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봄철 양평지역(楊平地域)의 지형(地形) 및 고도(高度)에 따른 일최저기온(日最低氣溫)의 분포(分布)
강안석,윤진일,정영상,노부테루 타니,Kang, An-Seok,Yun, Jin-Il,Jung, Yeong-Sang,Tani, No Bureru 한국토양비료학회 1986 한국토양비료학회지 Vol.19 No.4
농작물(農作物)에 대(對)한 서리의 피해(被害)는 재배지(栽培地)의 지형적(地形的) 특성(特性)과 밀접(密接)한 관계(關係)가 있으며, 일최저기온(日最低氣溫)의 평면적(平面的)인 분포(分布)는 야간복사냉각조건(夜間輻射冷却條件)과 냉기중력이동조건(冷氣重力移動條件)의 지역적(地域的)인 차이(差異)에 의(依)해 특징(特徵)지워진다. 과원지대(果園地帶)의 지형적조건(地形的條件)과 봄철 최저기온형성간(最低氣溫形成間)의 관계(關係)를 구명(究明)하기 위(爲)하여 1986년(年) 4월(月) 29일(日)부터 5월(月) 2일(日)까지 경기도(京畿道) 양평군(楊平郡) 남한강(南漢江) 유역의 과수원지대(果樹園地帶)에서 최저기온(最低氣溫)의 분포상태(分布狀態)를 조사(調査)하였다. 최근(最近) 수년간(數年間) 빈번한 동상해(凍霜害)로 인(因)해 과수재배(果樹栽培)가 중지(中止)된 지역(地域)을 관통(貫通)하는 직선거리(直線距離) 8.5km의 경로(經路) A에 대(對)하여 17개(個)의 고정관측점(固定觀測點)을 설치(設置)하였으며 피해(被害)를 거의 받지않아 현재(現在), 재배중(裁培中)인 지대(地帶)를 통과(通過)하는 직선거리(直線距離) 2.5km의 경로(經路) B에 대(對)해서는 일출직전(日出直前) 1시간여(時間餘)에 걸쳐 이동관측(移動觀測)을 수행(遂行)하였다. 관측(觀測)은 흐린 날과 갠 날로 나누어 실시(實施)하였다. 맑고 바람이 잔잔했던 (풍속(風速)<0.5 m/sec) 4월(月) 30일(日) 아침의 최저기온(最低氣溫)은 대체(大體)로 해발온도(海拔溫度)가 높을수록, 높게 나타났으며(강변(江邊), 마을지역제외(地域除外)), 흐리고 바람이 다소(多少) 강(强)했던 (풍속(風速) 1.5~2.5 m/sec) 5월(月) 1일(日) 아침에는 지형조건(地形條件)이나 해발고도(海拔高度)에 따른 최저기온변화(最低氣溫變化)가 거의 없었다. 피해(被害)가 경미(輕微)한 대흥리과수원(大興里果樹園)은 맑은 날 아침 최저기온(最低氣溫)이 주변저지대(周邊低地帶)에 비(比)하여 $1^{\circ}C$ 높았으나, 폐원(廢園)된 병산리일대(屛山里一帶)는 극최저기온(極最低氣溫)이 나타나는 중간지대(中間地帶)임이 확인(確認)되었다. Frost damage which can reduce yields, impair fruit quality and cause loss of trees is closely related to the occurrence of daily minimum temperature. Horizontal distribution of air temperature minima can be characterized by conditions of radiational cooling and gravitational movement of cold air, which are influenced by the regional topographic features. Observations were made on the air temperature minima over Yangpyeong area, to delineate potential effects of topography on the temperature pattern during spring season. Two routes were selected for the observation. Liquid glass minimum thermometers were installed at 17 sites through the old peach orchards which had been closed due to the frequent freeze-frost hazards during the recent years. This route was 8.5km long and the highest point was 350m above mean sea level. The other route, which was 2.5km in distance, was run with a digital resistance thermometer during the hour just before sunrise. Observations were made both on a calm-clear day (April 30, 1986) and a windy-overcast day (May 1, 1986). The temperature on April 30 was in increasing trend with elevation but this was modified at near the riverside and the downtown area. An orchard lying on a hilltop showed the temperature $1^{\circ}C$ higher than near by lowland of which elevation was about 30m lower. The minimum temperature on the overcast day was little affected by terrestrial conditions but by the atmospheric lapse condition. The peach orchards severely damaged by cold air were found in the area where the lowest minimum temperature was observed. The results may be useful for selection of the proper orchard location to be developed in an area.
