• 설비공학논문집
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• 제16권12호
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• pp.1190-1196
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• 2004

Significant air temperature increases in urban areas are known as the heat island phenomenon in a global scale. Therefore, we propose numerical model in order to analyze quantitative effects of building environmental factors on the heat island phenomenon in urban area. In this paper, we propose a predicting model to analyze the heat island phenomenon quantitatively. Using this model, numerical simulation is performed in order to analyze quantitative effects of many factor on the heat island phenomenon.

• 한국지하수토양환경학회지:지하수토양환경
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• 제17권2호
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• pp.62-70
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• 2012

Rainfall, on Jeju Island varies regionally in relation to Mt. Halla with higher rainfall within southern area and lower in western area, and its variability is expected to expand according to the climate change scenario. Non-parametric trend analysis for rainfall, using both historic (1971-2010) and simulated (2011-2100) data assuming the A1B emissions scenario, shows regionally increasing trends with time. In perspective of agricultural land use, area for market garden including various crop types with high water demand is increasing over the Island, especially in the western area with lower rainfall compared to southern area. On the other hand, area for fruit including mandarin and kiwi with low water demand is widely distributed over southern and northern part having higher rainfall. These regional disparity of water demand/supply may be more affected by extreme events such as drought and heavy rainfall that has not yet been considered. Therefore, it is necessary to make policies for water resource management considering both demand and supply in different regions with climate change impacts over Jeju Island.

• 한국수산과학회지
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• 제37권2호
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• pp.148-158
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• 2004

In the adjacent seas of Cheju Island, the oceanographic conditions show low salinity surface waters starting in May. This water flows from the southeast part of the China Coastal Water, which flows southeastward along the Great Yangtze Sand Bank until April, with the help of southeasterly winds and flows from the adjacent sea off Cheju Island. In May, the Tsushima Warm Current and the low salinity surface water fluctuate in short and long-term periods as influenced by Yellow Sea Cold Water, which flows to the bottom layer at the western entrance of Cheju Strait. Temperature and salinity fronts in the northeastern sea area of U Island are formed in the boundary area between the Tsushima Warm Current, which expands towards Cheju Island from the southeastern sea area of Cheju Island and Hows out from the eastern entrance of the strait. Seasonally, additional oceanographic conditions, such as coastal counter-currents, which flow southward, appears within limited areas in the adjacent eastern and western seas of Cheju Island.

• 환경영향평가
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• 제26권5호
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• pp.315-330
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• 2017

본 연구는 도서지역에 침입한 굴토끼(Oryctolagus cuniculus)의 서식양상과 섭식 영향을 밝혀 효과적인 관리에 필요한 기초자료를 제공하고자 수행되었다. 조사 대상지인 범섬과 까막섬은 도입식물의 식재, 답압, 경작활동 등 인위적 간섭에 의해 교란된 이차식생 유형이다. 범섬에 정착한 굴토끼는 벌채지를 중심으로 높은 흔적밀도를 보였고, 까막섬에 정착한 굴토끼는 낙엽활엽수림대를 중심으로 높은 흔적밀도를 나타내었다. 조사지역에서 확인된 굴토끼 섭식 가해 식물은 총 12과 17분류군으로 확인되었다. 범섬에서는 총 9과 11분류군의 섭식 가해 식물이 확인되었고, 먹이 가용 식물이 대부분 소실된 까막섬에서는 총 5과 6분류군의 섭식 가해 식물이 확인되었다. 범섬의 식생지수는 도서 전체 면적의 약 6.6% 감소하였고, 까막섬의 식생지수는 전체 도서지역에서 감소하였다. 까막섬은 Enhanced Vegetation Index가 -0.008unit/yr 이상 감소하는 지역이 전체의 5.2%였으며, -0.008~-0.006unit/yr으로 감소하는 지역은 전체의 13.32%로 확인되어 심각한 식생 교란과 생물다양성 손실이 예상되므로 도서생태계의 보전과 복원을 위한 즉각적인 관리가 필요하다.

• 환경생물
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• 제18권2호
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• pp.237-246
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• 2000

섬 생물지리학에서 평형설(equilibrium theory)은 섬의 면적과 본토에서 떨어진 거리에 따른 이입율과 절멸율의 작용에 의해 섬에 분포하고 있는 종 수가 결정된다는 이론이다. 본 연구는 한반도 부속도서에서 여러 생태학적인 요인들인 섬의 면적, 격리정도, 위도 및 섬의 최고 고도로 표시한 서식지 다양성과 나비의 종 수에 관한 상관관계를 파악하기 위하여 71개의 섬에서 기록된 나비의 종 수와 이들 요인들 사이의 상관분석 및 회귀분석을 실시하였다. 그 결과 나비 종 수는 섬 면적($r^2$=0.405, P<0.005) 및 고도로 표시한 서식지 다양성($r^2$=0.341, P<0.005)과는 유의한 상관관계를 보였으나 본토와의 거리 ($r^2$=0.018, P>0.05)및 섬 위도($r^2$=0.040, P>0.05)와는 유의한 상관관계를 나타내지 않았다. 본 연구와 이전의 연구결과를 종합해보면 한반도 부속도서의 나비 종 수는 섬의 면적, 식생 그리고 최고 고도와 같은 생태적 변수에 영향을 받는 것으로 요약된다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 1992년도 가을학술발표회 논문집
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• pp.107-112
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• 1992

Housing lots and area for industrial construction are very serious problem because of narrow country area and high population density of Korea. Especially the form of Pusan is long from north to south. Since the city is surrounded by the sea, traffic trouble and housing lots problem is very serious condition. To solve these problems, Reclamation & Man-made island is needed. So Pusan city is planning for Man-made Island for 2000 year. I will consider about the content of Man-made Island, which is planned by Pusan, and the character of Geotechnical Engineering.

