• 대기
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• 제25권1호
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• pp.31-49
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• 2015

From the hourly data of 75 Korean weather stations over a 12-year period (2001~2012), this study has chosen three cases (January 12, 2006; January 11, 2008; and February 22, 2009) of multiple freezing rains and investigated the atmospheric circulations that seemed to cause the events. As a result, the receding high pressure type (2006), prevailing high pressure type (2008), and warm front type (2009) are confirmed as synoptic patterns. In all three cases, freezing rain was found in regions with a strong ascending current near the end point of a low-level jet that carried the warm humid air from low latitudes. The strong ascending current resulted from lower-level convergence and upper-level divergence. In 2006 and 2009, the melting process was confirmed. In 2008, the supercooled warm rain process (SWRP) was confirmed. In contrast to existing SWRP theory, it was found that the cool air produced at the middle atmosphere and near the earth's surface led to the formation of freezing rain. The sources of this cool air were supposed to be the evaporative latent heat and the cold advection coming from the northeast. On the other hand, a special case was detected, in which the freezing rain occurred when both the soil surface temperature and surface air temperature were above $0^{\circ}C$. The thickness distributions related to freezing rain in Korea were found to be similar to those in North America. A P-type nomogram was considered for freezing rain forecasting; however, it was not relevant enough to Korea, and few modifications were needed.

• 한국환경과학회지
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• 제26권7호
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• pp.827-836
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• 2017

Freezing rain is a phenomenon when precipitation falls as a liquid rain drop, but freezes when it comes into contact with surfaces or objects. In this study, we investigated the predictability of freezing rain and its characteristics, which are strongly related with the occurrence of black ice using synoptic scale meteorological observation data. Two different cases occurred at 2012 were analyzed and in the presented cases, freezing rain often occurs in the low-level low pressure with the warm front. The warm front due to the lower cyclone make suitable environment in which snow falling from the upper layer can change into supercooled water. The $0^{\circ}C$ temperature line to generate supercooling water is located at an altitude of 850 hPa in the vertical temperature distribution. And the ground temperature remained below zero, as is commonly known as a condition for black ice formation. It is confirmed that the formation rate of freezing rain is higher when the thickness after 1000-850 hPa is 1290-1310 m and the thickness of 850-700 hPa layer is larger than 1540 m in both cases. It can also be used to predict and estimate the generation of freezing rain by detecting and analyzing bright bands in radar observation.

• 한국지구과학회지
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• 제23권1호
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• pp.59-71
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• 2002

Theoretical models of radiative transfer are developed to simulate the 85 GHz brightness temperature (T85) observed by the Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) radiometer as a function of rain rate. These simulations are performed separately over regions of the convective and stratiform rain. TRMM Precipitation Radar (PR) observations are utilized to construct vertical profiles of hydrometeors in the regions. For a given rain rate, the extinction in 85 GHz due to hydrometeors above the freezing level is found to be relatively weak in the convective regions compared to that in the stratiform. The hydrometeor profile above the freezing level responsible for the weak extinction in convective regions is inferred from theoretical considerations to contain two layers: 1) a mixed (or mixed-phase) layer of 2 km thickness with mixed-phase particles, liquid drops and graupel above the freezing level, and 2) a layer of graupel extending from the top of the mixed layer to the cloud top. Strong extinction in the stratiform regions is inferred to result from slowly-falling, low-density ice aggregates (snow) above the freezing level. These theoretical results are consistent with the T85 measured by TMI, and with the rain rate deduced from PR for the convective and stratiform rain regions. On the basis of this study, the accuracy of the rain rate sensed by TMI is inferred to depend critically on the specification of the convective or stratiform nature of the rain.

• 대기
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• 제25권3호
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• pp.389-405
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• 2015

In this study, the occurrence circumstances of 3 cases (12 Jan 2006, 11 Jan 2008, 22 Feb 2009) when the freezing rain was observed at more than two observatories in a day with more than three times each observatory, were investigated. Following the advanced study about the same cases, we have tried to find more delicate differences in using the Korea Local Analysis and Prediction System (KLAPS; 5 km reanalysis data) that has the smallest grid scale at current situation. As results, three common characteristics are found: (1) Just before the occurrence of the freezing rain, the wind direction was consistently continuous and the wind speed was constant or gradually increased for at least 3 hr more. (2) Surface air temperature (Relative humidity) was respectively $3.08^{\circ}C$ (28.76%), $0.47^{\circ}C$ (50.07%) and $-3.60^{\circ}C$ (71.07%) 3 hr ago to break out the freezing rain. It means the freezing rain occurs in a wide range of atmospheric environments. However, the closer it got to the occurrence time of the freezing rain, the closer the surface air temperature was to $0^{\circ}C$, and the bigger the humidity of the surface air was. (3) The liquid precipitation formed in the upper atmosphere, met a cold advection bellower than 950 hPa level and suspected to be changed to the super-cooled condition.

• 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.

