• 대한지리학회지
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• 제48권1호
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• pp.19-36
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• 2013

이 연구에서는 지난 58년(1954~2011년) 동안의 관측 자료를 보유한 14개 기상관측소의 일평균 상대습도, 일평균 수증기압을 분석하여 도시 규모별 습도 변화를 파악하였다. 연평균 상대습도는 분석기간 동안 지속적으로 감소하는 경향이며, 도시에서 비도시보다 감소하는 경향이 뚜렷하다. 계절별로는 봄철과 겨울철에 상대습도가 감소하는 경향이 뚜렷하고, 여름철에는 변화율이 작다. 연평균 수증기압은 변화 경향이 뚜렷하지 않고, 도시 규모에 의한 변화율 차이가 명확하지 않다. 상대습도와 평균기온 사이에는 음의 관계가 있으며, 도시 규모에 따른 상대습도 차이가 통계적으로 유의하였다. 상대습도와 수증기압 사이에는 양의 관계가 있지만, 도시 규모에 따른 수증기압의 차이가 뚜렷하지 않다. 한국에서 상대습도가 감소하는 경향은 도시화에 의한 기온상승 경향과 상당히 일치하지만, 수증기압의 변화는 뚜렷하지 않다.

• 한국조경학회지
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• 제17권2호
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• pp.27-39
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• 1989

The purpose of this study is to prove the factors affecting the fluctuation of daily visitors in five mountainous national park(Kayasan, kyeryongsan, Naejangsan, Soraksan, Songnisan), and to analyze the relationship between these factors and daily visitors in Korea. "Three Factors and Nine Categories"(Aoki, K. & Aoki, Y. : 1974, 1979) has been applied to this study, and statistical analysis method was carried out by computer program SAS and SPSS. The number of daily visitors is calculated based on the data of "Daily entrance ticket sale report" by administration office in each national park. The scope of time period is during the last 5years(1982∼1986: 1825days) and the results were as follows: 1) There were significant differences in the number of daily visitors of each national park among months, days of a week and weather-the same as the previous study of urban park case. But it wold be better for their category classification to be adjusted according to the fluctuation pattern of each national park. 2) The peak of monthly visitors comes in May(Kayasan, Soraksan, Songnisan) or October(Kyeryongsan, Naejangsan). These months are specified as group tour season. On the basis of monthly fluctuation pattern, Each national park were classified into seasonal type, that is, kayasan, Soraksan were proved to be three-season type(Spring, Summer, Autumn), Songnisan to be two-season type(Spring, Autumn), and Naejangsan to be one-season type(Autumn). 3) The weekly pattern differs from three category (weekday, weekend, holiday: Eom, Choi 1986) in the case of urban park study. And there is no significant difference in daily fluctuation pattern by weather (fine, cloudy and rainy day), but significant difference between snowy and the others. This result is due to the characteristics of visitors, which is, the major visits of national park are planned in a advance of the tour, therefore it is difficult to change the plan by the weather. 4) the result of correlation analysis showed that the most influential factor on national park use in Kayasan, Naejangsan, Soraksan and Songnisan is ′Monthly characters (M)′, on the contrary ′Day of week(D)′ in Kyeryongsan only. From the result, The more parks are resource-based, the more ′Monthly characters′-factor is supposed to affect the number of daily visitors rather than ′Day of the week′-factor. This means that kayasan, naejangsan, Sorakson and Songnisan are classified into resource-based type, but on the other hand Kyeryongsan should be classified into intermediate type.

• 한국농림기상학회지
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• 제24권4호
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• pp.201-217
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• 2022

