• Korean Journal of Agricultural and Forest Meteorology
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• v.3 no.1
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• pp.44-54
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• 2001

This study was conducted to estimate microclimate of natural deciduous forest in national forest of Pyungchang, Kangwon province and to investigate the effects of the microclimatic conditions on the periodic annual increment of diameter by site types. In this study, site was first classified by nine types considering both elevation (higher than 1,000 m, 700∼1,000 m, and lower than 700 m) and topographical conditions (ridge, slope and valley). For each of site types, diameter growth was measured by using increment borer and periodic annual increment of diameter was then analyzed. A topoclimatological technique, for estimating microclimatic conditions, which make use of empirical relationships between the topographical factor and the climatic normals in the study area was applied to produce monthly mean, maximum and minimum temperatures, relative humidity, precipitation and hours of sunshine. From these monthly estimtes, 17 weather variables such as warmth index, coldness index, index of aridity etc. which affect the diameter growth were computed for each of site types. The periodic annual increment of diameter was then correlated with and regressed on the 17 weather variables to examine effects of microclimatic conditions on the diameter growth by site types. From the correlation analysis, it was found that the diameter growth by site types was positively correlated with all of 17 weather variables except the warmth index. Especially, the conditions such as high relative humidity and large amount of sunshine hours provide favorable environment for the growth of diameter. On the other hand, it was also found that diameter growth was negatively iufluenced by warmth index. According to the regression analysis, the periodic annual increment of diameter could be well predicted by index of aridity and mean relative humidity for the growing season.

• Journal of the Korean Association of Geographic Information Studies
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• v.19 no.1
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• pp.154-166
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• 2016

This study aims to contribute to better understanding the effects of the changes in the parameter values of GroundFilter algorithm(GF), which performs filtering process, and of GridsurfaceCreate algorithm(GC), which creates regular grid, provided in Fusion software on the accuracy of elevation of the final LiDAR-DEM products through comparative analysis. In order to test whether there are significant effects on the accuracy of the final LiDAR-DEM products due to the changes of GF(1, 3, 5, 7, 9) parameter levels and GC(1, 3, 5, 7, 9) parameter levels, two-way ANOVA is conducted based on residuals. The residuals are calculated using the differences between each sample plot's paired field-measured and DEM-derived elevation values given each individual GF and GC level. After that, Tukey HSD test is conducted as a post hoc test for grouping the levels. As a result of two-way ANOVA test, it is found that the change in the GF levels significantly affects the accuracy of LiDAR-DEM elevations(F-value : 27.340, p < 0.01), while the change in the GC levels does not significantly affect the accuracy of LiDAR-DEM elevations(F-value : 0.457). It is also found that the interaction effect between GF and GC levels is not likely to exist(F-value : 0.247). From the results of the Tukey HSD test in the GF levels, GF levels can be divided into two groups('7', '5', '9', '3' vs '1') by the differences of means of residuals. Given the current conditions, LiDAR-DEM can achieve the best accuracy when the level '7' and '3' are given as GF and GC level, respectively.

• The Korean Journal of Quaternary Research
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• v.12 no.1
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• pp.17-30
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• 1998

연구지역인 대관령 서쪽 산지 사면은 진부에서 동쪽으로 고속도로를 따라 약 21km 떨어진 대관령까지이며 해발고도는 500∼900m 지형경사는 3.3%이다. 1989년 5월∼1992년 5 월에 진부에서 대관령 쪽으로 영동고속도로를 따라 진부(고도 544m) 간평기(고도 576m) 유 천리(고도 600m) 싸리재(고도800m) 대관령(고도 842m)등의 5개지점을 정하여 일 강수량을 측정하였다 각 고도별 일 강수량 자료를 기초로 한반도의 지상 기압배치형에 따른 대관령 서쪽 산지의 고도별 강수량 분포의 특성을 고찰하였다,. 이결과를 용약하면 다음과 같다. 총 강수일 258일을 지상 기압배치형(기압골, 저기압, 시베리아고기압, 장마전선, 고기압, 태풍, 오호츠크해고기압)에 따라 7가지 형으로 분류하였다, 이들중 기압골이 나타난 날이 113일로 제일 많고 오호츠크해고기압이 나타난 날은 8일로 가장적었다. 고도별 일평균 강수량은 태 풍이 나타났을 때 17,5∼54,4mm로 제일많았고 시베리아고기압이 나타났을 때는 5.9∼ 19.8mm로 제일 적었다, 대관령 서쪽 산지 사면에서 강수량이 제일 많은 고도는 대관령이고 제일적은 고도는 간평리이다, 태풍과 오호츠크해고기압이 출현한 경우는 고도가 증가할수록 강수량도 많아졌다. 간평리와 대관령 고도의 강수량 분포에 관한 사례분석(1989.5∼1991.12) 에서 기압골, 저기압, 장마전선등이 나타난 36일 시베리아고기압이 나타난 1일은 간평리가 대관령보다 강수량이 많았다.

