During the research period, error analysis of the amount of daily precipitation was performed with data obtained from 2DVD, Parsivel, and AWS, and from the results, 79 days were selected as research days. According to the results of a synoptic meteorological analysis, these days were classified into ‘LP type, CF type, HE type, and TY type’. The dates showing the maximum daily precipitation amount and precipitation intensity were ‘HE type and CF type', which were found to be attributed to atmospheric instability causing strong ascending flow, and leading to strong precipitation events. Of the 79 days, most days were found to be of the LP type. On July 27, 2011 the daily precipitation amount in the Korean Peninsula reached over 80 mm (HE type). The leading edge of the Northern Pacific high pressure was located over the Korean Peninsula with unstable atmospheric conditions and inflow of air with high temperature and high humidity caused ascending flow, 120 mm/h with an average precipitation intensity of over 9.57 mm/h. Considering these characteristics, precipitation in these sample dates could be classified into the convective rain type. The results of a precipitation scale distribution analysis showed that most precipitation were between 0.4-5.0 mm, and ‘Rain’ size precipitation was observed in most areas. On July 9, 2011, the daily precipitation amount was recorded to be over 80 mm (CF type) at the rainy season front (Jangma front) spreading across the middle Korean Peninsular. Inflow of air with high temperature and high humidity created unstable atmospheric conditions under which strong ascending air currents formed and led to convective rain type precipitation.

This study analyze the synoptic meteorological cause of rainfall, rainfall intensity, drop size distribution(DSD), fall velocity and oblateness measured by the 2D-Video distrometer(2DVD) by comparing two cases which are heavy rainfall event case and a case that is not classified as heavy rainfall but having more than 30 mm h-1 rainrate in July, 2014 at Gimhae region. As a results; Over the high pressure edge area where strong upward motion exists, the convective rain type occurred and near the changma front, convective and frontal rainfall combined rain type occurred. Therefore, rainrate varies based on the synoptic meteorological condition. The most rain drop distribution appeared in the raindrops with diameters between 0.4 mm and 0.6 mm and large particles appeared for the convective rain type since strong upward motion provide favorable conditions for the drops to grow by colliding and merging so the drop size distribution varies based on the location or rainfall types. The rainfall phases is mainly rain and as the diameter of the raindrop increase the fall velocity increase and oblateness decrease. The equation proposed based on the 2DVD tends to underestimated both fall velocity and oblateness compared with observation. Since these varies based on the rainfall characteristics of the observation location, standard equation for fall velocity and oblateness fit for Gimhae area can be developed by continuous observation and data collection hereafter.

기후변화에 따라서 강수량과 강수의 강도는 지속적으로 증가하여 집중호우의 빈도가 높아질 것으로 예측되고 있으며, 이러한 집중호우에 의한 피해를 최소화하기 위해서는 강수에 대한 지속적인 관측 및 그에 대한 특성 분석이 필요하다. 이에 따라 본 연구에서는 집중호우 사례에 대한 종관기상상태에 따라 그 원인을 분류하고, 분류된 사례의 강수율, 수직낙하 속도, 강수입자의 크기 등에 대한 제반 특성을 분석하였다. 본 연구에서 경상남도 김해시를 대상으로 2011년 여름철 기간 동안(총 34일의 강수일) AWS와 2DVD를 이용하여 관측을 수행하였다. 집중호우 사례는 장마전선, 태풍, 기압골, 고기압 가장자리의 4가지 원인으로 분류되었다. 각 사례에 대한 대표사례일의 강수율, 빗방울 크기분포, 강수의 침강속도, 강수직경에 따른 입자의 편평도를 분석해본 결과, 강수 입자크기와 입자에 따른 수직 낙하 속도와 편평도의 변화를 알 수 있었다. 또한 각 시간대의 강수율은 평균 강수율이 아닌 수 차례의 peak를 나타내었는데 이를 10분 단위로 세분화 시켜 분석해본 결과, 시간 강수량의 강수율과 강수입자의 분포와 거의 유사하게 나타났으며, 10분 간격으로 나타나는 강수량의 편차가 크게 나타나는 것을 알 수 있었다. 이는 강수에 의한 재해는 짧은 시간에 많은 비가 내리는 것이기 때문에 기후변화에 따른 집중호우의 특성을 밝히고, 대비책을 수립하는데 기초자료를 제시해 줄 것으로 판단된다. 향후 보다 장기적인 관측을 통해 많은 사례에 대한 분석이 이루어진다면 기후변화로 인해 변화하고 있는 강수의 특성에 대해 이해할 수 있을 것이며, 향후 집중 호우 등에 의한 재해를 예방하는데 중요한 기초자료로 활용될 수 있을 것이다.