미국은 전 세계 주요 곡물(밀, 옥수수, 콩 등)의 생산 및 수출 국가로 알려져 있다. 따라서 신뢰할 만한 기상 예측 정보를 바탕으로 해당 지역에 대한 작황을 추정하는 것은 우리나라의 곡물 수급을 안정적으로 계획하기 위해서 중요하다. 본 연구에서는 지역 규모의 일 기온 및 이를 기반으로 산출되는 농업기후지수의 계절 예측성을 향상시키는 데 목적을 두었다. 이를 위해 먼저 역학적 규모축소법을 위한 지역기후모형으로 WRF가 사용되었으며, 해당 모형의 초기 및 측면 경계조건으로 PNU CGCM에서 생산된 시간 별 전지구 예측자료가 활용되었다. WRF의 적분은 22년(2000~2021년) 동안 매년 하반기를 포함하는 기간(6~12월)에 대해 수행되었다. 본 연구에서는 WRF에 의해 모의된 일 평균⋅최저⋅최고기온에 대해 EQM을 적용하여 모형이 갖는 편의를 보정하였다. EQM을 이용하여 보정된(보정되지 않은) 자료들은 WRF_C (WRF_UC)로 명명하였다. WRF_UC는 미국 내 대부분의 지역에서 일 최저기온(최고기온)을 과대(과소) 모의했는데, 이는 저온(고온) 범위를 과소 모의한 특징에서 비롯되었다. WRF_C는 WRF_UC에 나타난 일 평균⋅최저⋅최고기온의 편의가 감소하고 공간분포에 대한 예측성이 향상되었기 때문에 결과적으로 일 기온을 기반으로 산출되는 농업기후지수의 예측성 향상을 유도했다.

• 한국물환경학회지
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• 제27권3호
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• pp.273-285
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• 2011

This study describes the modeling of climate change impact on runoff across southeast Korea using a conceptual rainfall-runoff model TANK and assesses the results using the concept of environmental flows developed by International Water Management Institute. The future climate time series is obtained by scaling the historical series, informed by 4 global climate models and 3 greenhouse gas emission scenarios, to reflect a $4.0^{\circ}C$ increase at most in average surface air temperature and 31.7% increase at most in annual precipitation, using the spatio-temporal changing factor method that considers changes in the future mean seasonal rainfall and potential evapotranspiration as well as in the daily rainfall distribution. Although the simulation results from different global circulation models and greenhouse emission scenarios indicate different responses in flows to the climate change, the majority of the modeling results show that there will be more runoff in southeast Korea in the future. However, there is substantial uncertainty, with the results ranging from a 5.82% decrease to a 48.15% increase in the mean annual runoff averaged across the study area according to the corresponding climate change scenarios. We then assess the hydrologic perturbations based on the comparison between present and future flow duration curves suggested by IMWI. As a result, the effect of hydrologic perturbation on aquatic ecosystems may be significant at several locations of the Nakdong river main stream in dry season.

• 대기
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• 제32권1호
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• pp.1-15
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• 2022

Recently, Japan's Meteorological Research Institute presented the d4PDF database (Database for Policy Decision-Making for Future Climate Change, d4PDF) through large-scale climate ensemble simulations to overcome uncertainty arising from variability when the general circulation model represents extreme-scale precipitation. In this study, the change of precipitation characteristics between the historical and future climate conditions in the Yongdam-dam basin was analyzed using the d4PDF data. The result shows that annual mean precipitation and seasonal mean precipitation increased by more than 10% in future climate conditions. This study also performed an analysis on the change of the return period rainfall. The annual maximum daily rainfall was extracted for each climatic condition, and the rainfall with each return period was estimated. In this process, we represent the extreme-scale rainfall corresponding to a very long return period without any statistical model and method as the d4PDF provides rainfall data during 3,000 years for historical climate conditions and during 5,400 years for future climate conditions. The rainfall with a 50-year return period under future climate conditions exceeded the rainfall with a 100-year return period under historical climate conditions. Consequently, in future climate conditions, the magnitude of rainfall increased at the same return period and, the return period decreased at the same magnitude of rainfall. In this study, by using the d4PDF data, it was possible to analyze the change in extreme magnitude of rainfall.

