• 한국관개배수논문집
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• 제21권1호
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• pp.89-98
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• 2014

This study is to evaluate the future potential impact of climate change on soil erosion loss in a metropolitan area using Revised Universal Soil Loss Equation(RUSLE) with land use information of the Ministry of Environment and rainfall data for present and future years(30-year period). The spatial distribution map of vulnerable areas to soil erosion was prepared to provide the basis information for soil conservation and long-term land use planning. For the future climate change scenario, the MIROC3.2 HiRes A1B($CO_2720ppm$ level 2100) was downscaled for 2040-2069(2040s) and 2070-2099(2080s) using the stochastic weather generator(LARS-WG) with average rainfall data during past 30 years(1980-2010, baseline period). By applying the climate prediction to the RUSLE, the soil erosion loss was evaluated. From the results, the soil erosion loss showed a general tendency to increase with rainfall intensity. The soil loss increased up to 13.7%(55.7 ton/ha/yr) in the 2040s and 29.8%(63.6 ton/ha/yr) in the 2080s based on the baseline data(49.0 ton/ha/yr).

• 한국농림기상학회지
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• 제22권4호
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• pp.250-257
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• 2020

본 연구에서는 포도의 생육과 관련된 연평균기온, 생육기 기온, 성숙기 기온, 극최저기온, 저온요구도, 강수량과 같은 기후인자와 심토토성, 침식정도, 배수 등급, 유효토심, 경사도, 자갈함량, 지형과 같은 토양 인자를 선정하여 기후와 토양의 조건을 최대저해인자법을 이용해 통합한 재배적지 구분 연구를 수행하였다. 재배적지는 적지, 가능지, 저위생산지&부적지의 3단계로 구분하였으며, 연구결과는 전국 면적을 기준으로 적지가 3.43%로 나타났고, 가능지는 10.61%로 나타났다. 지역별로 적지는 경상북도가 1.15%로 가장 넓은 것으로 나타났고, 충청남도가 0.72%와 충청북도가 0.44%로 나타났다. 가능지는 경상북도가 2.67%로 가장 넓었으며, 충청남도가 2.11%, 전라남도가 1.54%인 것으로 나타났다.

• 한국농림기상학회지
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• 제18권3호
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• pp.127-134
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• 2016

사과 및 배의 재배적지 구분을 토양환경정보시스템을 통한 토양조건에 의한 재배적지값과 국립원예특작과학원에서 제작한 미래 상세 전자기후도 제공 시스템을 통한 기후조건에 의한 재배적지값을 최대저해인자법을 이용하여 통합된 적지 구분을 하였다. 사과 및 배 모두에서 통합된 적지구분은 토양의 적지 구분의 패턴과 상당히 유사하였다. 기후조건에 의거한 구분도에 비해서 토양조건에 의한 구분도가 전체적으로 상대적으로 적지의 등급이 낮은 것이 그 이유로 여겨진다. 토양조건에 있어서 적지등급을 결정하는 최종구간 값들이 상당히 높게 형성되어 있어 전체적으로 등급이 낮게 결정된 것으로 사료되어 최종구간값들의 정확도에 대한 보정이 요구된다. 최대저해인자법은 이렇게 하나의 인자의 값들이 저평가되었을 때, 그 값들이 대표화되어 전체적으로 등급의 영향을 미치는 단점을 가지고 있다고 여겨진다. 세부적 인자에 대한 최대저해인자법의 적용 및 계층분석방법(Analytic Hierarchy Process, AHP) 등의 다양한 방법론과 토양 및 기후의 세부적 요소에 근거한 실제 단위면적 당 생산량 혹은 경제적 수익 등의 실제 현장관측값들과의 보정을 통해 재배적지구분의 정확도 및 정보의 실효성을 높일 수 있을 것으로 사료된다.

• 대한원격탐사학회지
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• 제32권4호
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• pp.383-401
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• 2016

In this paper, we described the statistical modeling of crop yields using satellite images, climatic datasets, soil property maps, and fertilizer data for the Midwestern United States during 2001-2012. Satellite images were obtained from the Moderate Resolution Imaging Spectroradiometer (MODIS), and climatic datasets were provided by the Parameter-elevation Regressions on Independent Slopes Model (PRISM) Climate Group. Soil property maps were derived from the Harmonized World Soil Database (HWSD). Our multivariate regression models produced quite good prediction accuracies, with differences of approximately 8-15% from the governmental statistics of corn and soybean yields. The unfavorable conditions of climate and vegetation in 2012 could have resulted in a decrease in yields according to the regression models, but the actual yields were greater than predicted. It can be interpreted that factors other than climate, vegetation, soil, and fertilizer may be involved in the negative biases. Also, we found that soybean yield was more affected by minimum temperature conditions while corn yield was more associated with photosynthetic activities. These two crops can have different potential impacts regarding climate change, and it is important to quantify the degree of the crop sensitivities to climatic variations to help adaptation by humans. Considering the yield decreases during the drought event, we can assume that climatic effect may be stronger than human adaptive capacity. Thus, further studies are demanded particularly by enhancing the data regarding human activities such as tillage, fertilization, irrigation, and comprehensive agricultural technologies.

