The Korea native plants of south-east of Mt. Gumsan in the summer was 32 families and 77 species, then the compositae had the largest species as 16. The pteridaceae was I species. The south-west of Mt. Gumsan was 32 families and 72 species. The gramineae was 9 species, and selaginellaceae and aspidiaceae was 1 species, respectively. The north-east of Mt. Gumsan was 42 families and 100 species. The compositae was 9 species, and aspidiaceae was 5, polypodiaceae was 2, and pteridaceae was 1 species, respectively. The north-west of Mt. Gumsan was 43 families and 135 species. The compositae was 24 species, and aspidiaceae was 3, pteridaceae was 2, and lycopodiacea was 1 species, respectively.

본 연구에서는 여름철 호남 서해안 지역의 강수량 분포에 영향을 미치는 요인을 분석하고, 그 원인을 파악하기 위해 1971~2005년간의 호남 서해안 지역에 위치한 목포와 군산의 여름철 강수량 변화와 서해상의 죽도와 말도의 해수면 온도 변화, 그리고 두 변수간의 관계를 분석하였다. 또한 호남 서해안 지역의 여름철 강수 특성이 이 지역의 농업 발달에 미친 영향에 대해서도 파악하였다. 서해에 면한 호남 지방의 서해안 지역은 전반적으로 바다의 영향을 많이 받는다. 따라서 서해는 조석 현상으로 인한 냉수대와 조석 전선으로 인해 해수면이 차가워진다. 이로 인해 이를 지나는 공기가 냉각되어 안정되므로 비를 적게 내리는 소우 현상이 나타난다. 최근 이 지역의 강수량 증가 경향은 서해의 해수면 수온 상승에 따른 결과이다. 그리고 이는 이 지역의 여름철 강수가 서해의 영향을 강하게 받고 있음을 반증한다. 이로 인해 호남 지방의 서해안 지역과 그에 접한 평야 지역은 우리나라의 여름철 가뭄 발생 비율이 전국에서 가장 높은 지역에 속하였다.

This study aims to estimate a urban heat island potential distribution based on the land-use types using Landsat TM(1100 LST August 2004) and AWS data in Daegu. The heat island potential is defined as a difference between surface temperature and air-temperature at each place. The study area was selected as about 900㎢ square including Daegu metropolitan area. Land-use data obtained by dividing all of Daegu metropolitan area into 1-km-square three types of maps were prepared in the 1960s, 1970s and 2000s respectively. Land-use types were classified into 5 categories. Forest and farm lands have been reduced at a wide range during 40 years. Most of those changed into urban area. The heat island potential distribution presented a striking contrasts according to land-use types. For example, the heat island potential of urban area was higher than 10℃ in comparison to those of water or paddy rice areas.

수문시계열을 분석하기 위한 방법으로 낮은 차원에서 해석이 가능한 주성분분석 방법의 문제점을 검토하고 이를 보완할 수 있는 독립성분분석의 이론과 특성을 검토하였고 수문기상자료인 Nino지역의 해수면온도에 적용하여 El -Southern Oscillation(ENSO) 사상과의 상관성을 평가하였다. 혼합자료를 사용하여 독립성분분석 방법의 주성분 분리 능력을 검토한 결과 독립성분분석이 기존 주성분분석에 비해 통계적으로 우수한 결과를 나타내었다. El 의 감시

This study examines the local ozone photochemistry in the urban air. The photochemical formation and destruction of ozone was modeled using a photochemical box model. For the model prediction of ozone budget, measurements were carried out from an urban monitoring station in Seoul (37.6˚N, 127˚E), Korea for intensive sampling time period (Jun. 1～15, 2003). Photochemical process is likely to play significant role in higher ozone concentrations during the sampling period. The results of model simulation indicated that photochemical ozone production pathway was the reaction of NO with HO2 while ozone destruction was mainly controlled by a photochemical destruction pathway, a reaction of H2O with O(1D). The contribution of NMHCs to formation and destruction of ozone in the urban was significant. This was entirely different from remote marine environment. The rates of net photochemical ozone production ranged from 0.1 to 1.3 ppbv h-1 during the study period.

