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地上 氣壓配置型에 따른 高度別 강수량 分布 : 대관령 동쪽 산지 사면을 中心으로 The Case of The East Slope of Taegwllyong Area
이장렬 한국 지리·환경 교육학회 1997 한국지리환경교육학회지 Vol.5 No.1
This study aims to Characterize altitunal distribution of the precipitation according to the Synoptic patterns, on the East Slope of Taegwallong Area, for the periods 1989~1992. The results of the study are as follows. 1. There are 6types of precipitation according to precipitation cause for 235 wet days: Low-pressure type (Low-pressure trough and Front type), High-pressure type, Siberian high-pressure type, Jangma Front type, Typhoon type, Ohtzk-Sea High Pressure type. 2. The Scope of the daily precipitation with altitude is the most 28~54㎜ of Typhoon type and the least 12~20㎜ of Siberian high-Pressure. 3. Taegwallyong Area has the daily maximum Precipitation in the all altitudes of 6 Pressure types 4. The daily Precipitation with altitude in Low-pressure type, High-pressure type, and Ohtzk-Sea High-pressure tends to have more precipitation at higher altitude. 5. In the events in which the difference of precipidtation between Taegwallyong and Kangnung occured on spring, Autumn and Winter, Precipitation at Kangnung is much than that at Taegwallyong in 19 days of Siberian High-pressure, 5days of High-pressure.
이장렬 관동대학교 1996 關大論文集 Vol.24 No.1
The purpose of this paper is to investigate the climatological environment of Kangnung district. Local analysis and weather observations have seen tried to inquire into the climatological elements such as temperature, rain, snow, wind, sunshine and fog. This result may be summarized as follows : Compared monthly mean temperature in summer at Kangnung with that at Wonju, Hongchen of yeongseo Region, it is not great difference. But monthly mean temperature in winter at Kangung is higher 2∼3℃ than that at Wonju, Hongchen. The daily precipitation 30-80㎜ of monthly normals (1961-1990) at Kangnung and taegwallyong appeared from January to December and above 80㎜, largely from June to November. Monthly mean precipitation(1989-1992) increase with height to Taegwallyon from Anmock by the sea, the greatest of monthly mean precipitation appeared at Taegwallyoung. The most frequent wind direction for annual mean wind direction(1961-1990) at Kangnung is SW-wind(2.8m/s) and Taewalyong is W, WNW-wind(3.4∼3.8m/s). Summer around Taegwallyong is a short period and its opening day is on July 21, its closing day, on August 15.
이장렬 한국제4기학회 2002 제사기학회지 Vol.16 No.2
본 연구에서는 1995-2001년에 고성지방의 산불 다발생지 10개 지역을 대상으로, 산불발생의 인위적 요인과 기상요인을 파악하였다. 그 결과를 요약하면 다음과 같다. 같은 곳에서 산불이 3회 이상 발생한 곳은 거진읍 거진리, 간성읍 선유실리, 죽왕면 마좌리 등이고, 인접지역에서 계속, 산불이 3회 이상 발생한 곳은 토성면의 학야리, 성대리, 인흥리 등이다. 1995-2001년에 산불발생 퐁 46회 중, 3월 11회, 4일 11회, 11월 7회, 1월 6회, 2일 6회, 12일 3회, 10일 2회 등이고, 산불발생이 많은 시간은 11-18시이다. 산불 발생원인은 군사훈련, 논.밭두렁소각, 쓰레기소각, 농산물폐기물 소각, 성묘객실화, 담뱃불, 방화 등인데, 군사훈련과 군부대내의 쓰레기 소각으로 인한 산불발생이 제일 많았다. 산불이 제일 많은 3,4월, 산불 발생 22일의 일평균 최고기온은 일평년값보다 $5^{\circ}C$높았고, 일평균상대습도는 23% 낮았으며, 일평균풍속은 0.8m/s강했다. 그리고 3,4월에는 퓐의 특성을 가진 강풍이 자주 나타난다. 이때, 한반도 중심의 기압배치는 $\ulcorner$남고북저$\lrcorner$형이다. In this paper, the writer attempts to clarify causes by general man and weather factor on forest fire occurrence in Kosong-Area, 1995-2001. The major results are summarized as follows: The forest fire at Kojin-ri, Sonyusil-ri and Majwa-ri occurred at the same area over 3 times and that Hakya-ri, Songdae-ri and Inhung-ri, at the adjoining land over 3times. In the total 46 times of forest fire, fire frequence was greatest in March(11 time) and April(11 time) followed by November(7 time), January(6 time), February(6 time). December(3 time), October(2 time). Hours on frequent forest fire are from 11:00 till 18:00. Number for forest fire occurrence by causes was greatest in military training followed by burning paddy fields, debris burning, burning agricultural debris, visiting a grave, cigarette and arson. Frequent forest fire in Kosong-Area coincide not only with above normal temperatures, but also with below normal relative humidity. When the strong winds appear at Kosong-Area, the properties of daily surface chart re the south high and north low pressure pattern in the Far East Asia.