• 한국환경과학회지
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• 제8권5호
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• pp.633-637
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• 1999

A series of meterological observation using automation weather station(AWS) carried out to investigate characteristics of nocturnal meteorological parameters for 16~17 June 1998 at Buljeongdong mountain slope, Kyungbuk. Dry temperature at valley was lower than mountain because of high lapse rate at valley, so the strong inversion layer occurrenced at mountain slope for nighttime. Contrary of dry temperature, relative humidity of valley was higher than mountain for nighttime. Wind speed at valley from sunset to next day morning was lower than mountain, but that of valley after sunrise was higher than mountain. Wind direction at valley for all observation time were southeasterlies(SE), that of mountain for nighttime were northeasterlies(NE) or northnorthwesterlies(NNW), and that of mountain after sunrise were irregular. Vapor pressure at valley for all observation time was higher mountain, particularly the difference was high for nighttime.

• 지질공학
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• 제27권2호
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• pp.125-132
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• 2017

우리나라는 국토의 64% 가량이 산지로 되어 있어 하절기 집중호우 및 태풍으로 인해 지속적인 산지재해(사면붕괴, 산사태, 토석류 등)가 발생하고 있다. 이러한 산지를 중심으로 사회기반시설의 개발 및 확충을 통해 산지 개발이 이루어지고 있으나 체계적인 관리는 미흡한 실정이다. 산지사면을 대상으로 임도시설의 개설은 대상 산지를 인위적으로 변화시킴에 따라 하절기에 집중적으로 산지재해 발생의 원인으로도 작용한다. 이처럼 불안정한 상태의 산지환경에서 재해에 강한 환경을 건설하기 위한 노력이 절실히 요구되는 시점이다. 본 연구는 자연산지와 산지 내 임도 개설 여부를 기준으로 극한강우 조건하에서 강우의 침투특성을 고려하여 토층심도(1~5 m) 및 산지경사($20{\sim}60^{\circ}$) 조건에 따른 산지사면의 안정성을 분석하였다. 그 결과, 산지사면의 안정성은 토층심도와 토층의 포화면적에 따라 안전율의 차이를 갖는 것으로 나타났으며, 산지 내 임도 개설에 따른 산지의 안정성이 자연산지보다 낮은 것으로 분석되었다. 특히, 강우 침투양상의 경우에는 임도 상부측 사면부에서 강우 침투수의 유출이 발생하는데 이는 토층심도가 낮을수록 유출 현상이 뚜렷이 발생하는 것으로 나타났다.

• 대한공간정보학회지
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• 제17권2호
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• pp.81-90
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• 2009

등산로는 시민들의 건강과 일상생활에 있어서 매우 중요한 역할을 하며, 여가선용의 중요한 공간이 되고 있다. 그런 측면에서 관리자는 건강증진과 야외생활에 대한 욕구를 갖고 있는 등산객을 만족시키기 위해 노력하고 있다. 본 연구에서는 휴대용GPS를 이용하여 도시 근교에 있는 등산로의 경사를 분석하고 시민의 건강증진을 위해 적합한 등산로를 제시하는데 연구 목적을 두고 있다. 그 결과 휴대용GPS에 의한 등산로 경사분석이 산책 난이도를 평가하는데 효과적임을 제시하였다.

• 한국환경과학회지
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• 제11권9호
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• pp.865-880
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• 2002

As prevailing synoptic scale westerly wind blowing over high steep Mt. Taegulyang in the west of Kangnung coastal city toward the Sea of Japan became downslope wind and easterly upslope wind combined with both valley wind and sea breeze(valley-sea breeze) also blew from the sea toward the top of the mountain, two different kinds of wind regimes confronted each other in the mid of eastern slope of the mountain and further downward motion of downlsope wind along the eastern slope of the mountain should be prohibited by the upslope wind. Then, the upslope wind away from the eastern slope of the mountain went up to 1700m height over the ground, becoming an easterly return flow in the upper level of the sea. Two kinds of circulations were detected with a small one in the coastal sea and a large one from the coast toward the open sea. Convective boundary layer was developed with a thickness of about 1km over the ground in the upwind side of the mountain in the west, while a thickness of thermal internal boundary layer(TIBL) form the coast along the eastern slope of the mountain was only confined to less than 200m. After sunset, under no prohibition of upslope wind, westerly downslope wind blew from the top of the mountain toward the coastal basin and the downslope wind should be intensified by both mountain wind and land breeze(mountain-land breeze) induced by nighttime radiative cooling of the ground surfaces, resulting in the formation of downslope wind storm. The wind storm caused the development of internal gravity waves with hydraulic jump motion bounding up toward the upper level of the sea in the coastal plain and relatively moderate wind on the sea.

