• 한국환경농학회지
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• 제14권1호
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• pp.15-22
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• 1995

전북 평야지역의 산성(酸性)비 강수양상(降水樣相)을 파악하기 위하여 이리시(裡里市) 교외에 위치한 호남농업시험장 내에서 1992년 1월부터 12월까지 강수(降水)의 화학적(化學的) 조성(組成)을 분석 조사한 결과를 요약하면 다음과 같다. 1. '92년 산성비 출현율(出現率)은 연평균(年平均) 82.5%이었으며 6월이 17%로 가장 낮았다. 2. pH 수준별 강수량 분포(分布)는 pH $4.5{\sim}5.0$의 범위가 54.0%로 가장 많았으며 pH 4.0 이하의 강수(降水)는 9.6 mm로 연강수량(年降水量)의 1.1%이었다. 3. 강수(降水) PH를 계절별로 보면 여름(4.78)>가을(4.59)>봄(4.52)>겨울(4.16)의 순(順)으로 높은 경향이었다. 4. 강수(降水)의 pH 감소(減少)와 상관(相關)이 높은 성분은 $SO_4^{2-}$ 와 $NO_3^-$이었으며 두 성분(成分)의 당량비(當量比)는 2.85:1 이었다. 5. 강수성분조성(降水成分組成)은 $SO_4^{2-}$>$NH_4^+$>$Cl^-$>$Ca^{2+}$>$NO_3^-$>$Na^+$>$H^+$>$K^+$>$Mg^{2+}$의 순(順)으로 함량이 높았으며 음이온의 양이온에 대한 당량비(當量比)는 1.20이었다. 6. 질소($NO_3-N$ + $NH_4-N$)와 칼리($K_2O$)의 연강하량(年降下量)은 각각 1.19, 0.53 kg/10a ${\cdot}$ year이었다.

• 한국환경과학회지
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• 제20권7호
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• pp.857-872
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• 2011

The variation of groundwater level in Jeju Island is analyzed with the data of precipitation observed from 48 monitoring post and groundwater level observed from 84 monitoring wells during 2001 to 2009. The groundwater level rises in summer and falls in winter. The rise of groundwater level by precipitation is fast and small in the eastern region and slow and large in the western region. However, the speed of fall during the period of no rain is slower in the eastern region than in the western region. It tells that permeability is greater in the eastern region than in the western region. In this paper, we set up the base level of groundwater and calculate recharge volume between the base level and groundwater surface. During the period, the average recharge volume was $9.83{\times}10^9m^3$ and the maximum recharge volume was $2.667{\times}10^{10}m^3$ after the typhoon Nari. With these volume and the recharge masses obtained by applying the recharge ratio of 46.1%, estimated by Jeju Province (2003), the porous ratio over the whole Jeju Island is 16.8% in average and 4.6% in the case of maximum recharge volume just after typhoon Nari. A large difference in the two ratios is because that it takes time for groundwater permeated through the ground just after rain fall to fill up the empty porous part. Although the porous ratios over the whole Jeju Island obtained in this way has a large error, they give us the advantage to roughly estimate the amount of recharged groundwater mass directly from observing the groundwater level.

• 한국산림과학회지
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• 제106권1호
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• pp.63-69
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• 2017

본 연구에서는 경상남도 산청군 웅석봉군립공원 내 활엽수림유역을 대상으로 산악성 강수특성과 녹색댐 기능을 구명하기 위해 총 6년 동안(2011~2016년) 수문 모니터링을 실시하였다. 산지(시험유역)와 평지(산청 기상관측소)의 강수특성을 비교한 결과, 평지에 비해 산지에서 강수량이 많았으며, 산지에서 강수강도가 높은 것으로 볼 때 산악성 강수효과가 작용하는 것을 알 수 있었다. 또한 조사대상 기간(2011~2016년)은 평년(1981~2010)에 비해 강수량이 증가하였고, 계절적 강수분배 등이 변화한 것은 나타나 기후변화로 인해 산청지역의 강수환경도 변화한 것으로 나타났다. 한편, 유출률은 봄이 가장 높게 나타났고 겨울, 여름, 가을 순으로 나타났으며, 이는 산지적설과 융설의 영향으로 판단된다. 그리고 유출수량은 여름, 봄, 가을, 겨울 순으로 높았으며, 총 유출량은 $10,143.8ton{\cdot}ha{\cdot}yr^{-1}$로 산정되었다.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2008년도 학술발표회 논문집
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• pp.299-303
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• 2008