• 한국환경과학회지
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• 제6권4호
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• pp.303-311
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• 1997

The characteristics of spring machanism In the Cheju Island were analyzed by statistical techniques. Basic characteristics, areal and altitudinal variations, and correlations of spring data were investigated. In this study. however, the subjects of the study are the 451 springs, the whole basin of Cheju Island derided Into four groups. In this study, analyzed the spring phenomena on the basis of both the geologic elements and the topogaphic elements. Also, the spring zone In Cheju Island are classified Into three types that the mountain area, the muddle area, the coastal area in spring distribution by attitude. The quentity of spring and variability show subvariety on the average according to Meinzer's classilfication and the whole basin of spring shows various distributions from Third to Sixth. The results of this study can be utilized to evaluate the condition of groundwater development In Cheju Island.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2019년도 학술발표회
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• pp.218-218
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• 2019

Jeju island has an area of $1,810km^2$ and is considered the largest island in South Korea. In Jeju Island the average annual precipitation is 1,957mm. About 54% of precipitation is estimated to be lost due to evapo-transpiration and direct runoff, and the remainder is recharged. Historically springs and puddles were the island's primary sources of water. However, after 1970 all sectors, including the urban and industrial sectors depended solely on groundwater as their water resource. As vast amount of water is being recharged the Island has many springs, especially near the coastlines. Historlcally, spring of Jeju Island formed village and make it possible to continue a life. Also it produces many values such as the spring related story, culture, tourism and ecosystems. Especially, the naturally rare phenomenon that about 900 springs appear over the whole area of Jeju Island makes it possible to call it as a natural heritage. As a result of this most springs have either been destroyed or been in the state of neglect. In some cases it has been observed that springs were preserved by nature, however majority of the cases saw springs losing their own nature as a result of abandonment. It was recorded that there were 911 springs in Jeju Island with most of them being distributed along the coast, which consequently increases their susceptibility to seawater intrusion. The objective of this study is therefore to analyze Eco-cultural and Engineering characteristics about springs in the island, highlighting its past utilization and reestablishing its potential as a source of spring.

• 한국측량학회지
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• 제36권4호
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• pp.305-316
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• 2018

우리나라의 도시화 비율이 증가함에 따라 도시열섬으로 인한 도시 열 환경의 중요성이 증대되고 있다. 본 연구에서는 2012년에 출범하여 급속도로 발전을 이룬 세종특별자치시의 도시 열 환경 분석을 위해 열섬포텐셜을 이용하였다. 우선 도심지의 비율 및 변화율을 분석하기 위해 Landsat-8 OLI/TIRS 위성영상을 기반으로 연구지역의 시계열 토지피복도(2013년~2015년, 2017년)를 생성하였다. 그리고 취득된 위성영상에서 제공하는 두 가지 열적외선 밴드에서 산출된 밝기온도와 자동기상관측망 자료와의 정확도 평가를 통해 연구에 활용할 밴드를 선정하였다. 선정된 밴드와 지표면 방사율을 고려하여 지표면온도를 산출하였으며, 이를 기반으로 산출된 열섬포텐셜 변화분석을 수행하였다. 분석결과, 연구지역의 행정구역별 도심지 변화율이 크게 관측되는 지역의 지표면온도는 주변지역 보다 $3^{\circ}C{\sim}4^{\circ}C$ 높고, 열섬포텐셜 또한 $4^{\circ}C{\sim}5^{\circ}C$ 높게 관측되었다. 하지만 도심지 변화율이 크고 녹지의 비율이 높은 지역에서는 열섬현상이 완화되는 경향을 보였다. 이를 통해 면적대비 도심지가 차지하는 비율이 높아지면 열섬을 유발할 가능성이 증가하지만 녹지를 통해 열섬을 완화 시킬 수 있다는 것을 알 수 있었다.

• 한국지하수토양환경학회:학술대회논문집
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• 한국지하수토양환경학회 1997년도 추계 국제학술심포지움 논문집
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• pp.97-142
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• 1997

The Seoguipo Formation occurs only in a small exposure along the coast of the Seoguipo City, but in the subsurface, underlies tile western part of the Bugcheon-Pyoseon Line in the northeastern part of tile island. The Bugcheon-Pyoseon Line is presumed to be a facies boundary that reflects tile distribution of hyaloclastites resulted from submarine volcanic activity. The Seoguipo Formation is distributed in the subsurface along the part which is lower than 400m in average altitude, and occurs at El. -5.76∼-46.63m in tile southern area, El. -41.89∼-57.97m in the western area, El. -13.15∼-50.59m in the northern area. Therefore, the southern area was uplifted after the deposition of the Seoguipo Formation. In the subsurface, the vertical depth of the volcanic rocks of the Cheju Volcanic Edifice is El. -40.6m in the southern area, El. -111.3m in the western area, El. -81.5m in the northern area and El. -134.7m in the eastern area. The unconsolidated U Formation, which is, overlying the basement and about 70∼250m thickness underlies the whole island. There is a positive correlation between tile groundwater level and the depth of the subsurface distribution of the Seoguipo Formation. Consequently, it is conformed that the subsurface distribution of the Seoguipo Formation plays important role for controlling the characteristics of the reservoir of tile groundwater in Cheju Island.