http://chineseinput.net/에서 pinyin(병음)방식으로 중국어를 변환할 수 있습니다.
변환된 중국어를 복사하여 사용하시면 됩니다.
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.
文勝義 부산대학교 환경문제 연구소 1989 環境硏究報 Vol.7 No.-
Not only do the average temperature, precipitation, wind, and other elements determine the climate of a region, but also their variations. In Pusan area, the climatic environments can be summarized as follows: 1) Pusan has mild climate. Mean annual temperature is 14.0℃ with maximum(25.5℃) in August and minimum(2.2℃) in Janury. Mean annual and diurnal range of temperature are 23.3℃ and 7.3℃ respectively. 2) Pusan belongs to an area of much rain in Korea during the whole season. Mean annual precipitation is 1,466.2mm with maximum(242.7mm) in July and minimum(26.9mm) in January. The variability of annual precipitation is 24.5%. Orographic precipitation is not an important factor in rainfall distribution in Pusan. 3) Relative humidity is high in summer with maximum(86%) in July and low in winter with minimum(52%) in January. 4) Prevailing wind directions are NNE and NW. Mean annual wind speed(4.4m/s) is the strongest in Korea. 5) The lists of meteorological diesasters occurred in Pusan during 1904∼1985 are presented.
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.