림은 양토, 보통 이하의 얕은 토심지역이며 배수가 양호한 화성암 지역에 주로 분포한 반면, 참나무류림은 사양토, 보통 이하의 얕은 토심지역이며 배수가 양호한 변성암 지역에 주로 분포하고 있는 것으로 나타났다. 이상과 같은 지리형태학적 인자에 따른 소나무림과 참나무류림의 공간분포 패턴을 회귀식으로 도출한 결과 통계적 유의성이 매우 높게 나타났다. 본 연구 결과는 지형, 기후, 토양 등의 환경 요소를 고려한 소나무림과 참나무류림 임분의 합리적인 관리에 기여할 것으로 기대된다.

• 대한원격탐사학회지
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• 제36권5_1호
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• pp.667-677
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• 2020

작물 수분 스트레스는 토양수분 함량, 농작물 생리학적 특성 및 원격탐사 기술을 이용하여 감지할 수 있으며, 작물의 생산량 감소를 평가하는데 매우 중요하다. 작물 수분 스트레스 지수(CWSI)는 작물의 엽온과 기온의 차이를 이용하여 산출할 수 있다. 본 연구에서는 드론 기반 열적외 영상을 이용하여 봄배추를 대상으로 관수 처리구(WCP)와 무관수 처리구(WDP)에 대한 CWSI 분포도를 작성하였다. 그 결과, CWSI 공간분포는 배추의 생육이상 반응 요소(구고, 구직경 및 엽록소 함량 측정치)와 높은 일치율을 나타내었다. 따라서 CWSI는 작물 생육이상 모니터링 및 평가에 좋은 수단으로 활용 가능할 것으로 판단된다.

• 한국태양광발전학회지
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• 제6권1호
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• pp.21-34
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• 2020

Sri Lanka has strongly understood the importance of mitigation of climate change and various measures have been taken. To tackle the climate change, after ratifying Paris Agreement, Sri Lanka has pledged to reduce her greenhouse gas emission in the energy sector by 20% (16% unconditional and 4% conditional) by 2030 based on the BAU scenario. Simultaneously, the government introduced its new energy policy and strategies in 2019 with a vision of achieving carbon neutrality by 2050. This paper survey related key government documents, policies, reports, and academic articles to investigate opportunities for the private sector to invest large scale solar power deployment (10 MW or above) and to get support from climate finance under article 6 of the Paris Agreement. It has found, growing concern on the environment, energy security issues and increase import expenses for fossil fuels are the main influencing factors to move renewable sources. Further, government investment and FDI both have gradually decreased in the energy sector. Therefore, an alternative financing mechanism is needed. Although the private sector allowed investing in the energy sector since 1996 with the introduction of IPP (Independent Power Producers), it could not make considerable progress on involving large scale solar utility projects. This has revealed government policy is not aligning with the long term generation plan of the electricity sector. The study has also found, it needs more strategic road map, coordination with different institutions, monitoring system to enhance large scale solar contribution.

• 한국환경복원기술학회지
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• 제25권2호
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• pp.39-53
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• 2022

The purpose of this study is to find out the applicability of LANDIS-II model to Korea. The case study was carried out in Daecheong Dam basin. In order to operate the model, a total of 63,107 cells of 100x100m unit were constructed, each cell consists of ecoregion map, initial communities map, plant physiological data, and climate change prediction data using SSP2-4.5 scenario. Forest distributions of year 2050 and 2100 were predicted by distribution intensity and interference among trees based on field surveys of 147 points in 2020. As a result, trees of decreased distribution area in the future are in the order of Quercus mongolica, Pinus rigida, Pinus densiflora and Robinia pseudoacacia, which characterized vulnerable to the effects of climate change or artificially planted trees. While warm climate trees of Quercus variabilis, Quercus serrata, Quercus acutissima and Quercus aliana are predicted to increase their distribution area in the order. These results analyzed using the LANDIS-II model are consistent with the studies on potential natural vegetation and succession tendency in Korea. In conclusion, the applicability of LANDIS-II model in Korea is highly effective and it is also expected to serve as a scientific basis for determining forest policies on afforestation and restoration.

• 한국환경복원기술학회지
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• 제20권3호
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• pp.1-18
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• 2017

This study constructed a high-resolution bioclimatic classification map of South Korea which classifies land into homogeneous zones by similar environment properties using advanced statistical techniques compared to existing ecological area classification studies. The climate data provided by WorldClim(1960-1990) were used to generate 27 bioclimatic variables affecting biological habitats, and key environmental variables were derived from Correlation Analysis and Principal Component Analysis. Clustering Analysis was performed using the ISODATA method to construct a 30'(~1km) resolution bioclimatic classification map. South Korea was divided into 21 regions and the results of classification were verified by correlation analysis with the Gross Primary Production(GPP), Actual Vegetation map made by the Ministry of Environment. Each zones' were described and named by its environmental characteristics and major vegetation distribution. This study could provide useful spatial frameworks to support ecosystem research, monitoring and policy decisions.