In this study, an uncertainty assessment for surface air temperature(T2m) and precipitation(PCP) over East Asia is carried out. The data simulated by the intergovermental Panel on Climate Change (IPCC) Fourth Assessment Report (AR4) Atmosphere-Ocean coupled general circulation Model (AOGCM) are used to assess the uncertainty. Examination of the seasonal uncertainty of T2m and PCP variabilities shows that spring-summer cold bias and fall warm bias of T2m are found over both East Asia and the Korea peninsula. In contrast, distinctly summer dry bias and winter-spring wet bias of PCP over the Korea peninsula is found. To investigate the PCP seasonal variability over East Asia, the cyclostationary empirical orthogonal function(CSEOF) analysis is employed. The CSEOF analysis can extract physical modes (spatio-temporal patterns) and their undulation (PC time series) of PCP, showing the evolution of PCP. A comparison between spatio-temporal patterns of observed and modeled PCP anomalies shows that positive PCP anomalies located in northeastern China (north of Korea) of the multi-model ensemble(MME) cannot explain properly the contribution to summer monsoon rainfalls across Korea and Japan. The uncertainty of modeled PCP indicates that there is disagreement between observed and MME anomalies. The spatio-temporal deviation of the PCP is significantly associated with lower- and upper-level circulations. In particular, lower-level moisture transports from the warm pool of the western Pacific and corresponding moisture convergence significantly contribute to summer rainfalls. These lower- and upper-level circulations physically consistent with PCP give a insight of the reason why differences between modeled and observed PCP occur.

• 대기
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• 제26권3호
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• pp.435-444
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• 2016

In spite of considerable progress in the recent decades, there still remain large uncertainties in numerical cloud models. In this study, effects of uncertainty in terminal velocity of graupel on cloud simulation are investigated. For this, a two-dimensional bin microphysics cloud model is employed, and deep convective clouds are simulated under idealized environmental conditions. In the sensitivity experiments, the terminal velocity of graupel is changed to twice and half the velocity in the control experiment. In the experiment with fast graupel terminal velocity, a large amount of graupel mass is present in the lower layer. On the other hand, in the experiment with slow graupel terminal velocity, almost all graupel mass remains in the upper layer. The graupel size distribution exhibits that as graupel terminal velocity increases, in the lower layer, the number of graupel particles increases and the peak radius in the graupel mass size distribution decreases. In the experiment with fast graupel terminal velocity, the vertical velocity is decreased mainly due to a decrease in riming that leads to a decrease in latent heat release and an increase in evaporative cooling via evaporation, sublimation, and melting that leads to more stable atmosphere. This decrease in vertical velocity causes graupel particles to fall toward the ground easier. By the changes in graupel terminal velocity, the accumulated surface precipitation amount differs up to about two times. This study reveals that the terminal velocity of graupel should be estimated more accurately than it is now.

• 한국수자원학회논문집
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• 제34권4호
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• pp.335-345
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• 2001

본 연구에서는 최근 들어 빈번해지고 잇는 기상이변들의 가장 큰 원인으로 지목 받고 잇는 지구온난화 현상이 한반도 수문환경의 변화에 끼치는 영향에 대한 분석을 시도하였다. 이를 위해 $CO_2$의 증가 시나리오에 따라 모의한 대기대순환모형(GCM) 모의 결과를 이용하여 대청댐 상류 유역의 강수량과 기온 변화에 따른 토양함수비, 증발산, 유출량 등의 변화를 물수지 모형을 이용하여 분석하였다. 이를 통해 $CO_2$배증에 따른 지구온난화 현상이 발생할 경우 강수량의 전반적인 증가 경향과 기온의 상승이 나타났으며, 잠재증발산량의 증가와 이로 인한 토양함수비의 감소 및 증발산량의 증가가 예측되었다. 또한, 대청댐 상류 유역의 유출량은 전반적으로 증가경향을 보였다. 그러나, 유출량의 계절적 변화는 여름과 가을의 증가 및 겨울의 감소가 뚜렷할 것으로 분석되어 가뭄과 홍수의 발생 가능성이 현재보다 높아질 것으로 예상되었다.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2018년도 학술발표회
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• pp.155-155
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• 2018