• 한국수자원학회논문집
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• 제37권3호
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• pp.185-193
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• 2004

본 연구는 기후변화가 유역의 유출량과 수자원에 미치는 영향을 조사하고 평가하는데 목적이 있다. 이를 위하여 먼저, YONU GCM의 제한실험과 점증실험을 실시하여 전구적 규모의 기후변화 시나리오를 작성하였으며, 통계학적 축소기법과 추계학적 일기발생기법을 이용하여 대상지점의 일 수문기상 시계열을 모의하였다. 이렇게 얻은 시계열자료를 2CO2 상황에서의 유출량자료로 변환하기 위해 준 분포형 강우-유출 모형인 SLURP 모형에 입력하였다. 본 연구에서는 이 방법을 용담댐 유역에 적용하였으며, 그 결과, 기후변화시 연 평균 유출량의 경우 현재상황에 비해 약7.6％ 감소하는 것으로 모의되었으며, 계절적으로 볼 때 겨울철과 가을철에는 유출량이 증가하였으나 여름철에는 감소하였다. 그러나, 유출량의 계절적 패턴은 변화가 없는 것으로 모의되었다.

• 한국농림기상학회지
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• 제14권4호
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• pp.196-206
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• 2012

본 연구에서는 기후변화가 농업생태계 식물군락에 미치는 영향을 해석하기 위하여 기상요건이 다른 해남, 영동, 철원 3지역의 논둑에서 시기별로 식생변화를 조사하였다. 그 결과 출현종수에서 $C_3$식물은 해남과 영동에서는 이른 봄부터 5월 중순까지 증가하다가 $C_4$식물이 출현하는 이후부터 계속적으로 감소하였지만, 철원에서는 이른 봄부터 가을까지 계속적으로 증가하는 경향을 나타냈다. $C_4$식물은 해남과 영동에서는 6월 중순, 철원에서는 7월 하순에 출현하여 가을까지 계속적으로 증가하는 경향을 나타냈다. 종다양성의 계절변화에서 해남은 $C_4$식물이 출현하기 전에 가장 높은 값을 나타냈으며 이후에는 급격히 감소하였다. 영동은 $C_3$와 $C_4$식물이 혼생하는 초기에 가장 높은 값을 나타냈으며 이후에 서서히 감소하였다. 철원은 감소경향이 나타나지 않고 계속적인 증가 패턴을 나타냈다. 이들 논둑에 출현하는 식물을 $C_3$와 $C_4$ 두 그룹으로 나누어 상대피도 및 상대우점율의 계절변화를 확인한 결과 지역별 차이를 나타내기는 하지만 $C_3$식물에서 $C_4$식물로 교대가 나타나는 것을 확인할 수 있었다. 이러한 교대시기를 온도와 일조시간을 고려한 관계식을 이용하여 추정할 수 있었으며, 일평균기온 5 이상인 날에 대한 일조시간의 누적 합이 1017시간에서 논둑식생의 상대우점율이 $C_3$식물에서 $C_4$식물로 교대하는 것으로 예측했다. 이러한 연구결과는 기후변화에 따른 국내 식생분포의 예측에도 중요한 기초자료로 활용될 수 있을 것으로 판단된다.

• Journal of Ecology and Environment
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• 제42권2호
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• pp.77-84
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• 2018

Background: For understanding and evaluating a more realistic and accurate assessment of ecosystem carbon balance related with environmental change or difference, it is necessary to analyze the various interrelationships between soil respiration and environmental factors. However, the soil temperature is mainly used for gap filling and estimation of soil respiration (Rs) under environmental change. Under the fact that changes in precipitation patterns due to climate change are expected, the effects of soil moisture content (SMC) on soil respiration have not been well studied relative to soil temperature. In this study, we attempt to analyze relationship between precipitation and soil respiration in temperate deciduous broad-leaved forest for 2 years in Gwangneung. Results: The average soil temperature (Ts) measured at a depth of 5 cm during the full study period was $12.0^{\circ}C$. The minimum value for monthly Ts was $-0.4^{\circ}C$ in February 2015 and $2.0^{\circ}C$ in January 2016. The maximum monthly Ts was $23.6^{\circ}C$ in August in both years. In 2015, annual precipitation was 823.4 mm and it was 1003.8 mm in 2016. The amount of precipitation increased by 21.9% in 2016 compared to 2015, but in 2015, it rained for 8 days more than in 2016. In 2015, the pattern of low precipitation was continuously shown, and there was a long dry period as well as a period of concentrated precipitation in 2016. 473.7 mm of precipitation, which accounted for about 51.8% of the precipitation during study period, was concentrated during summer (June to August) in 2016. The maximum values of daily Rs in both years were observed on the day when precipitation of 20 mm or more. From this, the maximum Rs value in 2015 was $784.3mg\;CO_2\;m^{-2}\;h^{-1}$ in July when 26.8 mm of daily precipitation was measured. The maximum was $913.6mg\;CO_2\;m^{-2}\;h^{-1}$ in August in 2016, when 23.8 mm of daily precipitation was measured. Rs on a rainy day was 1.5~1.6 times higher than it without precipitation. Consequently, the annual Rs in 2016 was about 12% higher than it was in 2015. It was shown a result of a 14% increase in summer precipitation from 2015. Conclusions: In this study, it was concluded that the precipitation pattern has a great effect on soil respiration. We confirmed that short-term but intense precipitation suppressed soil respiration due to a rapid increase in soil moisture, while sustained and adequate precipitation activated Rs. In especially, it is very important role on Rs in potential activating period such as summer high temperature season. Therefore, the accuracy of the calculated values by functional equation can be improved by considering the precipitation in addition to the soil temperature applied as the main factor for long-term prediction of soil respiration. In addition to this, we believe that the accuracy can be further improved by introducing an estimation equation based on seasonal temperature and soil moisture.

