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爸山의 年降水量 및 夏季降水量의 Normality에 關한 研究
文勝義 부산대학교 과학교육연구소 1975 교사교육연구 Vol.2 No.2
The normality of the annual and summer rainfall in Busan were analysed statistically with rainfall rocords (1905… 1974). The annual rainfall in Busan shows the normal distribution at the 5% significance level. However, the summer rainfall does not fit the normal distribution at the same significance level.
文勝義,黃水鎭 釜山大學校 師範大學 1977 교사교육연구 Vol.4 No.2
There are f reezing phenonena in summer at so called "Ice-valley" in the south-eastern part of the Korean peninsula. The purpose of this paper is to examine the causes of this ice-forming phenomena which can be explained by following causes. (1) As the valley is very deep and is toward the North, the insolations to the "Ice-valley" are very little through the year. Therefore, the under ground (15m from the surface) temperatures maintain about 6°C in summer. (2) The upper capillary zone is considered as a adiabatic situation because this zone is insulated from the solar radiation by the Talus having very large boulders(50-20G<* in dia.) (3) As the defferences of saturated vapor pressure between upper capillary zone and outside of the Talus are very high, the evaporization will be occur on the upper capillary zone. (4) Consequently, water is frozen by the loss of evaporization heat due to the evaporation at the upper capillary zone.
지형인자를 사용한 금강산지역의 강수량 추정에 관한 연구
문승의,박종길 한국지구과학회 1990 韓國地球科學會誌 Vol.11 No.3
The purpose of this study is to estimate rainfall around the district of Mt. Kumgang using several orographic factors where rainfall can not be measured routinely. Orographic factors used are height-reading, direction of main valley, relative relief, degree of exposure, and direction of maximum slope. The distribution of calculated rainfall around Mt. Kumgang coincides well with that of observed one and shows much rainfall in summer.
수평조밀격자 GCM을 이용한 적도 태평양상의 SST anomaly에 대한 대기 반응 연구
문승의,안중배,김유근 한국환경과학회 1995 한국환경과학회지 Vol.4 No.5
The atmospheric responses to a Sea Surface Temperature Anomaly(SSTA) over the equatorial eastern Pacific Ocean have been investigated using the horizontally fine resolution model based on OSU 2-layer Atmospheric General Circulation Model(AGCM). The SSTAs during the peak phase of 1982-83 El Nin∼o have been applied to the model as the boundary conditions of the experiment. The model simulates the eastward movement of the rising branch of the Walker circulation. That is, the major features associated with the El Nin∼no such as the increase of the precipitation rate over the center of the Pacific and decrease over the Indonesia, and the 500hPa geopotential height anomaly in the middle latitude are properly described in the fine resolution model experiment. The model results indicate that this horizontally fine resolution GCM can successfully simulate the ENSO anomalies and be more effectivelly used for the study of the climate and the climate changes.