• Title/Summary/Keyword: terrain factors

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The Performance Analysis of an Airborne Radar Altimeter based on Simultaneously Acquired LiDAR Data (비행 시험을 통한 레이더 전파고도계 특성 분석)

  • Yoon, Jongsuk;Kwak, Hee Jun;Kim, Yoon Hyoung;Shin, Young Jong;Yoo, Ki Jeong;Yu, Myeong Jong
    • Korean Journal of Remote Sensing
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    • v.29 no.1
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    • pp.81-94
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    • 2013
  • The Radar altimeter transmits radio signals to the surface, receives the backscattered signals and measures the distance between the airplane and the nadir surface. The measurements of radar altimeter are affected by various factors on the surface below the aircraft. This study performed flight campaigns in June 2012 and acquired raw data from radar altimeter, LiDAR and other sensors. Based on the LiDAR DSM (Digital Surface Model) as a reference data, the characteristics of radar altimeter were analyzed in the respect of range and surface area affecting on the receiving power of the radar altimeter. Consequently, the radar altimeter was strongly affected by the surface area within beam width and reflectivity related to RCS (Radar Cross Section) rather than range.

A Study of a Heavy Rainfall Event in the Middle Korean Peninsula in a Situation of a Synoptic-Scale Ridge Over the Korean Peninsula (종관규모 기압능이 한반도를 덮고 있는 기간에 중부지방에서 나타난 호우의 발생 원인)

  • Kim, Ah-Hyun;Lee, Tae-Young
    • Atmosphere
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    • v.26 no.4
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    • pp.577-598
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    • 2016
  • Observational and numerical studies have been carried out to understand the cause and development processes of the heavy rainfall over the middle Korean Peninsula during 0300 LST-1500 LST 29 June 2011 (LST = UTC + 0900). The heavy rainfall event occurred as the synoptic-scale ridge extended from Western Pacific Subtropical High (WPSH) was maintained over East Asia. Observational analysis indicates that the heavy rainfall is mainly due to scattered convective systems, formed over the Yellow Sea, traveling northeastward across the middle peninsula without further organization into larger systems during 0300 LST-0800 LST, and mesoscale convective systems (MCSs) over the Yellow Sea, transformed into a squall line, traveling eastward during 0800 LST-1500 LST. Organization of convective systems into MCSs can be found over the area of mesoscale trough and convergence zone in the northern end of the low-level jet (LLJ) after 0600 LST. Both observational and numerical investigations indicate that a strong LLJ extended from the East China Sea to the Yellow Sea plays an essential role for the occurrence of heavy rainfall. The strong LLJ develops in between the WPSH and a pressure trough over eastern China. Numerical experiments indicate that the land-sea contrast of solar heating of surface and latent heating due to convective developments are the major factors for the development of the pressure trough in eastern China. Numerical study has also revealed that the mountainous terrain including the mountain complex in the northern Korean Peninsula contributes to the increase of rainfall amount in the middle part of the peninsula.

LOS Analysis Simulation considering Canopy Cover (수목차폐율을 고려한 가시선 분석 시뮬레이션)

  • Kong, Seong-Pil;Song, Hyun-Seung;Eo, Yang-Dam;Kim, Yong-Min;Kim, Chang-Jae
    • Journal of Korean Society for Geospatial Information Science
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    • v.20 no.2
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    • pp.55-61
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    • 2012
  • The primary factors of the LOS(Line-of-Sight) analysis process are terrain height, camera capacity, and canopy cover. The canopy cover rate differs depending on the changing season, and its value is influenced by the tree density, tree height, and etc. This study generated the canopy cover value based on relationship between NDVI(Normalized Difference Vegetation Index) and DMT(Density Measure % of Tree/Canopy Cover), which is a digital map attribute, and then performed the LOS analysis on six station of test sites. As results, It was found that NDVI and DMT are correlated with each other through the experiments. Based on this finding, new DMT map can be generated using NDVI. Also, There is a difference between the result of visibility analysis using the present DMT and one using a new DMT. Especially, the spatial distributions of the detected visible areas are significantly different between the two visibility analysis results.

Characteristic of PM10 Distribution Related to Precise Local Wind Patterns in Busan Metropolitan Area (상세 국지 기류 분포를 고려한 부산 지역 내 미세 먼지 분포 특성)

  • Hong, Seon-Hwa;Lee, Soon-Hwan
    • Journal of Environmental Science International
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    • v.26 no.12
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    • pp.1375-1387
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    • 2017
  • In order to investigate the $PM_{10}$ concentration trend and its characteristics over five different sub area in Busan from 2013 to 2015, data analysis with considering air flow distribution according to its topography was carried out using statistical methodology. The annual mean concentrations of $PM_{10}$ in Busan tend to decrease from $49.6{\mu}g/m^3$ in 2013 to $46.9{\mu}g/m^3$ in 2015. The monthly mean concentrations value of $PM_{10}$ were high during spring season, from March to May, and low during summer and fall due to frequent rain events. The concentration of $PM_{10}$ was the highest in five different sub-area in Busan. High concentration episodes over 90 percentile of daily $PM_{10}$ concentration were strongly associated with mean daily wind speed, and often occurred when the westerly wind or southwesterly wind were dominant. Regardless of wind direction, the highest correlation of $PM_{10}$ concentrations was observed between eastern and southern regions, which were geographically close to each other, and the lowest in the western and eastern regions blocked by mountains. Wind flow along the complex terrain in Busan is also one of the predominant factors to understand the temporal variation of $PM_{10}$ concentrations.