Meteosat-5 IR 위성영상을 사용하여 1999년과 2000년 여름몬순기간 동안 발생한 네팔과 인디아 북쪽 히말라야 산악지역에 발생하는 여러 형태의 대류계 즉, 중규모 대류계들 (Mesoscale Convective Complex, MCC and Convective Cloud Clusters, CCC) 와 보다 약한 Disorganized Short-lived Convection (DSL)의 이동특성 및 시공간적인 생성특성 등을 조사하였다. 대상지

The meteorological elements were measured to investigate cause of summertime ice formation at Unchiri, Gangwon Province. The cause of freezing at valley was conformed as adiabatic expansion theory, latent heat of evaporation, natural convective theory, cold air remain theory, and convective freezing theory according to former study. However nither theory produced a satisfactory explanation. This studying area is not valley but ridge, and underground water surface exists at below than freezing height. wintertime temperature drop and summertime cold air spouting were explain as natural convective theory, generation of water drop on the rock was explained as cooling theory by air expansion, and ice formation on the rock was explained as adiabatic expansion theory. In conclusion, formation of ice valley at Unchiri was formed by natural convective theory, adiabatic expansion theory, and latent heat of evaporation successively.

Photochemical-Trajectory model was used to understand the production of ozone in the atmospheric boundary layer. This model was composed of the trajectory and the photochemical models. To calculate trajectories of air parcels, winds were obtained from the three-dimensional nonhydrostatic mesoscale model (PSU/NCAR MM5V2), and the results were interpolated into constant height surfaces. Numerical integration in the trajectory model was performed by the Runge-Kutta method. The photochemical model consisted of chemical reactions and photodissociation processes. Chemical equations were integrated by the semi-implicit Bulirsch-Stoer method. We performed our experiments from 21 July to 23 July 1994 during the summer time for Seoul area. During the time of maximum ozone concentration in Seoul, four trajectories of air parcels which traveled from Inchon to Seoul were selected. Ozone concentrations estimated by two models are compared with observed one in Seoul area and the photochemical-trajectory model is better fitted than pure photochemical model. During the selected period, high ozone concentrations in Seoul area were more influenced by transferred pollutants from Inchon than emitted pollutants in Seoul.

1998년 여름철, 기상레이더와 레이더 주위의 고밀도 우량계 관측자료를 이용하여 관계식을 산출하기 위하여 관악산 레이더 자료와 강우강도 자료의 확률밀도함수를 구해 확률이 같은 지점을 매치시키는 Window Probability Matching Method(WPMM)라는 통계적 방법을 사용하였다. 레이더 반사도의 확률 분포는 약 15dBZ에서 가장 많은 빈도 분포를 보였고 강우강도의 확률분포는 대부분의 영역에서 시간당 10mm 이하의 비가 내리는 것으로

The purpose of this study was to quantitatively determine the indoor infiltration of pollutants of outdoor origin. The relationship between indoor and outdoor air is dependent, to a large extent, on the rate of air exchange between these two environments. Mean indoor/outdoor ratios measured from this study were: 0.70 for HNO_3; 1.60 for HNO_2; 0.56 for SO_2; 1.30 for NH_3; 0.96 for PM_2.5(d_p<2.5μm); 0.89 for SO_4^2-; 0.87 for NO_3^- and 0.79 for NH_4^+. Mean indoor concentrations for PM_2.5, SO_4^2-, HNO_3, NO_3^- and NH_4^+ were similar to outdoor levels. Indoor HNO_2 and NH_3 values were higher than outdoors. However, the indoor level of SO_2 was lower than ambient level.