• 대한토목학회논문집
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• 제26권5D호
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• pp.813-819
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• 2006

미끄럼 저항은 타이어와 도로노면의 마찰저항을 나타내는 지수로 차량의 주행 안전성에 지대한 영향을 미친다. 타이어의 상태, 노면의 마모도, 주행속도, 노면의 건조, 습윤, 결빙 등에 따라 미끄럼저항의 크기는 달라진다. 특히 겨울철 도로노면의 경우 강설 후 기온강하에 도로포장표면이 결빙이 발생할 경우 미끄럼저항이 급격히 저하되며, 미끄럼저항을 회복하고자 제설 작업을 수행하게 된다. 제설작업 후에는 습윤상태로 노면조건이 바뀌게 되는데, 제설제가 노면에 잔류하게 되면 일반적인 습윤상태에서의 미끄럼저항을 확보치 못할 수 있다. 본 연구에서는 국내 포장도로의 대다수를 차지하는 밀입도 아스팔트와 타이닝 콘크리트 포장노면에 대하여 실험실 조건에서 노면 결빙시, 제설중 제설후 잔류물이 노면에 있을 경우의 조건에서의 미끄럼저항을 정량적으로 평가하였다. 연구 결과 노면 결빙시 미끄럼저항 회복시간은 수용액 살포방법이 고체염 살포방법 보다 빠르며 제설제 중에는 소금이 가장 빠르게 나타났다. 노면에 잔류한 제설제는 콘크리트 시편이 아스팔트 시편보다 미끄럼저항 값이 높게 나타났으며 습윤 노면 상태와 비교시 미끄럼저항 확보율은 54~80% 이다.

• 한국구조물진단유지관리공학회 논문집
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• 제25권4호
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• pp.46-55
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• 2021

콘크리트 구조물은 외부 극한기후환경에 노출 될 경우 공용년수가 증가할수록 다양한 문제점들이 발생할 수 있다. 이러한 문제들 중 최근 가장 문제가 되고 있는 폭우, 폭설과 같은 극한 기후요소의 작용으로 동결융해 현상이 발생한다. 본 연구에서는 서울의 경우, 동결융해가 발생하는 기간 동안에 매우 건조한 날씨를 나타내기 때문에 KS F 2456 를 참고하여 콘크리트의 기중 급속 동결 융해 시험법을 제시하였다. 콘크리트 공시체 및 철근콘크리트 휨 부재를 제작하여 0, 100, 200, 300 사이클의 기중 급속 동결 융해를 수행하였으며 성능 평가를 통해 각 실험체의 재료 및 부재 단위에서의 성능 저하를 확인하였다. 300사이클까지 기중 급속 동결 융해를 수행한 설계 강도 24 MPa의 콘크리트 압축 강도는 5.24 MPa(21%) 만큼 감소하며, 기중 급속 동결 융해가 진행될수록 콘크리트의 재료적 강도 감소에 의해 철근콘크리트 휨 부재의 철근의 응력 부담이 증가되어 지진과 같은 외력 발생에 따른 구조물의 에너지 흡수(소산) 능력이 감소한다.

• 대기
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• 제26권1호
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• pp.73-84
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• 2016

A method to make ice spike using home refrigerator with ice tray was found. Many experiments have carried out with this method and many natural phenomena occurring on the formation of ice spike are found. A new concept of the Latter Freezing Water (LFW) was imported to explain the ice spike formation. At LFW position on water surface, the Sprout of Super cooled Water (SSW) grows by the Volume Expansion Effect (VEE) caused by the phase change of water in water. And air bubbles that are expelled from ice during freezing process, gather, rise, and detonate at the upper most part of SSW that make SSW freeze and grow upward with the water pipe in it. Together with VEE the capillarity in the water pipe makes the column grow more, that makes the ice spike. Many other findings were succeeded; 1) Ice spike process is completed before the whole water freezes. 2) If water is corrupted or shocked, even though it is very slight, ice spike is not generated. 3) Rain water contains the most LFW among all kind of waters used in experiments. 4) LFW is changed into normal water after passing the ice spike. 5) A new concept of the ice bullet is introduced. 6) The reason of frequent occurrences of the ice spike at Mt. Mai is investigated also.

• Communications for Statistical Applications and Methods
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• 제12권2호
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• pp.381-394
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• 2005

In order to estimate the damage of orchards due' to natural disasters such as typhoon, severe rain, freezing or frost, it is necessary to estimate the number of fruit bearing before and after the damage. To estimate the fruit bearing after the damages are easily done by delegations, but it cost too high to survey every insured farm household and calculate the fruit bearing before the damage. In this article, we suggest to use a random coefficient model to predict the numbers of fruit bearing in the orchards before the damage based on the tree age and the area information.

• 한국방재학회 논문집
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• 제10권4호
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• pp.47-54
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• 2010

지정폐기물인 폐페인트를 이용한 단열골재 개발을 위한 자료를 제시하기 위하여 이를 위한 실험으로 함수비, 진밀도, 액성한계, 소성한계, 마모감량, 모래당량, 체가름 시험을 진행하였다. 함수비 시험은 80:20의 배합이 1.4이고, 쇄석 골재만 사용한 것은 1.0으로 폐페인트 단열골재의 용적비가 증가하면서 함수비의 증가도 많았다. 또한, 진밀도 시험은 혼입율의 증가에 따라 점점 상승하였고, 흡수율도 증가하였다. 이는 골재와 폐페인트의 특성상 발생되는 공극분포의 차이로 인한 현상으로 판단된다. 모래당량과 마모감량 실험에서는 마모감량은 쇄석골재만 사용한 경우는 13.5이고 20% 혼입한 경우는 14.4로 증가하지만, 이는 단열골재의 약한 조직으로 인한 현상이라 판단된다. 이러한 실험으로 볼 때, 도로공사 시방서의 동상방지층은 모래당량 20, CBR 10으로 만족하도록 규정하고 있어 본 실험은 전 배합에서 모두 품질기준에 만족하는 결과를 보였다. 현재 폐페인트는 단순 매립용하거나, 소각 처리되는 현 실정에서 골재로 활용할 수 있게 됨으로써 천연골재의 부족이나 자원의 낭비를 해소할 수 있을 것으로 파악된다. 기존의 자갈보다 단열효과가 뛰어나고, 가벼우며, 단단한 단열골재를 사용함으로써 재활용이 활발할 것으로 예상된다.