• 한국농공학회논문집
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• 제61권1호
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• pp.1-8
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• 2019

Developing reliable soil moisture prediction techniques at agricultural regions is a pivotal issue for sustaining stable crop productions. In this study, a physically-based SWAP(Soil-Water-Atmosphere-Plant) model was suggested to estimate soil moisture dynamics at the study sites. ROSETTA was also integrated to derive the soil hydraulic properties(${\alpha}$, n, ${\Theta}_r$, ${\Theta}_s$, $K_s$) as the input variables to SWAP based on the soil information(Sand, Silt and Clay-SSC, %). In order to predict the soil moisture dynamics in future, the mid-term TIGGIE(THORPEX Interactive Grand Global Ensemble) and long-term S2S(Subseasonal to Seasonal) weather forecasts were used, respectively. Our proposed approach was tested at the six study sites of RDA(Rural Development Administration). The estimated soil moisture values based on the SWAP model matched the measured data with the statistics of Root Mean Square Error(RMSE: 0.034~0.069) and Temporal Correlation Coefficient(TCC: 0.735~0.869) for validation. When we predicted the mid-/long-term soil moisture values using the TIGGE(0~15 days)/S2S(16~46 days) weather forecasts, the soil moisture estimates showed less variations during the TIGGE period while uncertainties were increased for the S2S period. Although uncertainties were relatively increased based on the increased leading time of S2S compared to those of TIGGE, these results supported the potential use of TIGGE/S2S forecasts in evaluating agricultural drought. Our proposed approach can be useful for efficient water resources management plans in hydrology, agriculture, etc.

• Journal of Animal Science and Technology
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• 제63권2호
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• pp.339-353
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• 2021

This study aimed to assess the causality of different climate variables on the production of whole crop maize (Zea mays L.; WCM) in the central inland region of the Korea. Furthermore, the effect of these climate variables was also determined by looking at direct and indirect pathways during the stages before and after silking. The WCM metadata (n = 640) were collected from the Rural Development Administration's reports of new variety adaptability from 1985-2011 (27 years). The climate data was collected based on year and location from the Korean Meteorology Administration's weather information system. Causality, in this study, was defined by various cause-and-effect relationships between climatic factors, such as temperature, rainfall amount, sunshine duration, wind speed and relative humidity in the seeding to silking stage and the silking to harvesting stage. All climate variables except wind speed were different before and after the silking stage, which indicates the silking occurred during the period when the Korean season changed from spring to summer. Therefore, the structure of causality was constructed by taking account of the climate variables that were divided by the silking stage. In particular, the indirect effect of rainfall through the appropriate temperature range was different before and after the silking stage. The damage caused by heat-humidity was having effect before the silking stage while the damage caused by night-heat was not affecting WCM production. There was a large variation in soil surface temperature and rainfall before and after the silking stage. Over 350 mm of rainfall affected dry matter yield (DMY) when soil surface temperatures were less than 22℃ before the silking stage. Over 900 mm of rainfall also affected DMY when soil surface temperatures were over 27℃ after the silking stage. For the longitudinal effects of soil surface temperature and rainfall amount, less than 22℃ soil surface temperature and over 300 mm of rainfall before the silking stage affected yield through over 26℃ soil surface temperature and less than 900 mm rainfall after the silking stage, respectively.

• 생태와환경
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• 제56권4호
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• pp.440-448
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• 2023

This study measured soil respiration in pine forests dominated by Pinus densiflora in Mt. Jeombong, Mt. Namsan, Mt. Jirisan in Republic of Korea from 2009 to 2010. The seasonal variations, along with temperature and soil moisture content, were measured to understand the characteristics at each site. Soil respiration was highest in summer and autumn, closely influenced by the increase in soil temperature. Throughout the measurement period, soil respiration ranged from 205.6 to 312.2 mg CO₂ m^-2 h^-1, with Mt. Namsan showing the highest values and Mt. Jirisan the lowest. A strong correlation was observed between soil respiration and soil temperature, with Q₁₀ values ranging from 2.5 to 3.0. Precipitation significantly affected soil moisture content, and although it appeared to influence soil respiration, no significant correlation was found.

