• Proceedings of the Korea Committee for Ocean Resources and Engineering Conference
• /
• 2006.11a
• /
• pp.473-476
• /
• 2006

천해역의 파랑발달에 대한 태풍경로의 영향력을 분석 하였다. 우리나라 남동해안에 주로 피해를 초래할 것으로 판단되는 태풍의 경로를 '남해안 상륙 후 내륙 통과'와 '대한해협통과'로 분류하고 각 경로에 따른 태풍규모와 파랑발달을 1956년 부터 2004년까지의 기상자료를 바탕으로 검토하였다. 태풍 경로의 영향력 분석은 천해역 파랑발달의 주요외력이 지형조건에 의해 결정되므로(즉, 폐쇄해역은 태풍의 바람장이 주요외력이며, 개방해역은 심해 전달파랑과 바람장의 영향을 동시에 받는다), 개방해역과 폐쇄해역의 경우로 나누어 수치모형실험을 통해 수행하였다. 실험조건은 태풍 "매미"의 강도와 특성 값을 기준으로 하였으며, 대상해역은 부산신항 인근해역과 원전항 인근해역을 개방형과 폐쇄형 해역으로 대별하여 실험을 수행하였다. 자료의 분석결과 최근 이상기후현상으로 태풍의 강도가 커지고 있음을 뒷받침 하는 근거는 찾아보기 힘들었으며, 2000년대 이후로 남해안에 상륙하는 경로'1'이 대한해협을 통과하는 경로(경로'2')보다 그 내습빈도가 커지고 있음을 볼 수 있었다. 태풍의 경로와 풍향이 같은 방향인 경로'1'일 때 에너지가 집중되어 태풍중심기압과 풍속과 파고의 증가가 함께 일어난다. 그러나 태풍의 경로와 풍속의 방향이 일치하지 않는 경로'2'의 경우는 에너지가 분산되므로 태풍중심기압과 풍속은 함께 증가하나 파랑에너지는 함께 발달하지 않는 것으로 보였다. 내습한 태풍의 강도를 경로별로 비교한 결과, 경로'1'이 경로'2'보다 큰 강도를 가지고 연악역에 영향을 미치는 것으로 판단되었다.

• Journal of the Korean Association of Geographic Information Studies
• /
• v.16 no.1
• /
• pp.59-66
• /
• 2013

When the typhoons are passing over the ocean, the ocean environment has both physical and biological impacts on the East, South sea and Yellow sea of Korea. As a result of typhoon path, vertical mixing and upwelling injured colder subsurface water, and leaded to phytoplankton blooming along the typhoons. The ocean environment before and after a typhoon played an important role in the biological effect of sea surface. Although the magnitude of sea surface temperature (SST) gets cooler because of typhoon path, other physical and biophysical responses are quite different such as chlorophyll, K490 and SST. The purpose of this study is to compare with the typhoon path that influenced the Korean Peninsula and ocean environment parameters which were observed by ocean color remotely-sensed data. The MODIS data were used to assess the parameters of ocean environments such as K490 and chlorophyll data from 2002 to 2005. Mean chlorophyll from MODIS data increased by about 1-4% in the East sea after the typhoon. Mean concentration of MODIS chlorophyll in the post-typhoon period increased along the typhoon passage. However, Jeju coastal area has different patterns from those of the East sea.

• Journal of the Korean Association of Geographic Information Studies
• /
• v.22 no.1
• /
• pp.93-102
• /
• 2019

In this study, in order to analyze the possibility of observing a typhoon track based on the Global Navigation Satellite System(GNSS), Typhoon NARI, the 11th typhoon of 2007, was analyzed in terms of the typhoon track as well as the local variation of perceptible water over time. The perceptible water was estimated using data obtained from observatories located on the typhoon track from Jeju to the southern coast of Korea for a total of 18 days from September 7(DOY 250) to September 24(DOY 267), 2007, including the period when the observatories were affected by the typhoon at full-scale, as well as one previous week and one following week. The results show that the trend of the variation of perceptible water was similar between the observatories near the typhoon track. Variation of perceptible water over time depending on the development and landing of the typhoon was distinctively observed. Several hours after the daily maximum of perceptible water was found at the JEJU Observatory, the first struck by the typhoon on the typhoon track, the maximum value was found at other observatories located on the southern coast. In the observation period, the time point at which the maximum perceptible water was recorded in each location was almost the same as the time point at which the typhoon landed at the location. To analyze the accuracy of the GNSS-based perceptible water measurement, the data were compared with radiosonde-based perceptible water data. The mean error was 0.0cm, and the root mean square error and the standard deviation were both 0.3cm, indicating that the GNSS-based perceptible water data were highly accurate and precise. The results of the this study show that the GNSS-based perceptible water data may be used as highly accurate information for the analysis of typhoon tracks over time.