• 한국컴퓨터정보학회논문지
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• 제28권10호
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• pp.103-111
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• 2023

산악지대, 특히 오픈스페이스에서의 보행은 산악지형을 기반으로 이루어지는 특수 활동영역에서 중요하다. 그러나 최근의 보행 경로 연구는 보행자와 환경 요소를 포괄적으로 네트워크 분석에 포함시키지만, 주로 한정된 공간을 대상으로 하며 산악지형 등, 데이터가 부족한 지형은 분석 대상에서 제외된다. 본 논문에서는 산악지형의 오픈스페이스에서 그물망 기반의 가상 보행 네트워크를 만들며, 경사도를 반영한 산악 보행 경로 생성 방법을 제안한다. 이 방법은 거리측정에 경사도를 고려하여 실제 지형을 더 잘 반영하며, 기존 경로 분석 서비스에서 제공하지 않는 오픈스페이스를 이용한 산악 보행 경로를 제시하고, 시험을 통해 이를 입증하였다. 본 논문의 설계 방법은 조난, 산악구조, 전술 훈련 등에서 산악지형의 오픈스페이스를 포함한 경로 생성 방법으로 활용될 수 있을 것으로 기대한다.

• 한국초지조사료학회지
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• 제10권3호
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• pp.137-140
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• 1990

본 연구는 山地草地에 있어서 사경方向과 海技標高가 牧草의 乾物生塵量과 品質에 미치는 影響을 究明 하고자 1986년부터 1987년까지 2년간 수행되었다. 1. 山地草地에 있어서 順料方向에 의한 orchardgrass의 乾物生塵量과 租蛋白質 含量은 北料面아 南料面보다 높았고, 南北 t 兩料面 모두 標高가 높아짐에 따라서 乾物生塵量과 組蛋白質 含量이 增加하였다. 2. Neutral detergent fiber(NDF), acid detergent fiber(ADF) 含量 및 in vitro 乾物消化率은 碩料方向間(南, 北) 그리고 標高間(250m, 350m, 500m)에 差異가 나타나지 않았다.

• 농업과학연구
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• 제45권4호
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• pp.749-760
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• 2018

In Korea, the largest agricultural lands are paddy fields which have poor infiltration and drainage properties. Recently, the Korean government has pursued cultivating upland crops in paddy fields to reduce overproduced rice in Korea. For this policy to succeed, it is critical to understand the topographic information of paddy fields and its effects on upland crops cultivated in the soils of paddy fields. The objective of this study was to characterize the growth properties of sesame and perilla from paddy fields with three soil topographic features and soil water effects which were induced by the topographic features of the sesame and perilla. The crops were planted in paddy fields located in Miryang, Gyeongnam with different topographies: mountain foot slope, local valley and alluvial plain. Soil water contents and groundwater levels were measured every hour during the growing season. The paddy field of the mountain foot slope was significantly effective in alleviating wet injury for the sesame and perilla in the paddy fields. The paddy field of the mountain foot slope had a decreased average soil water content and groundwater level during cultivation. Stress day index (SDI) from the alluvial plain paddy field had the greatest values from both crops and the smallest from the ones from the paddy field of the mountain foot slope. This result means that sesame and perilla had the smallest stress from the soil water content of the paddy field on the mountain foot slope and the greatest stress from the soil water content of the alluvial plain. It is important to consider the topography of paddy fields to reduce wet injury and to increase crop yields.

