• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume II
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• pp.918-921
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• 2006

The short-term variation of sea surface temperature before and after typhoons and increase of chlorophyll a concentration that accompany with the typhoons during summer in the East/Japan Sea were explored by satellite. Four typhoons (NAMTHEUN, MEGI, CHABA and SONGDA) and a typhoon (NABI) passed over the East/Japan Sea in 2004 and 2005, respectively. Decreasing of SST was observed in the every five typhoons, however the magnitude of SST decreasing were various from 1 to $5^{\circ}C$. Chlorophyll a increases were found after the typhoons (0.1-3 ${\mu}g$ $l^{-1})$ except NAMTHEUN, and the area was approximately included in SST decreasing area by the typhoons. It suggests that chlorophyll a increase was caused by nutrient input from subsurface layer by strong mixing. On the other hand, rarely chlorophyll a increase was observed in northern area of polar frontal zone, which is located in $38-41^{\circ}N$, than northern area, and chlorophyll a increase in coastal area was higher (more than 3 times) than offshore area. It might suggest that chlorophyll a increase in the East/Japan Sea is also related with the depth or nitracline depth that affects the amount of nutrients supply to the upper layer by typhoon mixing.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2003년도 Proceedings of ACRS 2003 ISRS
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• pp.718-719
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• 2003

It is very important to monitor change of a forest. We compare the different seasonal remote sensing data to detect forest damaged by typhoons and build a method to detect the area damaged by typhoons. Study site is located in western Oita prefecture. The multitemporal satellite dataset of this study were consisted of four Landsat TM scenes taken before and after the typhoons. As compared with non-damaged area, it was shown that the reflective characteristic of the damaged area becomes high by band 3, band 5, and band 7. These bands are effective in extracting the typhoon damaged area.

• 해양환경안전학회지
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• 제22권5호
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• pp.508-520
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• 2016

본 연구에서는 7년(2009-2015)간 한반도 주변을 통과한 태풍의 이동 경로에 따른 수온의 변동을 분석하였다. 자료는 위성관측 수온영상, 동해 연안의 양양, 강릉, 삼척, 영덕에서 실시간 계류부이에서 관측한 수온과 기상청에서 제공한 바람을 분석하였다. 위성 영상을 이용한 태풍 통과 전후의 근해 수온의 차이는 태풍의 이동 경로에 따른 바람의 방향뿐만 아니라 해면 가열과 해면 상승의 시기와도 관계가 깊게 나타났다. Muifa, Chanhom, Nakri, Tembin과 같은 태풍들의 오른쪽에 위치한 동해 연안의 수온은 남풍계열의 바람에 의한 연안용승으로 표층뿐만 아니라 15m, 25m의 수온까지 하강하는 것을 알았다. 특히, 태풍 Chanhom과 Tembin에 의한 수온의 하강은 각각 $8-11^{\circ}C$와 $16^{\circ}C$ 하강하였다. 한편 그 반대편에 태풍이 위치할 때는 외해쪽에 있는 고온의 해수를 연안쪽으로 이동하여 침강시킴으로서 중층과 저층의 수온이 상승하였다. 또한, 태풍 통과 이후에 동해 연안에서 남풍(북풍)계열의 바람에 의한 하강(상승)된 수온의 혼합은 1-2일 및 4일간 지속되었다.

• 한국지형학회지
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• 제28권4호
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• pp.1-13
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• 2021

In this study is aerial photos and UAV(Unmanned Aerial Vehicle) images were used to analyzed the characteristics of depositional landform changes in the Geum river channels before and after the opening gate of Gongju weir. Based on the depositional landform classification result, the main stream and the bare land occupied most of the area in all periods, and also found that the main stream, mid-channel island, and sand bar occupied a greater degree of area increase or decrease compared to other landforms in the classification items. As a result of analyzing the characteristics of depositional landform changes before and after the opening gate of Gongju weir, it is judged that the depositional landforms have changed due to the decreased water level of the Geum river after the opening of the weir, the summer rainy season and typhoons, river stabilization after the effluence of Daecheong dam, supply and deposition of river sediments and fixation of vegetation. The results derived from this study can be used as basic data for the study of river depositional landforms and the establishment of management and conservation plans for the landforms in river channels.