• Proceedings of the Korean Institute of Navigation and Port Research Conference
• /
• 2010.04a
• /
• pp.238-239
• /
• 2010

근래, 이산화탄소로 대표되는 온실효과 기체의 증가에 동반하여 대류권의 기온이 정정 상승하는 지구 온난화의 경향이 나타나고 있다. 지구 온난화가 지속되면 해수면온도가 상승하고 그에 따라 해빙 면적의 축소와 해수면 상승이 동반된다. 이와 같은 지구 온난화의 상황이 지속되면 이상기상이 지구상 각지에서 빈발할 것이라는 주장도 제기되고 있다. 이 연구에서는 장기간의 태풍 관련 데이터를 이용하여 지구 온난화와 관련한 태풍의 변화 경향을 분석하였다. 연구 결과 지구 온난화와 더불어 태풍의 발생 수는 감소하고 있으며, 태풍의 세기는 서서히 강화되고 있음을 확인하였다. 그리고 태풍의 이동경로 중에서 정상진로는 증가하는 경향을 보이고 서진형진로는 감소하는 추세를 보이고 있다는 사실을 알았다. 우리나라의 경우는 최근에 들어 통해(또는 일본)를 통과하면서 영향을 미치는 태풍의 수가 증가하는 반면 서해를 통과하는 태풍의 수는 감소하는 경향을 보인다. 그리고 우리나라에 가장 큰 기상재해를 입히는 남해를 통과하는 태풍의 수는 시계열 상 큰 변화를 보이지 않는다.

• Proceedings of the Korea Water Resources Association Conference
• /
• 2008.05a
• /
• pp.304-309
• /
• 2008

기존의 태풍예측과 관련된 연구들은 전 지구적인 흐름이 직접적으로 계산되지 않은 중규모 기상모형이나 태풍모형들을 이용하여왔다. 하지만 최근 전 세계적으로 전구 규모의 모형들이 40km 이하의 고해상도 모형들이 개발되어 20km이하의 초고해상도 시물레이션이 가능해짐에 따라 지역적인 기상현상들을 전구모형을 통해서 재현해 내고 있다. 따라서 본 연구에서는 고해상도 전구모형을 이용하여 태풍 실험을 하고자 하며, 독일기상청에서 개발된 Icosahedral-hexagonal 격자체계의 GME전구 모형을 이용한 태풍모의 결과를 기상청 태풍 best track과 비교 분석 하였다. 실험에 사용된 모형 분해능은 연직 47layer (7 soil layer 포함), 수평 약 40km와 20km으로 구성되었다. 최근 3년($2005{\sim}2007$)간의 동아시아지역을 지나간 태풍을 대상으로 하였다. 태풍모의 시작시간은 각 TD(Tropical Depression)발생 24시간 전 자료를 이용하였으며, 각 태풍의 소멸 24시간 후까지 모의하였다. GME 모형을 이용한 태풍모의 결과에서 best track의 경우 모의 시작 후 약 168시간 forcast 결과가 매우 유사한 경로를 따라 진행해 가고 있으며, 태풍의 전향이 이루어지는 시각은 ${\pm}3$시간 내외의 오차를 보이고 있다. 태풍경로의 경우 40km 결과에 비해 20km 모의 결과가 best track에 더 가까운 결과를 보이고 있다. 중심기압변화의 경우 40km의 결과가 20km 결과에 비해 변화경향이 유사한 형태를 보이고 있으며, 20km 결과의 경우 중심기압의 변화가 다소 급하게 나타나는 경향을 보이는 특성을 가지고 있지만 40km결과에 비해 최저 중심기압이 더욱 뚜렷하게 나타나고 있으며 특히, MANYI case의 경우 관측값 930hPa보다 더 낮은 911.4hPa의 결과를 보이고 있다. 풍속의 경우도 중심기압변화와 유사한 결과를 보이고 있으나, 최대 풍속의 경우 40km 결과에 비해 20km결과가 관측과의 오차범위가 $2{\sim}3\;m/s$ 내외로 나타나고 있다. 그리고 GME모형의 경우 태풍(TD) 발생 약168시간 이전에 예측이 가능한 결과를 보인다. 이 연구의 결과는 다른 기상모형에서 태풍 강도가 약하게 모의되던 현상이 상당히 개선된 것을 알 수 있으며, 이는 20km 고해상도 GME 모형이 태풍예측모형으로 활용이 간능 할 것으로 사료 된다.