Uncertainty in flood forecasting using a coupled meteorological and hydrological model is arisen from various sources, especially the uncertainty comes from the inaccuracy of Quantitative Precipitation Forecasts (QPFs). In order to improve the capability of flood forecast, the uncertainty estimation and mitigation are required to perform. This study is conducted to investigate and reduce such uncertainty. First, ensemble QPFs are generated by using Monte - Carlo simulation, then each ensemble member is forced as input for a hydrological model to obtain ensemble streamflow prediction. Likelihood measures are evaluated to identify feasible member. These members are retained to define upper and lower limits of the uncertainty interval and assess the uncertainty. To mitigate the uncertainty for very short lead time, a blending method, which merges the ensemble QPFs with radar-based rainfall prediction considering both qualitative and quantitative skills, is proposed. Finally, blending bias ratios, which are estimated from previous time step, are used to update the members over total lead time. The proposed method is verified for the two flood events in 2013 and 2016 in the Yeonguol and Soyang watersheds that are located in the Han River basin, South Korea. The uncertainty in flood forecasting using a coupled Local Data Assimilation and Prediction System (LDAPS) and Sejong University Rainfall - Runoff (SURR) model is investigated and then mitigated by blending the generated ensemble LDAPS members with radar-based rainfall prediction that uses McGill algorithm for precipitation nowcasting by Lagrangian extrapolation (MAPLE). The results show that the uncertainty of flood forecasting using the coupled model increases when the lead time is longer. The mitigation method indicates its effectiveness for mitigating the uncertainty with the increases of the percentage of feasible member (POFM) and the ratio of the number of observations that fall into the uncertainty interval (p-factor).

• 한국물환경학회지
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• 제37권3호
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• pp.204-216
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• 2021

It is important to understand the factors influencing the temporal and spatial variability of water quality in order to establish an effective customized management strategy for contaminated aquatic ecosystems. In this study, the spatial diversity of the 5-year (2015 - 2019) average total phosphorus (TP) concentration observed in 40 Total Maximum Daily Loads unit-basins in the Nakdong River watershed was analyzed using 50 predictive variables of watershed characteristics, climate characteristics, land use characteristics, and soil characteristics. Cross-correlation analysis, a two-stage exhaustive search approach, and Bayesian inference were applied to identify predictors that best matched the time-averaged TP. The predictors that were finally identified included watershed altitude, precipitation in fall, precipitation in winter, residential area, public facilities area, paddy field, soil available phosphate, soil magnesium, soil available silicic acid, and soil potassium. Among them, it was found that the most influential factors for the spatial difference of TP were watershed altitude in watershed characteristics, public facilities area in land use characteristics, and soil available silicic acid in soil characteristics. This means that artificial factors have a great influence on the spatial variability of TP. It is expected that the proposed statistical modeling approach can be applied to the identification of major factors affecting the spatial variability of the temporal average state of various water quality parameters.

• 한국작물학회지
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• 제31권1호
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• pp.78-83
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• 1986

본 실험은 과맥에서 문제가 되고 있는 낮은 출현율의 원인을 구명하기 위하여 피주성 isogenic line을 육성 공시하여 발아 및 출현에 저해요인이 될 수 있는 수확기의 강우, 탈곡기회전수, 파종심도, 온도등을 달리하여 비교 검토한 바 다음과 같은 결과를 얻었다. 1. 수확 전일 강우시는 피성에 비하여 과성의 발아율이 4∼6 % 낮았으며, 5 일 인공강수처리에서는 과성의 발아율은 현저히 저하되었다. 2. 탈곡기회전수가 600rpm에서 1,000rpm 으로 상승할 때 피성의 발아율이 100 %에서 90%로 저하된 반면, 과성은 98%에서 76%로 발아율이 크게 저하되었다. 3. 과성에서 발아율보다 출현율이 피성에 비하여 큰 차이가 있었으며 파종심도가 깊을수록 그 차이가 컸다. 4. 파종심도, 고탈곡회전수, 수확시의 강우 순으로 피성보다 과성의 출현율을 크게 저하시켰다. 따라서 과맥을 육종할 때 출현율 및 유묘활력 향상을 위한 육종적 노력이 필요할 것으로 생각된다.

• 한국물환경학회지
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• 제23권3호
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• pp.339-347
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• 2007

Zooplankton community dynamics were studied after establishment of an artificial vegetation island (AVI) in Lake Paldang, from April 2005 to November 2006. There were distinct seasonal and inter-annual changes of total zooplankton abundance at the survey site. Total zooplankton abundance rapidly increased in spring and fall, while it remained low throughout winter. During summer, the dynamics of zooplankton community seemed to be largely affected by hydrological parameters such as, precipitation and inflow. Total zooplankton abundance and biomass below AVI was much higher than that of pelagic zone (L1) in Lake Paldang. Copepoda and cladocera represented the main bulk of the zooplankton community from summer to fall at the both sites. Copepods were more dominant at AVI area, while cladocera were more dominant at pelagic zone (L1). Water quality, prey and habitat condition, species competition between zooplankton seemed to play important roles in dominance of the copepoda and cladocera in zooplankton community at AVI area. Our results conclude that artificial vegetation island provide the stable habitat and besides phytoplankton, diverse food to zooplankton, and consequently influence the diversity and richness of zooplankton community.