• 대한지리학회지
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• 제49권3호
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• pp.321-338
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• 2014

본 연구의 목적은 우리나라에 분포하는 463개 하구를 대상으로 하구습지의 권역별 분포특성과 시계열 변동추이를 하구순환 관점에서 파악하는 데 있다. 환경관리에 널리 이용되는 유역을 토대로 한강서해권역, 한강동해권역, 금강권역, 영산강권역, 섬진강권역, 낙동강권역, 제주권역을 대상으로 하구습지의 분포실태를 조사하고, 권역별 하구습지의 시계열 변동추이를 1980년대, 1990년대, 2000년대 토지피복지도를 확보하여 분석하였다. 분석결과, 한강서해권역, 금강권역, 영산강권역의 하구습지는 크게 감소한 것으로 나타났으며, 특히 하구둑, 배수갑문 등 인공구조물에 의해 하구순환이 차단된 닫힌하구에서의 습지감소폭이 크고, 하구순환이 유지되는 열린하구에서의 습지훼손은 상대적으로 적은 것으로 나타났다. 하구습지와 관련된 갯벌, 개방수면, 염습지, 암석해안, 모래해안 등 하구내 서식지 다양성은 하구순환이 차단된 닫힌하구에 비해 하구순환이 유지되는 열린하구에서 높게 나타났다. 본 연구에서 제시한 권역별 하구습지의 분포특성과 시계열 변동추이는 하구환경의 관리방향을 설정하거나 훼손된 하구습지의 복원전략을 마련하는 데 효과적으로 활용할 수 있다.

• 한국환경생태학회지
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• 제19권4호
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• pp.375-384
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• 2005

본 연구는 시가화지역 토지이용 및 녹지구조에 따른 온도변화를 파악하고자 강남구 내 시가화지역을 대상으로 44개소 조사지를 블록단위로 선정하여 실시하였다. 온도값은 1999${\~}$2002년까지의 Landsat TM 및 ETM+ 영상 6scene을 적용하였다. 도시온도변화에 대한 영향요인 분석결과 토지 이용유형은 그 자체로 도시온도변화의 중요 인자로 작용하지는 않는 것으로 판단되었으며 토양피복유형은 상관관계 분석결과 상관계수가 건폐율이 0.368(2001년 6월)${\~}$0.709(1999년 5월)로 양(+)의 상관관계에 있었으며 녹지율은 -0.551(2001년 6월)${\~}$-0.860(1999년 6월)으로 음(-)의 상관관계를 보였다. 녹지용적(녹지용적계수${\times}$100), 녹피율과 온도값과의 상관관계 분석 결과 녹피율과의 상관계수는 -0.549(2001년 6월)${\~}$-0.817(1999년 6월)의 범위이었으며 녹지용적은 -0.517(2001년 6월)${\~}$-0.882(1999년 6월)로 녹피율과 녹지용적 모두 각 온도값과 강한 음(-)의 상관관계를 보였다. 도시화지역 온도변화 예측모형 구축을 위한 회귀분석 결과 녹지용적이 설명 변수로 채택되었다.

• 한국지리정보학회지
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• 제12권2호
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• pp.23-33
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• 2009

위성영상은 도시의 물리적 확장 및 변화를 예측하고 분석하는데 있어 매우 유용하게 활용되고 있다. 도시의 물리적 확장 및 변화는 도시의 토지이용과 밀접하게 관련되어 있으며, 지속 가능한 도시성장을 위해서는 토지이용을 중심으로 한 지속적인 성장관리가 필수적이다. 본 연구에서는 인공위성에 의한 원격자료를 기초 입력 자료로 1985년~2000년 사이의 토지피복과 토지이용의 변화를 분석하였다. 또한 토지이용 전환율을 파악하여 부산시 시가화지역의 확산동향과 확산지역의 토지이용특성을 파악하였다. 그 결과, 첫째, 도시지역의 면적은 지속적으로 늘어난 반면 농업, 산림, 수계지역의 면적은 연도별로 부산시 행정구역개편으로 인해 면적의 변화가 상이함을 알 수 있었다. 둘째 부산시의 도시화 지역 면적이 1985년도 $92.5km^2$에서 2000년도에는 $167.5km^2$로 3.8% 증가한 것을 알 수 있었다. 셋째 토지이용의 전환율을 분석한, 결과 농경지 나지가 도시화 지역으로 가장 많이 전환 되었고, 다음이 산림의 순서로 나타났다. 넷째, 2001년에 구축된 부산시건물 database와의 overlay 분석결과 농업지역 나지는 제1, 2종 근린생활시설(45.63%), 산림지역은 공동주택(18.49%), 수계지역은 공장(31.84%)등의 비율이 높음을 알 수 있었다.