스펙트로레디오메터를 이용한 벼 생장시기의 분광반사 특성 변화분석
장세진(Se Jin Jang),서애숙(Ae Sook Suh),김판기(Pan Gi Kim),윤진일(Jin Il Yun) 한국지리정보학회 2000 한국지리정보학회지 Vol.3 No.3
Knowledge for reflectance characteristic of interesting targets will provide us with actual application of remote sensing on agriculture, In this study, we have measured and analyzed reflectivity characteristic based on growing status form transplanting t
김수옥 ( Soo Ock Kim ),윤진일 ( Jin Il Yun ),정유란 ( U Ran Chung ),황규홍 ( Kyu Hong Hwang ) 한국농림기상학회 2010 한국농림기상학회지 Vol.12 No.4
본 연구는 3면이 바다로 둘러싸인 우리나라에서 해안지대 기온 관측자료에 포함되어있지도 모르는 바다의 영향을 정량적으로 추정하기 위해 수행하였다. 1981-2009 기간 중 전국 66개 기상관서에서 관측한 일별 최고 및 최저기온자료를 수집하여 월별 평균을 계산하고 이들 가운데 27개 내륙지점 자료만을 이용하여 거리역산가중평균법에 의해 남한 전역의 가상기온분포도를 제작하였다. 이 가상기온분포도 상에서 해안에 가까운 나머지 39개 지점의 국지기온을 지리지형정보 및 소기후모형에 의해 정밀하게 추정하였다. 실측 기온과 이 추정기온과의 편차를 `외견상의 바다효과`로 간주하고 39개 지점의 해안거리 대수를 독립변수로 하는 회귀모형을 월별로 작성하였다. 이 모형에 의하면 우리나라의 바다는 잠재적으로 여름철 일 최고기온에 6℃ 냉각효과, 겨울철 일 최저기온에는 7.5℃의 가온 효과가 있다. 해안은 물론 내륙의 기온자료에도 포함된 공통오차를 제거한 `실제의 바다효과`를 추정한 결과 서해안의 경우 여름철 냉각효과는 1.5℃, 겨울철 가온효과는 1.0℃인 반면, 남해안과 동해안은 각각 3.0℃ 및 3.5℃ 내외로 판명된다. This study was carried out to quantify potential effects of the surrounding ocean on the observed air temperature at coastal weather stations in the Korean Peninsula. Daily maximum and minimum temperature data for 2001-2009 were collected from 66 Korea Meteorological Administration (KMA) stations and the monthly averages were calculated for further analyses. Monthly data from 27 inland sites were used to generate a gridded temperature surface for the whole Peninsula based on an inverse distance weighting and the local temperature at the remaining 39 sites were estimated by recent techniques in geospatial climatology which are widely used in correction of small - scale climate controls like cold air drainage, urban heat island, topography as well as elevation. Deviations from the observed temperature were regarded as the `apparent` sea effect and showed a quasi-logarithmic relationship with the distance of each site from the nearest coastline. Potential effects of the sea on daily temperature might exceed 6.0℃ cooling in summer and 6.5℃ warming in winter according to this relationship. We classified 25 sites within the 10 km distance from the nearest coastline into `coastal sites` and the remaining 15 `fringe sites`. When the average deviations of the fringe sites (0.5℃for daily maximum and 1.0℃ for daily minimum temperature) were used as the `noise` and subtracted from the `apparent` sea effects of the coastal sites, maximum cooling effects of the sea were identified as 1.5℃ on the west coast and 3.0℃ on the east and the south coast in summer months. The warming effects of the sea in winter ranged from 1.0℃ on the west and 3.5℃on the south and east coasts.
지형 - 기후 관계식에 의한 제주도의 월별 기온분포의 추정
신만용(Man Yong Shin),윤진일(Jin Il Yun) 한국산림과학회 1992 한국산림과학회지 Vol.81 No.1
The use of meteorological information is essential in the industrial society. More specialized weather services are required to perform better industrial activities including forestry. A topoclimatological technique, in this study, which makes use of empirical relationships between the topography and the weather in Cheju Island was applied to produce reasonable estimates of monthly air temperatures over remote land area where routine observations are rare. Altitude values of the 250m grid points were first read from a 1 : 25000 topographic map. The mean altitude and other valuable topographical variables were then determined for each 1 ㎢ land area. Daily minimum, maximum and mean air temperature data were collected from 19 points in Cheju Island from June 1987 to September 1988. The data were analyzed and grouped into 36 sets by type of air temperature and by month. Each of data set was regressed to the topographical variables to delineate empirical relationships between the local air temperature and the site topography. The total of 36 regression equations were finally selected and the equations were used to calculate the monthly air temperature for each 1 ㎢ land area. The outputs were presented in a fine-mesh grid map with a 6-level contour capability.