• 한국지반신소재학회논문집
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• 제23권1호
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• pp.49-60
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• 2024

최근 기후변화 등 달라진 해양 환경으로 인해 태풍 파랑의 빈도 및 강도가 증가하고 있다. 뿐만 아니라 일본, 칠레, 아이티, 중국, 인도네시아 등 세계적으로 잦은 지진으로 인해 많은 피해가 발생하고 있다. 우리나라 역시 2000년대에 들어서 태풍에 의한 피해가 증가하고 있으며, 지진의 발생 빈도와 강도도 증가하고 있다. 우리나라는 삼면이 바다로 되어있어 태풍에 의해 해안구조물에 많은 피해가 발생할 수 있으며 지진 역시 해안구조물에 많은 피해를 야기시킨다. 이처럼 국내·외적으로 태풍 파랑과 지진의 빈도 및 강도가 증가하는 추세이나 태풍과 지진을 연계한 연구는 전무하다. 따라서, 본 연구에서는 케이슨식 방파제에 태풍 파랑과 지진을 연계하여 총 4가지 Case에 대해 수치해석을 수행하였다. Case 1은 파랑하중, Case 2는 지진파를 각각 적용하였고, Case 3은 파랑하중 이후 지진 발생, Case 4는 지진파 이후 파랑하중까지 적용하여 수치해석을 수행하였다. 수치해석 결과 태풍과 지진을 연계한 Case 3과 Case 4의 경우 기존에 지반의 강도가 저하된 상태에서 하중을 적용하여 각 하중에 의한 피해가 Case 1과 Case 2에 비해 증가한 것을 확인하였다. 또한, 파랑하중 이후 지진파를 적용한 Case 3에서 피해가 가장 큰 것을 확인하였다.

• 한국지리정보학회지
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• 제16권1호
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• pp.59-66
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• 2013

태풍이 해양을 이동할 때 해양환경은 물리 생물학적으로 한반도 주변해역에 영향을 미친다. 태풍이동의 결과로써 해양의 수직적 혼합과 용승작용은 해양 표층수 냉각을 유도하고 태풍의 경로에 따라 식물플랑크톤의 증가를 초래하며, 태풍 전과 후의 해양환경은 해양표층의 생물학적 변화에 중요한 역할을 했다. 비록 태풍 이동의 원인으로 해양 표층수의 냉각이 확대되지만, 엽록소, K490, SST와 같은 다른 물리-생물리적 반응은 서로 다른 경향을 나타낸다. 본 연구의 목적은 한반도 주변해역에 영향을 미치는 태풍 이동경로와 해색센서에 의해 관측된 해양환경변수를 비교하는데 있다. 부유물질, 흡광계수(K490), 엽록소와 같은 해양환경변수는 2002년부터 2005년 MODIS 자료가 적용되었다. 태풍이동 후 동해에서는 평균 엽록소 농도가 1-4배 증가하였고, 태풍 이동경로를 따라 태풍 이후 MODIS 엽록소의 평균 농도가 증가하였다. 그러나 제주도 해역은 동해역과 반대의 경향을 나타내었다.

• Ocean and Polar Research
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• 제43권4호
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• pp.205-217
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• 2021

A shallow channel between Jeju and Udo Islands, which is located in the northeastern Jeju Island, is influenced by storm- or typhoon-induced currents and surface waves as well as strong tidal currents. This study examines the typhoon-induced current and wave patterns in the channel, using Acoustic Doppler Current Meter (ADCP) measurements and an ocean-wave coupled modeling experiment. Three typhoons were chosen - Chaba (2016), Soulik (2018), and Lingling (2019) - to investigate the responses of currents and waves in their pathways. During the pre-typhoon periods, dominant northward flow and wave propagation were observed in the channel due to the southeasterly winds before the three typhoons. After the passage of Chaba, which passed over the eastern side of Jeju Island, the northward flow and wave propagation were totally reversed to the opposite direction, which was attributed to the strong northerly winds on the left side of the typhoon. In contrast, in the cases of Soulik and Lingling, which passed over the western side of Jeju Island, strong southerly winds on the right side of the typhoons continuously intensified the northward current and wave propagation in the channel. The model-simulated current and wave fields reasonably coincided with observational data, showing southward/northward flow and wave propagation in response to the right/left side of the typhoon pathways. Typhoon-induced downwind flows, and surface waves could enhance up to 2m/s and 3m due to the strong winds that lasted for more than 12 hours. This suggests that the flow and wave patterns in the Udo channel are highly sensitive to the pathway of typhoons and accompanying winds; thus, this may be a crucial factor with regard to the movement of seabed sediments and subsequent coastal erosion.