• 대한전자공학회:학술대회논문집
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• 대한전자공학회 2004년도 학술대회지
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• pp.842-845
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• 2004

The aim of this study is to compare the classification results for choosing the fuzzy membership function within fuzzy rules. There are various methods of extracting rules from training data in the process of fuzzy rules generation. Pattern distribution characteristics are considered to produce fuzzy rules. The accuracy of classification results are depended on not only considering the characteristics of fuzzy subspaces but also choosing the fuzzy membership functions. This paper shows how to produce various type of fuzzy rules from the partitioning the pattern spaces and results of land cover classification in satellite remote sensing images by adopting various fuzzy membership functions. The experiments of this study is applied to Landsat TM image and the results of classification are compared by fuzzy membership functions.

• 한국환경복원기술학회지
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• 제17권2호
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• pp.49-60
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• 2014

This study was conducted to evaluate the effect of forest fire on natural distribution and regeneration of Pinus densiflora Sieb. & Zucc. in Goseong, Gangwon province, Korea. After 13 years of the last forest fire in 2000, five investigation plots ($10m{\times}10m$) in each of rocky land and ridge, the well-known location as a favorite site for natural distribution of P. densiflora, were set to investigate stand characteristic and soil environment including physico-chemical properties and moisture contents of soil. Also, five investigation plots in slope area were set and investigated as well. The concentration of organic matter, total nitrogen, and exchangeable nutrients ($K^+$, $Ca^{2+}$, $Mg^{2+}$) were highest in the slope while the soil in the rocky land showed the lowest concentration of organic matter, total nitrogen, available $P_2O_5$, and exchangeable nutrients ($K^+$, $Na^+$, $Ca^{2+}$, $Mg^{2+}$). The soil in the slope only showed higher concentration of total nitrogen, $K^+$ and $Ca^{2+}$ than the unburned area in Goseong. Mean soil moisture contents in the rocky land (5.77%) were lowest while the slope (15.78%) and the ridge (15.27%) showed almost three times as much than the rocky land. P. densiflora was dominant in the rocky land and Quercus spp. were dominant in the ridge and slope. The average proportion of P. densiflora was highest in rocky land (58.4%, 14.6 trees per plot) followed by the ridge (25.2%, 7.8 trees per plot) and the slope (11.3%, 3.4 trees per plot) while the average height of P. densiflora was highest in slope (277cm) followed by the ridge and the rocky land. The height and crown width of Quercus spp. were higher than P. densiflora in the every plot. The results suggest that P. densiflora may be able to naturally regenerate and survive in the rocky land after the fire while P. densiflora in the ridge and the slope are suppressed by Quercus spp.

• 한국조경학회지
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• 제33권1호
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• pp.71-80
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• 2005

In order to search for ecologically indicative characteristics on the street tree plots in Daegu area, plant communities and their floras were investigated. A total of 105 plots were collected and numerically analyzed by PCoA(Principal Coordinates Analysis). These plots were classified into 4 types containing 139 species, 97 genera, 42 families(including 37 exotic species): urban-dry type, urban-wet type, rural-dry type, rural-wet type. Habitat connectivity to the surrounding vegetation cover, extent and frequency of human impacts, and soil moisture recognizably were the main factors to allow the plots differentiation. Indicative species composition to these four types was generated as Eleusine indica-Eragrostis multicaulis-Oxalis corniculata to the urban-wet, Digitaria ciliaris-Eleusine indica-Eragrostis multicaulis to the urban-dry, Setaria viri-dis-Artemisia-Lactuca indica var. laciniata to the rural-wet, and Setaria viridis-Digitaria ciliaris-Erigeron canadensis to the rural-dry, respectively. Mean species number per plot for rural type was 2.5 times higher than for urban types. Street tree species representative to the rural-wet type is Zelkova serrata, which is a key species of potential natural vegetation in the alluvial land of Daegu area. Street tree plots were characterized by Eleusine indica showing the highest r-NCD value and also C4-assimilation grass plants. Views on the efficacy of the rural-wet type and the reinforcement of vegetation connectivity and soil moisture in rehabilitating street tree plots, are discussed.

• 환경영향평가
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• 제17권4호
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• pp.243-253
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• 2008

The purpose of this study was to simulate the reduction effect of soil loss in the Yongdam reservoir watershed using SWAT model. To evaluate accuracy for flow and sediment yield of SWAT model, calibration was performed for the period from Jan. 2002 to Dec. 2003, and the verification for Jan. 2005 to Dec. 2005. The calibration and the verification were carried out using data observed at the Cheoncheon gaging station. The $R^2$ and EI values in terms of a flow were 0.8 and 0.78 respectively for calibration, whereas they for verification were 0.88 and 0.86 respectively. In terms of a sediment yield, they were 0.7 and 0.48 respectively for calibration, whereas for verification were 0.64 and 0.54 respectively. As a results from model simulation, annual mean soil loss rates in terms of forest, paddy and upland were 0.02 ton/ha/yr, 0.15 ton/ha/yr and 7.58 ton/ha/yr, respectively. The results show that the land use type of a upland has more significant impact on a total soil loss as well as a sediment yield than other types of land use. The sediment delivery ratio was determined to be about 0.35. In this study 2 land cover change scenarios for upland area were considered. These scenarios were used an input to SWAT model in order to evaluate their impact on soil loss and sediment delivery. The results show that a reduction of the upland area would reduce the soil loss and sediment yield.