In order to see the stratification related to the heat flux in Deukryang Bay, the oceanographic data on July 12, 1994 and the meteorological data of Kohung and Kwangju meteorological stations were analyzed. The temperature differences between the sea surface and the near bottom were 1∼3℃ on spring tide (July 12, 1994) in Deukryang Bay. The air temperature anomalies were high about 3℃ during summer in 1994. These mean that the tidal mixing was not effective in destroying the stratification due to the sea surface heating by the solar radition, even though it was on spring tide. The maximum solar radiation was about 600 ly/day, which was the value of the same date of oceanographic observation. The sensible and the latent heat flux which are 0∼100 ly/day were not so varied during summer. The absorbed heat flux through the sea surface was mostly lost by the back radiation, which ranges are about 0∼-400 ly/day. The dimensionless mixing parameter related to the buoyancy flux was 5∼-150×l0 ㄷ테 (-5). The efficiency of tidal mixing to destroy the stratification was 0.4∼0.6%.

1961년 이전에 관측이 시작되어 30년 이상의 관측자료가 있는 기상청의 15개 관측소의 강수량 자료를 이용하여 우리나라의 여름철 강수량 분포 특성을 조사하였다. 특히 이 연구에서는 우리나라 강수량 기후 평년값을 이용하여 기후적 특성을 조사하였으며, 지역별로 연 강수량, 여름철 강수량, 장마기간중 강수량의 연도별 변동을 비교 분석하고 그 상관을 조사하였다. 대체로 우리나라의 경우 연 강수량의 반 이상이 6, 7, 8월의 여름철에 집중되어 있고, 또 이

A Lagrangian dispersion model has been developed to study the transport of atmospheric pollutants over the southern Korean peninsula on sunny summer days. A mesoscale atmospheric model has been employed to provide the wind fields and information for turbulent diffusion for the calculation of trajectories using a conditioned particle technique. The model has been applied to the simulation of trajectories transport of atmospheric pollutants emitted from five sources in the coastal locations under various synoptic scale winds. Under calm synoptic scale condition, the particles emitted during daytime are mixed vertically and transported toward inland by sea-breeze, according to the model simulation. The particles are then transported upward at the sea-breeze front or by the upward motion over the mountain, and some particles show tendency of returning toward the coast by the return flow of the sea-breeze circulation. The particles are found to remain over the peninsula throughout the integration period under calm synoptic scale condition. When there is westerly synoptic scale wind, the particles emitted in the west coast can reach the east coast within a day or faster depending on the speed. With a synoptic scale southerly wind of 5 m/s, most of the particles from the five sources are advected toward inland during daytime. During nighttime, significant portion of particles released in the west coast remains over the land, while most particles released in the east coast move toward the sea to the east of the middle peninsula.

땅두릅 여룹철 연화재배(軟化栽培) 가능성(可能性)을 검토(檢討)하기 위하여 흑색(黑色) PE와 은색(銀色) 단섬유불직포(短纖維不織布)를 이용하여 5월 정식(定植)을 포함하여 6월, 7월, 8월 정식기(定植期)에 대하여 시험(試驗)한 결과(結果)는 다음과 같다. 1. 수확소요일수(收穫所要日數)는 5월 정식(定植)에서 20일(日)이고 7월, 8월 정식(定植)에서는 15일로 단축(短縮)되었으나 생육기간중(生育期間中)의 적산온도(積算溫度)는 400℃ 범위이었다. 2. 7월 정식(定植)에서 땅두릅 연화수(軟化莖)의 수량(收量)은 고온(高溫)으로 인한 연부현상(軟腐現狀)으로 낮은 경향(傾向)이었다. 3. 각(各) 부위별(部位別) 경도(硬度)는 상위부(上位部)가 연(軟)하고 하위부(下位部)가 단단한 경향(傾向)이고, 저온저장(低溫貯藏) 7일후(日後)에도 신선도(新鮮度)는 유지(維持) 되었다. 4. 5월, 6월 정식재배시(定植栽培時) 18,000천원/ha 이상(以上)의 소득(所得)을 얻을 수 있었다.