• 한국지형학회지
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• 제28권4호
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• pp.15-30
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• 2021

This study analyzed the changes in land-cover and sedimentary environment before and after flooding through drone images and sediment analysis for the Seomjin River Chimsil Wetland. The results showed that the area of some land-covers such as sand bar, grass, and trees were continuously changed. The acidity level of the sediments in the Seomjin River Chimsil Wetland was weakened gradually by flooding and EC was also decreased. The levels of organic matter, effective phosphoric acid, and CEC, however, were fluctuating depending on branches, which seems to be the result of landization as new sedimentary environment was developed and vegetation was settled after the flood. Average mean size of river sediments was found to be fine sand, and it exhibited various particle size characteristics from granule to medium silt depending on the location. As the sedimentary environment changed due to the effects of floods and typhoons, the particles were granulated or grain refined depending on the position. In the Seomjin River Chimsil Wetland, there were factors that could interfere with geomorphic development and sedimentary environment, contamination sources in and around the wetland, and natural threat factors. Therefore, in this study, a conservation and management plan was proposed to remove these threat factors and to preserve the scarcity, naturalness, and dynamics of Seomjin River Chimsil Wetland.

• 한국지리정보학회지
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• 제20권1호
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• pp.85-97
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• 2017

최근 전 세계적으로 지구온난화, 기후변화 등으로 태풍, 지진해일, 폭염 및 폭설 등과 같은 수재해의 피해가 대규모로 확대되었다. 특히 태풍으로 인한 경제적 손실은 1960년대 이후 경제개발 및 도시화로 인한 인구과밀지역에서 크게 나타나고 있다. 본 연구에서는 2016년 한반도를 강타한 태풍 차바를 비롯하여 태풍 루사('02), 태풍 매미('03) 및 태풍 볼라벤('12)에 대하여 한반도 내습 전 후 촬영된 위성 현황에 대하여 조사 및 분석을 실시한 결과, 기존 위성을 활용함에 있어 한계를 느끼게 되었다. 국내 위성은 주로 기상, 해양, 지형 및 통신 등의 목적으로 개발 운영됨으로 물 관리 및 수재해 대응에 필요한 시 공간적 데이터 관측 정보가 많이 부족하였다. 때문에 국외 위성으로 범위를 넓혀 조사를 실시하였으며, 이에 GMS, TRMM, COMS 및 GPM 등의 위성 자료를 수집하였다. 향후 한반도에 빠르고 정확한 수재해 정보를 얻기 위하여 시 공간적 데이터 분석단위를 만족시키는 수자원 위성의 개발 및 적용이 필요하다.

• 한국대기환경학회지
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• 제30권2호
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• pp.128-138
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• 2014

This study has analyzed the concentration variation of four air pollutants ($PM_{10}$, $NO_2$, CO, and $SO_2$) during the typhoon periods over 10 years (2002~2011). In this study, 10 typhoon events which had rainfalls in Korean Peninsula were selected during the study period. The analysis was performed using the observation data of both the air pollutants and rainfall. In order to examine and compare the concentrations of the air pollutants between normal periods and typhoon periods, we have obtained monthly average concentrations from July to September and daily average concentrations during typhoon periods. For the period from July to September, 34% of the total rainfalls can be explained by typhoons, and the concentration of air pollutants during the typhoon period was lower than the normal period. In addition, the concentration variations of the pollutants during the typhoon period were analyzed according to two categories: differences in the concentrations between the day before and the day of the typhoon (Case 1) and between the day before and after the typhoon (Case 2). The results indicated that the reduction rate of $PM_{10}$, $NO_2$, CO, and $SO_2$ was 30.1%, 17.9%, 11.6%, 9.7% (Case 1) and 22.8%, 21.0%, 9.0%, 8.0% (Case 2), respectively. This result suggested that air quality was significantly improved during the typhoon period than after the typhoon period by the rainfall.