• 대한원격탐사학회:학술대회논문집
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• 대한원격탐사학회 2005년도 Proceedings of ISRS 2005
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• pp.403-406
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• 2005

In order to evaluate the Capability of ETM+ remotely- sensed data to provide 'Forest-shrub land-Rangeland' cover type map in areas near the timberline of northern forests of Iran, the data were analyzed in a portion of nearly 790 ha located in Neka-Zalemroud region. First, ortho-rectification process was used to correct the geometric errors of the image, yielding 0/68 and 0/69 pixels of RMS. error in X and Y axis, respectively. The original and panchromatic bands were fused using PANSHARP Statistical module. The ground truth map was made using 1 ha field plots in a systematic-random sampling grid, and vegetative form of trees, shrubs and rangelands was recorded as a criteria to name the plots. A set of channels including original bands, NDVI and IR/R indices and first components of PCI from visible and infrared bands, was used for classification procedure. Pair-wise divergence through CHNSEL command was used, In order to evaluate the separability of classes and selection of optimal channels. Classification was performed using ML classifier, on both original and fused data sets. Showing the best results of $67\%$ of overall accuracy, and 0/43 of Kappa coefficient in original data set. Due to the results represented above, it's concluded that ETM+ data has an intermediate capability to fulfill the spectral variations of three form- based classes over the study area.

• 환경영향평가
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• 제21권5호
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• pp.617-629
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• 2012

This study aims to find out critical areas of a soil loss and propose feasible measures to reduce the water quality deterioration by a soil lose. As a study area, the So-ok stream catchment locating at the upper area of Daecheong Reservoir is selected and intensive field observation was carried out. RUSLE model is applied to assess the impact of the pollution migration by a soil ross from the critical areas during storms on the water quality of Chusori embayment. As results, total amount of the soil ross assessed against to the critical area on which major type of land use is a orchard for fruits is 54.3 ton/ha/yr and that of an abandoned mine site is about 200 ton/ha/year. In particular as effective measures, a plantation of an appropriate species of fruit trees and an application of ecologic restoration schemes are proposed against to the orchard and the abandoned mine site, respectively.

• 대한원격탐사학회지
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• 제38권4호
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• pp.343-353
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• 2022

An attempt to derive the surface temperature from the Korea Multi-purpose Satellite (KOMPSAT)-3A mid-wave infrared (MWIR) data acquired over the southern California on Nov. 14, 2015 has been made using the MODerate resolution atmospheric TRANsmission (MODTRAN) radiative transfer model. Since after the successful launch on March 25, 2015, the KOMPSAT-3A spacecraft and its two payload instruments - the high-resolution multispectral optical sensor and the scanner infrared imaging system (SIIS) - continue to operate properly. SIIS uses the MWIR spectral band of 3.3-5.2 ㎛ for data acquisition. As input data for the realistic simulation of the KOMPSAT-3A SIIS imaging conditions in the MODTRAN model, we used the National Centers for Environmental Prediction (NCEP) atmospheric profiles, the KOMPSAT-3Asensor response function, the solar and line-of-sight geometry, and the University of Wisconsin emissivity database. The land cover type of the study area includes water,sand, and agricultural (vegetated) land located in the southern California. Results of surface temperature showed the reasonable geographical pattern over water, sand, and agricultural land. It is however worthwhile to note that the surface temperature pattern does not resemble the top-of-atmosphere (TOA) radiance counterpart. This is because MWIR TOA radiances consist of both shortwave (0.2-5 ㎛) and longwave (5-50 ㎛) components and the surface temperature depends solely upon the surface emitted radiance of longwave components. We found in our case that the shortwave surface reflection primarily causes the difference of geographical pattern between surface temperature and TOA radiance. Validation of the surface temperature for this study is practically difficult to perform due to the lack of ground truth data. We therefore made simple comparisons with two datasets over Salton Sea: National Aeronautics and Space Administration (NASA) Jet Propulsion Laboratory (JPL) field data and Salton Sea data. The current estimate differs with these datasets by 2.2 K and 1.4 K, respectively, though it seems not possible to quantify factors causing such differences.