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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.
釜山地方의 年降水量 및 月降水量의 Anomaly level에 關한 硏究
文勝義,水縝 부산대학교 과학교육연구소 1979 교사교육연구 Vol.6 No.2
The annual and monthly precipitations in Pusan area for 1904-1974 were classified into five anomaly, levels and were analyzed statistically to know the frequency distribution and its characteristcs of each anomaly level. The results of this study are as follows: 1) The maximum frequency of anomaly levels occurs on LN-level and a level is not denoted higher or lower than S-lvel or GA-level in the annual precipitation. 2) In the monthly precipitations, there are no EA-levels in January, March, June, July, September, December and no MEA-levels except in January, February, June, and October.
문승의,노재식,김백조,하창환,최성식 한국환경과학회 1998 한국환경과학회지 Vol.7 No.3
The intensive meteorological observations including pibal balloon at Ungcheon, airsonde and 10m meteorological tower observations at Gulup-Do, where are located in the western coastal region, are taken to investigate the characteristics of the upper and lower atmospheric structure and the local circulation pattern during the period of 17 to 22 September 1996. The diurnal variations of weather elements(i.e, air temperature, humidity, pressure, and wind speed) at Gulup-Do are analyzed and discussed with those at four inland meteorological stations. The vertical profiles of wind vector, orthogonality(Ω), and shear obtained from the pibal observations are also presented to examine the change of wind structure according to the synoptic-scale pressure system's movement. The diurnal temperature changes at Gulup-Do are more sensitive than that of inland meteorological stations in case of the inflow of southwesterlies but are not dominant due to the ocean effect under the influence of relatively cold northerlies. A well defined mixed layer is developed from the 500m to the maximum 1700m with a significant capping inversion layer on the top of it. It can be found from the vertical profiles of wind vector that the wind become generally strong at the interface heights between cloud layers and non-cloud layers. The maximum wind shear is appeared at the height where the variation of wind direction induced by the passage of synoptic-scale pressure system is accompanied with the increase of wind speed. Based on the wind orthogonality, the change of wind direction with height is more complicated in cloudy day than in clear day. In case of a fair weather, the change of wind direction is showed to be at around 2㎞