• 한국기후변화학회지
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• 제9권3호
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• pp.209-221
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• 2018

The characteristics of heat wave events in Seoul are analyzed using weather station data from Korea Meteorological Administration (KMA) and European Centre for Medium-Range Weather Forecast (ECMWF) ERA-Interim reanalysis data from 1979 to 2016. Heat waves are defined as events in the upper 10th percentile of the daily maximum temperatures. The associated synoptic weather patterns are then classified into six clusters through Self-Organizing Map (SOM) analysis for sea-level pressure anomalies in East Asia. Cluster 1 shows an anti-cyclonic circulation and weak troughs in southeast and west of Korea, respectively. This synoptic pattern leads to southeasterly winds that advect warm and moist air to the Korean Peninsula. Both clusters 2 and 3 are associated with southerly winds formed by an anti-cyclonic circulation over the east of Korea and cyclonic circulation over the west of Korea. Cluster 4 shows a stagnant weather pattern with weak winds and strong insolation. Clusters 5 and 6 are associated with F?hn wind resulting from an anti-cyclonic circulation in the north of the Korean Peninsula. In terms of long-term variations, event frequencies of clusters 4 and 5 show increasing and decreasing trends, respectively. However, other clusters do not show any long-term trends, indicating that the mechanisms that drive heat wave events in Seoul have remained constant over the last four decades.

• 동굴
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• 제68호
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• pp.75-98
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• 2005

Korea physiographic province is divided into two provinces which is northern Chugaryung graben zone and southern Chugraryung graben zone. Northern Chugraryung is also divided in to Gema block and Kohan block, and southern Chugraryung dividedinto Han block, Yongnam basin and Honam plain. The above mentioned macro geomorophic units is divided, mainly on the geotectonics. The meso geomorphic units is divided, based upon the regional distribution of topographic characteristic that is plateaus, mountains, mountain range, basins and great plain etc. Micro geomorphic units id into a mountain, a hill, a plain, and a lowland, and then it is formed by selfreliant topographic unit. And micro topographic (fan, peneplain, delta, etc) dealt with a characteristics unit. In this article has a disregarded amallest scale that is included flood plait natural levee, back marsh and oxbow lake etc. Accordingly, it shows macro units are meso units are 5, meso units are 53, micro units are 299. A study method of physiographic provincs prefered to aufsteigende and abstergands methoy. How to organically combine topographic factors can be seen in regional distribution of the peculiar topographic characteristics, for charage teristic of topographic makes a study on the topographic of micro unit such understanding as aufsteigende method. At the same time, since it can be studied systematically from marco unit to micro unit like the absteigende methods, I used both methods. And this establishment of physiographic province based on the scientific method depend on the base map of climate classification. Geology, Soil, Biology. I feel confident that it will be used the basic map for land use map, land classification map, study of geomorphology of Korea. And will be used for study of a topographic standard data.

• 한국기후변화학회지
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• 제7권4호
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• pp.451-463
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• 2016

We explore the impact of Chinese future air pollutant emissions on ozone air quality in Northeast Asia (NEA) and health in South-Korea using an assessment framework including ICAMS (The Integrated Climate and Air Quality Modeling System) and BenMAP (The Environmental Benefits Mapping and Analysis Program). The emissions data sets from the climate change scenarios, the Representative Concentration Pathways (RCPs) (emission scenarios, EMSO), are used to simulate ozone air quality in NEA in the current (1996~2005, 2000s), the near future (2016~2025, 2020s) and the distant future (2046~2055, 2050s). Furthermore, the simulated ozone changes in the 2050s are used to analyze ozone-related premature mortality and economic cost in South-Korea. While different EMSOs are applied to the China region, fixed EMSO are used for other country regions to isolate the impacts of the Chinese emissions. Predicted ozone changes in NEA are distinctively affected by large changes in NOx emission over most of China region. Comparing the 2020s with the 2000s situation, the largest increase in mean ozone concentrations in NEA is simulated under RCP 8.5 and similarly small increases are under other RCPs. In the 2050s in NEA, the largest increase in mean ozone concentrations is simulated under RCP 6.0 and leads to the occurrence of the highest premature mortalities and economic costs in South-Korea. Whereas, the largest decrease is simulated under RCP 4.5 leads to the highest avoided premature mortality numbers and economic costs. Our results suggest that continuous reduction of NOx emissions across the China region under an assertive climate change mitigation scenario like RCP 4.5 leads to improved future ozone air quality and health benefits in the NEA countries including South-Korea.

• 농촌계획
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• 제16권4호
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• pp.109-116
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• 2010

Climate change is known to affect both natural and managed ecosystems, and will likely impact on the terrestrail carbon balance. This paper reports the effects of climate change on spatial-temporal changes in carbon reductions in South Korea's during 2000-2100. Future carbon (C) stock distributions are simulated for the same period using various spatial data sets including land cover, net primary production(NPP) and leaf area index (LAI) obtained from MODIS(Moderate Resolution Imaging Spectroradiometer), and climate data from Data Assimilation Office(DAO) and Korea Meteorological Administration(KMA). This study attempts to predict future NPP using multiple linear regression and to model dependence of soil respiration on soil temperature. Plants store large amounts of carbon during the growing periods. During 2030-2100, Carbon accumulation in vegetation was increased to $566{\sim}610gC/m^2$/year owing to climate change. On the other hand, soil respiration is a key ecosystem process that releases carbon from the soil in the form of carbon dioxide. The estimated soil respiration spatially ranged from $49gC/m^2$/year to $231gC/m^2$/year in the year of 2010, and correlating well with the reference value. This results include Spatial-Temporal C reduction variation caused by climate change. Therefore this results is more comprehensive than previous results. The uncertainty in this study is still large, but it can be reduced if a detailed map becomes available.