• 한국물환경학회지
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• 제25권6호
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• pp.821-831
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• 2009

The study was aimed to assess the expected impact of climate change on the water cycle and soil losses in Daecheong Reservoir watershed, Korea using the Soil and Water Assessment Tool (SWAT) that was validated for the watershed in a previous study. Future climate data including precipitation, temperature and humidity generated by introducing a regional climate model (Mesoscale Model Version 5, MM5) to dynamically downscale global circulation model (European Centre Hamburg Model Version 4, ECHAM4) were used to simulate the hydrological responses and soil erosion processes in the future 100 years (2001~2100) under the Special Report on Emissions Scenario (SRES) A1B. The results indicated that the climate change may increase in the amount of surface runoff and thereby sediment load to the reservoir. Spatially, the impact was relatively more significant in the subbasin Bocheongcheon because of its lower occupation rate of forest land compared to other subbasins. Seasonally, the increase of surface runoff and soil losses was more significant during late summer and fall season when both flood control and turbidity flow control are necessary for the reservoir and downstream. The occurrence of extreme turbidity flow events during these period is more vulnerable to reservoir operation because the suspended solids that remained water column can be resuspended by vertical mixing during winter turnover period. The study results provide useful information for the development of adaptive management strategy for the reservoir to cope with the expected impact of future climate change.

• The Korean Journal of Ecology
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• 제23권2호
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• pp.117-123
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• 2000

Changing patterns and the possibility of climate change in the area of Cheiudo island, the southernmost Island in Korea, were analyzed using daily temperature and Precipitation data observed at the Cheiu Regional Meteorological Office from May 1923 to December 1998. A hydrologic simulation model "BROOK" was used to simulate and analyze the dynamics of daily soil moisture content and soil moisture deficit by applying the daily weather data. During the period, significantly increasing pattern was observed in temperature data of both annual and monthly basis, while no significantly changing pattern was observed in precipitation data. During the last 76 years. mean annual temperature was observed to have risen about 1.4$^{\circ}C$, which may show the Possibility of the initiation of climate change on the island whose validity should be tested in future studies after long-term studies on temperature. Based on the simulation, due to increased temperature, significant increase was predicted in evapotranspiration. while no significant decrease was detected in simulated soil moisture content during the period. Changing pattern of annual soil moisture content was markedly different from those of precipitation. In some dominant trees, negative effects of the drought of the late season for the previous year were shown to be statistically significant to radial growth of the tree for the current year. As annual variation of radial growth of trees is mainly affected by the soil moisture content. the information on the dynamics of soil moisture deficit possibly provides us with useful information for the interpretation of tree growth decline on the mountain. mountain.

• 생태와환경
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• 제56권4호
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• pp.330-338
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• 2023

산림 사업이 산림의 탄소저장량에 미치는 영향을 알아보기 위하여 임상도, 산림사업 정보 및 토양 정보 등을 활용하여 산림 사업 전후의 지상부 및 토양의 탄소저장량을 산정하고 그 변화를 분석하고자 하였다. 먼저 임상도 정보에 기초하여 면적이 넓고 영급이 감소하는 도엽 6곳을 선정하였다. 그리고 임상도와 생장계수, 산정 지역의 토양유기물함량, 토양용적밀도 등 데이터를 수집하여 산림 탄소저장량을 산정하였다. 그 결과 모든 곳에서 산림 탄소저장량은 산림사업 후 약 34.1~70.0%가 감소하였다. 그리고 기존 연구와 비교했을 때 국내 산림 토양은 지상부에 비해 더 적은 탄소를 저장하고 있어 우리나라의 산림 토양은 더 많은 탄소를 저장할 수 있는 잠재성이 큰 것으로 판단되며 탄소저장량 증대를 위한 전략이 필요할 것으로 판단되었다. 산림사업이 없을 때 있을 때보다 탄소저장량은 약 1.5배 많은 것으로 추정되었다. 그리고 본 연구에서 산림사업에 따라 간벌 전 산림 탄소저장량으로 회복되기까지 약 27년이 걸리는 것으로 추정되었다. 산림은 물리적 훼손에 의해 탄소저장량이 감소하면 원래의 탄소저장량으로 회복되기까지 오랜 시간이 걸리므로 특히 자연성이 높은 산림은 최대한 보전하는 계획을 수립하여 산림의 탄소저장 기능을 유지할 수 있도록 하여야 할 것이다.