• Journal of Korea Water Resources Association
• /
• v.50 no.4
• /
• pp.233-239
• /
• 2017

In this study, we analyzed typhoon affecting Korean Peninsula and runoff characteristic changes according to the typhoon based on Sumjin river dam, a representative multi-purpose dam. We quantified typhoon flow by applying the typhoon domain, and will provide base data for climate change adaptation and counterstrategy through correlation analysis of the change of typhoon statistical data and Indicators of Hydrologic Alterations (IHA). Korean Peninsula impact typhoon has a great effect on the scale of peak flow and the change of occurrence time. The occurrence frequency and duration of the peak flow were analyzed to be relatively unrelated to the typhoon affected by the Korean peninsula. These changes were also confirmed in the correlation analysis results. Correlation coefficient between the peak flow (0.41) and peak flow occurrence time (correlation coefficient = 0.83) was positively correlated with the Korean peninsula influenced typhoon.

• Journal of Korean Society of Coastal and Ocean Engineers
• /
• v.27 no.1
• /
• pp.25-37
• /
• 2015

Tide-surge interaction during typhoon periods has been analyzed. The quantitative analysis of the Chi-square test shows that the interaction is most prominent at the Southwestern coast whereas the Western and the Southeastern regions are not. Patterns of surge type were divided into two groups, that is, steep type and mild type. Then, the interaction was turned out to be more prominent for mild type data. The weak interaction at the Western region is considered due to negative surges when the south-track typhoons attack. However, the interaction is remarkable when the west-track typhoons attack. The weak interaction at the Southeastern coast is, on the other hand, considered due to abundance of the steep type typhoons. Thus, inundation risk would be so apprehensive at that region because large-scale surge might be caused even at high tide.

• Journal of Korea Water Resources Association
• /
• v.47 no.4
• /
• pp.385-396
• /
• 2014

Lately, more frequent typhoons cause extensive flood and wind damage throughout the summer season. In this respect, this study aims to develop a probabilistic clustering model that uses both typhoon genesis location and trajectories. The proposed model was applied to the 197 typhoon events that made landfall in the Korean peninsula from 1951 to 2012. We evaluate the performance of the proposed clustering model through a simulation study based on synthetic typhoon trajectories. The seven distinguished clusters for typhoons affecting Korean peninsula were identified. It was found that most of typhoon genesis originated from a remote position ($10^{\circ}{\sim}20^{\circ}N$, $120^{\circ}{\sim}150^{\circ}E$) near the Equator. Cluster, type B can be regarded as a major track due to the fact that its frequency is approximately about 25.4% out of 197 events and its direct association with strong positive rainfall anomalies.

• Journal of Korean Society of Coastal and Ocean Engineers
• /
• v.25 no.5
• /
• pp.291-300
• /
• 2013

Typhoon simulation method is widely used to estimate sea surface wind speeds during the typhoon periods. Holland (1980) model has been regarded to provide relatively better results for observed wind data. JTWC or RSMC best track data are available for typhoon modeling, but these data show slightly different because the data generation process are different. In this paper, a Newton-Raphson method is used to solve the two nonlinear equations based on the Holland model that is formed by the two typhoon parameters, i.e. the longest radius of 25 m/s and 15 m/s wind speeds, respectively. The solution is the radius of maximum wind speed which is of importance for typhoon modeling. This method is based on the typhoon wind profile of JMA and it shows that Holland model appears to fit better the characteristics of typhoons on the temporal and spatial changes than that of the other models. In case of using RSMC best track data, the method suggested in this study shows better and more reasonable results for the estimation of radius of maximum wind speed because the consistency of the input data is assured.

• Journal of Korean Society of Coastal and Ocean Engineers
• /
• v.21 no.1
• /
• pp.1-14
• /
• 2009

Linear-tracked typhoons were simulated to investigate the effect of parameter sensitivity at Gyeongnam coastal zone. To do this, appropriateness of the linear-tracked MAEMI(0314) was tested and 175 scenarios were simulated on the basis of virtual MAEMI. The results show surge heights are relatively large at Masan and Tongyeong, and it can be attributed to topographical effects. At Masan, 2.5 m-surge height is probable with the same intensity but slightly different track from the real typhoon MAEMI. At the other stations, surge heights induced by real MAEMI are nearly same as the maximum heights of the virtual typhoons, which indicates the real track of the typhoon MAEMI was almost the most severe one. Surge heights caused by the barometric effect are higher than those by the wind effect, and the former effect shows the maximum at the eye of typhoon.