Hydraulic Design of Natural Gas Transmission Pipeline in the Artic Area (극한지 장거리 천연가스 배관의 유동 설계)

  • Kim, Young-Pyo;Kim, Ho-Yeon;Kim, Woo-Sik
    • Journal of the Korean Institute of Gas
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    • v.20 no.2
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    • pp.58-65
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    • 2016
  • Hydraulic analysis of the natural gas transmission pipeline is to determine whether adequate flow can be sustained throughout the design life of pipeline under all expected flow conditions. Many factors have to be considered in the hydraulic design of long-distance pipelines, including the nature, volume, temperature and pressure of fluid to be transported, the length and elevation of pipeline and the environment of terrain traversed. This study reviewed the available gas operation data provided by pipeline construction project in the arctic area and discussed the gas properties such as viscosity and compressibility factor that influence gas flow through a pipeline. Pipeline inside diameter was calculated using several flow equations and pipeline wall thickness was calculated from Barlow's equation applying a safety factor and including the yield strength of the pipe material. The AGA flow equation was used to calculate the pressure drop due to friction, gas temperature and pipeline elevation along the pipeline. The hydraulic design in this study was compared with the report of Alaska Pipeline Project.

A Study on the Meaning and the Factors of Formation of the Prototypal Landscape (원형경관(原型景觀)의 개념 정립 및 형성요인 연구)

  • Kang, Young-Eun;Choi, Dong-Wook;Hong, Sung-Hee;Jung, Yun-Hee;Kim, Sang-Bum;Im, Seung-Bin
    • Journal of Korean Society of Rural Planning
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    • v.15 no.4
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    • pp.33-42
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    • 2009
  • This study is aimed at the necessity application in 'Prototype' general concept on discovering cultural identity landscape of our national characteristics landscape research. Accordingly, It is considered landscape, fundamental concept, the prototypal landscape concept from previously researches that have been used. At the same time, the concept of prototypal landscape has been established by commenting a point of view which is defining previous researches that controverted prototypal landscape, then establish concept of prototypal landscape and derive attribute by comparing and considering similar terminology of prototypal landscape. Previously, research prototypal landscape in depth by applying defined concept of prototypal landscape and considering inherence ideological and environmental background prototypal figure and structure. Formation pattern of the prototypal landscape is classified in both philosophical formative primary factor from philosophy, religion and environmental formative factor of human that accumulated cultural life from a region and life. Examples of forming the prototypal landscape by philosophical formative factor are classified as 'Feng-Shui(the theory of divination based on topography)', 'Yin-Yang theory', 'Confucian idea theory' 'Philosophical Taoism', 'Buddhism theory' and 'Nature theory' then environmental formative factor are interpreted by 'Taekliji(determining of advantageous land)', 'Imwon(forest) economical geography', 'land use', 'topography' and 'terrain' as examples. This study is anticipating a new point of view and an establishment of reliable preservation to our characteristic of the prototypal landscape by considering concept of prototypal landscape and formative factor as studying limits of prototypal landscape and researching concentrated origination of the prototype.

Microcellular Propagation Loss Prediction Using Neural Networks and 3-D Digital Terrain Maps (신경회로망과 3차원 지형데이터를 이용한 마이크로셀 전파손실 예측)

  • 양서민;이혁준
    • The Journal of Korean Institute of Electromagnetic Engineering and Science
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    • v.10 no.3
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    • pp.419-429
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    • 1999
  • Identifying the boundary of the effective receiving power of waves is one of the most important factors for cell optimization. In this paper, we introduce a propagation loss prediction model which yields highly accurate prediction in very complex areas as Seoul where a mixture of many large buildings, small buildings, broad streets, narrow alleys, rivers and forests co-exist in an irregular arrangement. This prediction model is based on neural networks trained on field measurement data collected in the past. Using these data along with 3-D digital elevation maps and vector data for building structures, we extract the parameter values which mainly affect the amount of propagation loss. These parameter values are then used as the inputs to the neural network. Trained neural network becomes the approximated function of the propagation loss model which generalizes very well and can predict accurately in the regions not included in training the neural network. The experimental results show a superior performance over the other models in the cells operating in the city of Seoul.

