• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2016년도 학술발표회
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• pp.202-202
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• 2016

Despite the potentially major influence of rainstorm patterns on the prediction of shallow landslides, this relationship has not yet received significant attention. In this study, five typical temporal rainstorm patterns with the same cumulative amount and intensity components comprising Advanced (A1 and A2), Centralized (C), and Delayed (D1 and D2) were designed based on a historical rainstorm event occurred in 2006 in Mt. Jinbu area. The patterns were incorporated as the hydrological conditions into the Transient Rainfall Infiltration and Grid-based Regional Slope-stability Model (TRIGRS), in order to assess their influences on pore pressure variation and changes in the stability of the covering soil layer in the study area. The results revealed that not only the cumulative rainfall thresholds necessary to initiate landslides, but also the rate at which the factor of safety (FS) decreases and the time required to reach the critical state, are governed by rainstorm pattern. The sooner the peak rainfall intensity occurs, the smaller the cumulative rainfall threshold, and the shorter the time until landslide occurrence. Left-skewed rainfall patterns were found to have a greater effect on landslide initiation. More specifically, among the five different patterns, the Advanced storm pattern (A1) produced the most critical state, as it resulted in the highest pore pressure across the entire area for the shortest duration; the severity of response was then followed by patterns A2, C, D1, and D2. Thus, it can be concluded that rainfall patterns have a significant effect on the cumulative rainfall threshold, the build-up of pore pressure, and the occurrence of shallow landslides, both in space and time.

• 한국측량학회:학술대회논문집
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• 한국측량학회 2006년도 춘계학술발표회 논문집
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• pp.313-318
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• 2006

The main cause of natural disaster in Korea is meteorological phenomenon, such as typhoon, heavy rain, storm, rainstorm, heavy snow, hailstorm, overflowing of sea and so on(including thunderstroke, blast, snow damage, freezing and earthquake), and among those disasters, heavy rain takes place most often, and it occupies 80% of total disaster Especially, disaster related to slope collapse (landslide, collapse of retaining wall, burying ect.) takes place every year due to meteorological cause such as localized heavy rain, which is getting stronger. (National Institute for Prevention Disaster, 2002, Meteorological Administration) Accordingly, it is necessary to analyze the features of slope collapse related to natural disaster in Korea, and also to make up counterplan to prevent disaster. This paper will try to analyze potential areas which are susceptible to landslide regarding factors inducing landslide and heavy rain, and to evaluate the potentiality of landslide regarding local particularity of rainfall, furthermore to provide essential information for development of community such as preventing damages from landslide, construction Industry, and effective use of land.

• 디지털융복합연구
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• 제16권7호
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• pp.47-54
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• 2018

최근 우리나라는 토사재해로 인하여 해마다 많은 인명과 재산피해가 발생하고 있다. 비교법적으로 검토해 보면, 일본 히로시마에서는 1999년에 폭우로 인한 토사재해로 엄청난 피해가 발생하였는데, 이후 제정된 토사재해방지법에 근거하여 도도부현에 토사 재해 방지를 위한 비 구조 대책이 도입되었다. 여기에는 토사재해 경보, 대피 표준 강우량 제정, 토사재해 경계 구역 지정 및 토사재해 특별 경계 구역 지정 등이 포함되어 있다. 또한 구체적인 실제 적용례로서, 일본 가고시마현의 토사재해경계정보시스템과 전문 인력 활용방안인 일본 국토교통성의 TEC-FORCE사례를 중점적으로 살펴보았다. 향후, 일본과 같은 토사재해경계시스템과 전문 인력을 활용한 피해예방 및 피해저감 대책이 절대적으로 필요하다고 할 것이다.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2005년도 춘계 학술발표회 논문집
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• pp.781-787
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• 2005

Recently, disaster that is earthquake, sever rainstorm and the tidal wave were increased by abnormal weather. These influence which is the slope stability of the completed slope as well as under construction slope is affected by disaster. But the management standard for the construction slope is incomplete. Also, the standard connected with construction slope is not integrated with the important public paper organic enemy and it is duplicated and the standards which conflict are being scattered. In this research which it sees consequently the inside and outside of the country construction slope the maintenance civil official relation law and standard investigation it leads and the problem point and a improvement program of management criterion and to sleep the construction slope which is suitable in domestic actuality it prepares and propose.

• 한국산림과학회지
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• 제78권2호
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• pp.228-241
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• 1989

1987년(年) 7월(月) 21일(日)에서 23일(日)까지 3일간(日間) 우리나라 중부지방(中部地方)에서 호우재해(豪雨災害)가 막심(莫甚)하였는데, 그중에서 충남(忠南) 부여(扶餘), 서천(舒川), 공주(公州), 보령(保寧), 청야지방(靑陽地方)에서 산사태(山沙汰)-토석유(土石流) 재해(災害)로 인명피해(人命被害)가 큰 곳을 조사(調査)하여 산사태재해(山沙汰災害)의 특성(特性)을 분석(分析)하고 또 재해대책면(災害對策面)에서의 예방대책(豫防對策)을 수립(樹立)함에 필요(必要)한 자료(資料)를 도출해 보고저 이 연구(硏究)를 수행하였다. 인명피해(人命被害)가 발생(發生)한 산사태(山沙汰)는 주로 7월(月)22일(日) 아침 6~8시 사이에 많이 발생(發生)되었는데, 그 주원인(主原因)은 집중호우(集中豪雨)(지역내(地域內) 3일(日) 연속강우량(連續降雨量) 300~673mm 정도)에 기인되었다. 산지(山地) 사면붕괴(斜面崩壞)를 방지(防止)하기 위해서는 지형적(地形的)으로 산지사면상부(山地斜面上部)의 곡두(谷頭)hollow 위치(位置)에 대한 붕괴억지대책(崩壞抑止對策)이 필요(必要)할 것이며, 위택(位宅)뒷산에서의 밤나무조성작업(造成作業)과 같은 토지이용변경목적(土地利用變更目的)에는 특히 사면배수계통(斜面排水系統)의 교란이 없도록 유의해야 될 것이다. 산사태재해예방(山沙汰災害豫防) 및 피난(避難)등에 대한 주민의식수준(住民認識水準)에서는 문제점이 많이 나타났음으로 민방위교육이나 반상회 등을 통하여 보다 몸에 닿는 풍수해예방대책홍보교육(風水害豫防對策弘報敎育)을 실시해야 될 것이다. 산사태재해대책상(山沙汰災害對策上)으로도 도로(各道) 치산사업소(治山事業所)를 축소하거나 사방전문직(砂防專門職) 기술인력자원(技術人力資源)을 감축해서는 아니될 것이며, 산림청(山林廳)의 "산사태위험지(山沙汰危險地)" 지정기준(指定基準) 및 조사방법(調査方法)에 대한 사방공학적(砂防工學的) 측면(側面)에서의 근본적인 연구(硏究) 검토(檢討)가 요망(要望)된다.