• The Hankook-Saengyark Bo
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• no.248
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• pp.5-5
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• 2001

송이 인공재배 길 열었다(경북도 산림환경연구소, 기술특허출원) - 새 '동충하초' 개발 - 상황버섯 톱밥재배법 개발 - 파주 '장단인삼' 특산명품 추진

• Journal of the Speleological Society of Korea
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• v.2 no.2
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• pp.14-17
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• 1976

본논문은 전국 처처에 분포하는 천여개소의 석화암 용식지형중에서도, 해발고도가 가장 얄고, 해안에서의 거리가 제일 가까운 위치에 발달한 선유산지괴의 지표면 Karst cycle에 대하여 고찰하고, 발달과정과 인문 관계를 밝히는데 목적을 두었다. (중략)

• Journal of the Korean Geographical Society
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• v.38 no.4
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• pp.490-504
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• 2003

The existence of coastal terraces, HH(High higher) surfaces found at Gampo of southeast coast and at Jeongdongjin of the central east coast were confirmed at Jjgyeong-Ri, the areal border between Gyeongjuand Ulsan city on the southeast coast of Korea Peninsula. Especially this study reports HH JK-surface located on the 155m a.s.l, which is the highest altitude among the ancient shorelines of the coastal terraces in Korea. The HH surfaces on the study area are classified into HH JK at 155m, HH I at 140m and HH II at 115m, and each formation stage is related to MIS 17(720∼690ka BP), MIS 15(630∼560ka BP) and MIS 13(510∼480ka BP) respectively. The HH-surfaces remain to be larger than those of H- and L-surfaces. The reason is caused by the unique factors of the coastal geology and morphology on the study area during the formation stage. And also the areal difference by the magnitude of upheaval doesn't exist from north to south because the altitude system of ancient shoreline on each coastal terrace is same along the east coast. The upheaval rate of the eastern coastal areas was measured in the relation to the ancient shoreline and formation stage among the coastal terraces such as HH JK-, HH I-, HH II, H I- and H II surface, and was almost same as 0.23mm/y.

• Journal of the Korean Association of Geographic Information Studies
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• v.20 no.4
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• pp.139-151
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• 2017

The habitat preference of roe deers(Capreolus pygargus) in Jeju island, South Korea was analyzed by using their occurrence probability in MaxEnt model in this study. Totally 490 surveying data were gathered and 15 environmental variables were chosen for the model in which 6 variables out of 15 ones were filtered and finally removed because of there being higher correlation(over 0.7 in correlation coefficient). According to the modeling, roe deers were known to prefer the area ranging from 200 to 700 meter and over 1,500 meter in sea level, where there were not many dominant tree and/or dominant vegetation with low density so that understory vegetation can grow well with plentiful sunlight and can be used as a food of herbivore like roe deers. Otherwise, the region ranging from 700 to 1,500 meter was mostly covered with high density vegetation which cut off sunlight trying to penetrate through the dominant vegetation. It can cause a lower density of vegetation on surface, which can not attract to roe deers.

• Korean Journal of Agricultural and Forest Meteorology
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• v.5 no.4
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• pp.238-246
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• 2003

This study evaluated forest vegetation structure according to elevation in Mt. Sokri and Odae. The dominance of Pinus densiflora, Quercus variabilis, Quercus serrata, Prunus serrulata var. spontanea was apparent at elevations below 500 m. Quercus mongolica, Fraxinus sieboldiana, Acer pseudo-sieboldianum and Symplocos chinensis for. pilosa were conspicuous above 800 m. Significant P. densiflora, Rhus trichocarpa, Lindera obtusiloba and P. serrulata var. spontanea populations appeared below 700 m elevation in Mt. Odae. Q. mongolica, F. sieboldiana, A. pseudo-sieboldianum, Tilia amuresis, Abies holophylla, Carpinus cordata, Betula costata, Kalopanax pintus and Pinus koraiensis were conspicuous at elevations 1000 m and above. P. densiflora, Q. monoglica, Q. serata, R. trichocarpa and L. obtusiloba populations were significant at elevations below 700 m. Q. mongolica, F. sieboldiana, A. pseudo-sieboldianum, T. amurensis, A. holophylla, C. cordata appeared at elevations above 1000 m.

• Proceedings of the Korean Environmental Sciences Society Conference
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• 2008.11a
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• pp.562-564
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• 2008

• Journal of the Speleological Society of Korea
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• v.33 no.34
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• pp.23-29
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• 1993

온달굴은 충청북도 단양군 영춘면 하리에 소재하며 남한강이 서남류하여 굽이치는 남안의 남산 기음에 위치한다. 이 남산은 서남쪽에 하리와 박자리의 경계를 이루고 있는 남한강변에 우뚝솟은 해발고도 427m 성산의 기슭에 해당하는 구릉봉으로 석회암 지대의 산지지형인 급경사의 산세를 이루고 있다. 영춘지역의 남산 산마루를 따라 성산으로 오르면 산정 부근에서 능선을 따라 그 유명한 성산고성이 축조되어 있다. 이것이 현재 온달성으로 불리우고 있는 고성이다.(중략)