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Korean Groal Potential Habitat Suitability Model at Soraksan National Park Using Fuzzy Set and Multi-Criteria Evaluation (설악산국립공원내 산양(Nemorhaedus Caudatus Raddeanus)의 잠재 서식지 적합성 모형; 다기준평가기법(MCE)과 퍼지집합(Fuzzy Set)의 도입을 통하여)

  • Choi Tae-Young;Park Chong-Hwa
    • Journal of the Korean Institute of Landscape Architecture
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    • v.32 no.4
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    • pp.28-38
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    • 2004
  • Korean goral (Nemorhaedus caudatus raddeanus) is one of the endangered species in Korea, and the rugged terrain of the Soraksan National Park (373㎢) is a critical habitat for the species. But the goral population is threatened by habitat fragmentation caused by roads and hiking trails. The objective of this study was to develop a potential habitat suitability model for Korean goral in the park, and the model was based on the concepts of fuzzy set theory and multi-criteria evaluation. The process of the suitability modeling could be divided into three steps. First, data for the modeling was collected by using field work and a literature survey. Collected data included 204 points of GPS data obtained through a goral trace survey and through the number of daily visitors to each hiking trail during the peak season of the park. Second, fuzzy set theory was employed for building a GIS data base related to environmental factors affecting the suitability of the goral habitat. Finally, a multiple-criteria evaluation was performed as the final step towards a goral habitat suitability model. The results of the study were as follows. First, characteristics of suitable habitats were the proximity to rock cliffs, scattered pine (Pinus densiflora) patches, ridges, the elevation of 700∼800m, and the aspect of south and southeast. Second, the habitat suitability model had a high classification accuracy of 93.9% for the analysis site, and 95.7% for the validation site at a cut off value of 0.5. Finally, 11.7% of habitatwith more than 0.5 of habitat suitability index was affected by roads and hiking trails in the park.

Numerical Simulation for the Field Tracer Experiment over the Kori Nuclear Power Plant (고리 원전주변에서 야외 확산실험 모사)

  • Suh, Kyung-Suk;Kim, Eun-Han;Whang, Won-Tae;Jeong, Hyo-Joon;Han, Moon-Hee
    • Journal of Radiation Protection and Research
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    • v.29 no.3
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    • pp.205-212
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    • 2004
  • Three-dimensional wind field and atmospheric dispersion models have been developed for estimating the concentration distributions of radioactive materials released into atmosphere. The field tracer experiment near the Kori nuclear power plant located over complex terrain was carried out for validating the atmospheric dispersion model. The wind fields were one of the most important factors for calculating the concentration. Therefore several numerical simulations using the measured wind data were performed to get more accurate concentration distributions compared with the analyzed values of the tracer gas. The calculated concentration distributions agreed well in the case of the usage of the more measured wind data in wind field model.

DOES LACK OF TOPOGRAPHIC MAPS LIMIT GEO-SPATIAL HYDROLOGY ANALYSYS?

  • Gangodagamage, Chandana;Flugel, Wolfgang;Turrel, Dr.Hagh
    • Proceedings of the KSRS Conference
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    • 2003.11a
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    • pp.82-84
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    • 2003
  • Watershed boundaries and flow paths within the watershed are the most important factors required in watershed analysis. Most often the derivation of watershed boundaries and stream network and flow paths is based on topographical maps but spatial variation of flow direction is not clearly understandable using this method. Water resources projects currently use 1: 50, 000-scale ground survey or aerial photography-based topographical maps to derive watershed boundary and stream network. In basins, where these maps are not available or not accessible it creates a real barrier to watershed geo-spatial analysis. Such situations require the use of global datasets, like GTOPO30. Global data sets like ETOPO5, GTOPO30 are the only data sets, which can be used to derive basin boundaries and stream network and other terrain variations like slope aspects and flow direction and flow accumulation of the watershed in the absence of topographic maps. Approximately 1-km grid-based GTOPO 30 data sets can derive better outputs for larger basins, but they fail in flat areas like the Karkheh basin in Iran and the Amudarya in Uzbekistan. A new window in geo-spatial hydrology has opened after the launching of the space-borne satellite stereo pair of the Terra ASTER sensor. ASTER data sets are available at very low cost for most areas of the world and global coverage is expected within the next four years. The DEM generated from ASTER data has a reasonably good accuracy, which can be used effectively for hydrology application, even in small basins. This paper demonstrates the use of stereo pairs in the generation of ASTER DEMs, the application of ASTER DEM for watershed boundary delineation, sub-watershed delineation and explores the possibility of understanding the drainage flow paths in irrigation command areas. All the ASTER derived products were compared with GTOPO and 1:50,000-based topographic map products and this comparison showed that ASTER stereo pairs can derive very good data sets for all the basins with good spatial variation, which are equal in quality to 1:50,000 scale maps-based products.

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