• Ocean and Polar Research
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• 제31권1호
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• pp.71-76
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• 2009

Drastic changes in the water quality and phytoplankton community of the new Saemankeum Lakeduring the first decade following the construction of the Saemankeum Sea Wall has been considered to be unavoidable. Input of eutrophicated water through the Mankyeong River and Dongjin River might produce more direct effects on the water quality and phytoplankton community, which lead us to launch a long-term semi-weekly investigation at the "Mankyeong Bridge" monitoring point to resolve its short-term effect as well as long-term stabilization of the ecosystem in the new Saemankeum Lake. During 15 months starting from June 2006, the water temperature varied in accordance with the typical seasonal variations in temperate on the coasts, and no significant daily variations evoked by tidal cycle could be detected. However, there was an inverse relationship between seasonal precipitation and salinity even though the range in annual variation was drastically reduced right after the construction of the Saemankeum Sea Wall. Species richness in the phytoplankton community was also reduced due to the narrowed annual range of salinity, which would eliminate the mid-high salinity species from the Mankyeong Bridge monitoring point. Similarly, species diversity was decreased with increased dominance of the phytoplankton community after the construction. Between the two summer seasons during the present study, species diversity was higher in 2007 than in 2006, which might indicate the early stage of a gradual stabilization in the ecosystem including the phytoplankton community at the monitoring station. The phytoplankton community thus needs to be monitored on a long-term basis to identify indirect signals that can be used to assess the stability of the ecosystem in the young Saemankeum Lake.

• Journal of Ginseng Research
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• 제7권2호
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• pp.172-192
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• 1983

Light environment and growth of Panax ginseng In habitat and cultivation under natural shade were renewed. Grower's experiences on ginseng stand In relation to light environment were assessed. Change of shading method and grower's concepts on light requirement of ginseng plant in Korea, Manchuria and Japan was counted. Growth of wild ginseng was better under rich light. Optimum crown density index appeared to be 0.7 In natural habitat and 0.4 to 0.7 for the cultivation in forest. Change of light Intensity in forest was greatest in May and reached near to constant value (from 40% to 3% for broad leaf deciduous forest and loom 4% to 2% for pine forest). Insufficient light condition induced long and thin stem, poor flowering and seed bearing, and sequent dormancy. Relation between light and ginseng strand was not clear but light Interception with cool weather was effective. Topography and orientation of bed have been deeply considered for light environment. Panel or bark of won were used for shading in deep forest manly In Manchuria while reed blind and straw thatch were used in Korea. Kinds and number of shades material and seasonal or daily schedule have been simplified probably by labor pressure due to eulargement of plantation. Post height has been greater while width of roof, bed and ditch has changed lisle. Scientific survey in the past omitted important light control methods (complete light hardening etc) which has been practiced in specific areas. The concept and technique of light control in the past in Korea were delicate and intensive including the control of temperature and moisture. For the application of old concept in modem cultivation precise Investigation of the technique including the measurement of light, temperature and moisture is needed.