• 한국환경복원기술학회지
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• 제19권6호
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• pp.101-110
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• 2016

Development activities in forest areas are analysed based on degree of slope, altitude, land cover, and prefectures in order to improve the capacity of existing regulations of 'feasibility of forest land conversion' and 'assessment of forest land characteristics' in this research. 959 land based developments between year 2007 and 2013 have been analysed. A development site includes over 50% of forest is categorized as a forest type, degree of slope is steeper than $8.5^{\circ}$ as mountain type, and a development included in the both categories as combined type. Distribution characteristics of the above three types are analysed by development categories and regions adopting Relative Mountain Development Index(RMDI). In results, 44.94% of total development activities have been carried out in Gyeongsang Do in order of urban development, industrial complex, sports facilities, and soil and stone collection quarrying. Developments less than $0.3km^2$ which are exempt from the feasibility of forest land conversion regulation consist 86 cases of forest type, 78 cases in mountain type, and 78 cases in combined type. SAI by slope range showed the highest value of 1.55 in less than $5^{\circ}$ and the lowest value of 0.69 between $20^{\circ}-25^{\circ}$. RMDI value in Gyeongsang Do where mountain ratio is 67.05% appeared 1.17, which is 5 times more than Gangwon Do where mountain area ratio is 81.30%, and 2 times more than Chungchung Do where mountain area ratio is 51.24%. Development activities in forestland in Korea showed unequal distributions and 26% of those developments were not subjected to the feasibility of forest land conversion regulation.

• 한국환경과학회지
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• 제13권8호
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• pp.721-731
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• 2004

The dispersion of suspended particulates in the coastal complex terrain of mountain-inland basin (city)-sea, considering their recycling was investigated using three-dimensional non-hydrostatic numerical model and lagrangian particle model (or random walk model). Convective boundary layer under synoptic scale westerly wind is developed with a thickness of about I km over the ground in the west of the mountain, while a thickness of thermal internal boundary layer (TIBL) is only confined to less than 200m along the eastern slope of the mountain, below an easterly sea breeze circulation. At the mid of the eastern slop of the mountain, westerly wind confronts easterly sea breeze, which goes to the height of 1700 m above sea level and is finally eastward return flow toward the sea. At this time, particulates floated from the ground surface of the city to the top of TIBL go along the eastern slope of the mountain in the passage of sea breeze, being away the TIBL and reach near the top of the mountain. Then those particulates disperse eastward below the height of sea-breeze circulation and widely spread out over the coastal sea. Total suspended particulate concentration near the ground surface of the city is very low. On the other hand, nighttime radiative cooling produces a shallow nocturnal surface inversion layer (NSIL) of 200 m thickness over the inland surface, but relatively thin thickness less than 100m is found near the mountain surface. As synoptic scale westerly wind should be intensified under the association of mountain wind along the eastern slope of mountain to inland plain and further combine with land-breeze from inland plain toward sea, resulting in strong wind as internal gravity waves with a hydraulic jump motion bounding up to about 1km upper level in the atmosphere in the west of the city and becoming a eastward return flow. Simultaneously, wind near the eastern coastal side of the city was moderate. Since the downward strong wind penetrated into the city, the particulate matters floated near the top of the mountain in the day also moved down along the eastern slope of the mountain, reaching the. downtown and merging in the ground surface inside the NSIL with a maximum ground level concentration of total suspended particulates (TSP) at 0300 LST. Some of them were bounded up from the ground surface to the 1km upper level and the others were forward to the coastal sea surface, showing their dispersions from the coastal NSIL toward the propagation area of internal gravity waves. On the next day at 0600 LST and 0900 LST, the dispersed particulates into the coastal sea could return to the coastal inland area under the influence of sea breeze and the recycled particulates combine with emitted ones from the ground surface, resulting in relatively high TSP concentration. Later, they float again up to the thermal internal boundary layer, following sea breeze circulation.

• 한국지능시스템학회:학술대회논문집
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• 한국퍼지및지능시스템학회 2000년도 추계학술대회 학술발표 논문집
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• pp.121-124
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• 2000

We introduce an advanced mountain clustering method which uses a normalized data space, a gaussian type mountain function and a deconstruction method using mountain slope. This is more useful than Yagers mountain method because it needs just one parameter to tune instead of three and finds out more resonable cluster centers. Computational examples are presented to show the validity of the advanced mountain method.