• 대한전기학회:학술대회논문집
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• 대한전기학회 2006년도 제37회 하계학술대회 논문집 A
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• pp.488-489
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• 2006

We investigated the trouble and the influence by weather in the distribution facilities of the home and foreign and analyzed the damage of power system, in domestic and japan, which is related to the latest typhoon and damage from sea wind. The interruption of distribution system is occurred by abnormal weather is cause of the rainstorm, lightning within the country, a tree contact by strong wind in the US and an earthquake, typhoon, damage from sea wind in japan.

• 대한전기학회:학술대회논문집
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• 대한전기학회 2015년도 제46회 하계학술대회
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• pp.398-399
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• 2015

The fault level of power transmission lines caused by natural disaster such as lightning and rainstorm has been on the rise. Especially, the cause of lightning stokes is large part of transmission faults. In order to reduce the lightning failures, it is necessary to measure and analyze the lightning characteristics. This paper deals with observation of the lightning strokes by KEPCO Lightning Detection Network(KLDNet) and analysis including lightning density, multiplicity and amplitude distribution.

• 한국지반환경공학회 논문집
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• 제17권12호
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• pp.5-16
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• 2016

This study aims to assess the influence of rainfall patterns on shallow landslides initiation. Doing so, five typical rainfall patterns with the same cumulative amount and intensity components comprising Advanced (A1 and A2), Centralized (C), and Delayed (D1 and D2) were designed based on a historical rainstorm event in Jinbu. Mt area. Those patterns were incorporated as the hydrological conditions into the Transient Rainfall Infiltration and Grid-based Regional Slope-stability Model (TRIGRS) to assess their influences on groundwater pressure and changes in the stability of the slope. The results revealed that not only the cumulative rainfall thresholds necessary to initiate landslides, but also the rate at which the factor of safety decreases and the time required to reach the critical state, are governed by rainfall patterns. The sooner the peak rainfall intensity, the smaller the cumulative rainfall threshold, and the shorter the time until landslide occurrence. Left-skewed patterns were found to have a greater effect on landslide initiation. Specifically, among five rainfalls, pattern (A1) produced the most critical state. The severity of response was followed by patterns A2, C, D1, and D2. Our conclusion is that rainfall patterns have a significant effect on the cumulative rainfall threshold, the build-up of groundwater pressure, and the occurrence of shallow landslides.

• 한국안전학회지
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• 제31권2호
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• pp.49-56
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• 2016

In Korea, there exist many mountains, and sudden storms occur during the summer season. When severe rainstorm events occur in steep slope topography, risk of debris flow is increased. Once debris flow occurs in urban area, it may cause casualties and physical damages due to rapid debris flow velocity along a steep slope. Accordingly, preventing method of sediment-related disaster for demage mitigation are essential. Recently, various studies on debris flow have been conducted. However, the prediction of the physical propagation of debris flow along the steep slope was not thoroughly investigated. Debris flow is characterized by various factors such as topography, properties of debris flow, amount of debris flow. In the study the numerical simulation was focused on the topographic factor. Fundamental analysis of the risk area was implemented with emphasis on the propagation length, thickness, and the development of maximum velocity. The proposed results and the methodology of estimating the structural vulnerability would be helpful in predicting the behavior and the risk assessment of debris flow in urban area. These results will be able to estimate the vulnerability of urban areas affected the most damage by debris flow.

• Environmental Engineering Research
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• 제21권3호
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• pp.226-232
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• 2016

Rainfall is one of crucial factors that impact on our environment. Rainfall data is important in water resources management, flood forecasting, and designing hydraulic structures. However, it is not available in some rural watersheds without rain gauges. Thus, effective ways of interpolating the available records are needed. Despite many widely used spatial interpolation methods, few studies have investigated rainfall center characteristics. Based on the theory that the spatial distribution of convective rainfall event has a definite center with maximum rainfall, we present a mathematical interpolation method to estimate convective rainfall distribution and indicate the rainfall center location and the center rainfall volume. We apply the method to estimate three convective rainfall events in Santa Catalina Island where reliable hydrological data is available. A cross-validation technique is used to evaluate the method. The result shows that the method will suffer from high relative error in two situations: 1) when estimating the minimum rainfall and 2) when estimating an external site. For all other situations, the method's performance is reasonable and acceptable. Since the method is based on a continuous function, it can provide distributed rainfall data for distributed hydrological model sand indicate statistical characteristics of given areas via mathematical calculation.