• Proceedings of the Korea Water Resources Association Conference
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• 2005.05b
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• pp.908-911
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• 2005

지표와 대기사이에서 식물의 광합성 및 증발산 능력과 밀접하게 관련되어 있는 엽면적지수는 식생밀도를 나타낼때 사용되는 식생지수이다. 본 연구에서는 NOAA-AVHRR 자료를 사용한 엽면적지수를 사용하여 남한지역 엽면적지수의 시공간변화도와 주기성분석을 실시하였고 소양강댐유역, 안동댐유역과 주요 도시의 엽면적지수의 월별, 년별, 계절별 추세를 분석하였다. 추세분석결과 월추세 분석에서는 장기간의 뚜렷한 변동성을 나타내지는 않았지만 겨울과 봄 보다는 여름과 가을에 식생의 밀도가 더 높은 계절적인 요인에 많은 영향을 받는 것을 볼 수 있었다. 시간변화 분석결과 계절변화를 제외한 특별한 장기변동을 확인할 수 없었으며 엽면적지수의 공간 변화는 정규식생지수가 보여주는 지형이나 위도의 변화와 밀접한 관계를 가지는 변화양상을 보여주지 않았다. 이는 농지 및 삼림 등의 인위적 조성으로 인한 엽면적지수의 공간변화도 양상과 관계있다 하겠다.

• Journal of the Korean Association of Geographic Information Studies
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• v.15 no.3
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• pp.52-65
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• 2012

The net biomass accumulation (or net primary production, NPP) and gross primary production (GPP) have closely related with carbon accumulations(or carbon exchange) in vegetation. There are many approaches to estimate biomass using remote sensing techniques. The vegetation indices (VIs) can be a methodology to estimate biomass which assumes total chlorophyll contents. Various VIs were characterized with difference development conditions as vegetation species, input datasets. The hyperspectral data have also different spatial/spectral resolutions for aerial surveying. Additionally they need particular spectral bands selection difficulty to calculate the VIs. The objective of this study is to evaluate the correlations with airborne hyperspectral data (compact airborne spectrographic imager, CASI) and spectral unmixing model (or spectral mixture analysis, SMA) to characterize vegetation indices in forest area. The spectral mixture analysis was used to model the spectral purity of each pixel as an endmember. The endmembers are the fraction components derived from hyperspectral data through the SMA. In this study, we choose three endmembers represented vegetation pixels in the hyperspectral data. These endmembers were compared with 9 VIs by the Pearson's correlation coefficient. The results show MTVI1 and TVI have same correlation coefficient with 0.877. The MCARI, especially has very high relationship with vegetation endmembers as 0.9061 at less vegetation and soil distributed site. The MTVI1 and TVI have high correlations with the vegetation endmembers as 0.757 in whole test sites.

• Journal of the Korean Society of Surveying, Geodesy, Photogrammetry and Cartography
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• v.32 no.1
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• pp.9-17
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• 2014

The Vegetation cover is a significant factor to comprehend characteristics of the ground surface for meterological and hydrological models, which measure energy in the atmosphere or predict the runoff of ground surface. Deardorff introduced vegetation cover fraction to quantitatively comprehend the vegetation cover in 1978. After Deardorff, most of previous researches were conducted on low-resolution or high-resolution images, but only few researches on Landsat that are in medium-resolution images. Therefore, this study aims to investigate a way of calculating the vegetation cover fraction by using NDVI of Landsat images, which were hardly handled previously. For accurate vegetation cover fraction, we compared the evaluated parameters from this study with past vegetation cover fraction parameters that have been calculated for using NDVI of Landsat OLI images. The result of research was shown that NDVI is quite correlated with the vegetation fraction cover in the previous researches. In fact, RMSE of vegetation cover fraction values that obtained through the suggested parameters on this study showed the highest accuracy of 7.3% among all the cases.

• 한국공간정보시스템학회:학술대회논문집
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• 2007.06a
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• pp.156-161
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• 2007

도시화에 따른 도시문제발생이라는 결과로 미루어 볼 때, 지속적인 도시 성장을 위한 도시 성장 관리는 필수적이며, 이것을 위해서 도시지역을 추출하는 것은 도시의 성장 추이를 파악할 수 있게 한다는 점에서 매우 의미 있는 일이다. 본 연구에서는 도시 성장 모니터링에 있어서 정규식생지수(NDVI)와 정규시가지화지수(NDBI)를 결합한 방법의 활용성을 규명하는데 목적을 두었다. 이를 위해 토지피복분류에 일반적으로 사용되는 감독 분류기법과 도시지역추출에 이용되는 NDVI와 NDBI를 결합한 방법(식생지수결합법)으로 1988년과 2000년 두 시기의 Landsat TM 영상을 이용하여 도시지역을 추출하고 일치도를 분석하였다. 분석 결과, 1988년 식생지수결합법과 감독분류기법으로 추출한 도시지역의 일치도는 98%, 식생지수결합법 비도시지역으로 추출된 지역이 감독분류기법으로는 도시지역으로 추출될 확률은 37.35%로 나타났고, 같은 경우 2000년은 각각 99.3%와 7.7%로 나타났다. 이를 통해 식생지수결합법을 사용한 도시지역 추출 결과와 감독분류기법을 사용한 도시지역 추출 결과의 일치도가 비교적 높게 나타남을 알 수 있었다. 또, 각 기법을 통한 도시지역 추출 결과와 실제 도시 검사점과의 일치도의 분석을 통해서도 도시지역 추출 결과의 일치도가 비교적 높게 나타났다. 따라서 분류를 통한 도시지역 추출 방법에 비해 식생지수결합법을 이용한 도시지역 추출이 절차상 수월한 점을 감안하면 도시지역 추출에 있어서 식생지수결합법의 효율성을 입증할 수 있었다.

• Journal of Korean Society of Forest Science
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• v.83 no.4
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• pp.441-449
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• 1994

The two reflective channels(red and near infrared spectrum) of advanced very high resolution radiometer(AVHRR) data were used to classify primary vegetation cover types in the Korean Peninsula. From the NOAA-11 satellite data archive of 1991, 27 daytime scenes of relatively minimum cloud coverage were obtained. After the initial radiometric calibration, normalized difference vegetation index(NDVI) was calculated for each of the 27 data sets. Four or five daily NDVI data were then overlaid for each of the six months starting from February to November and the maximum value of NDVI was retained for every pixel location to make a monthly composite. The six bands of monthly NDVI composite were nearly cloud free and used for the computer classification of vegetation cover. Based on the temporal signatures of different vegetation cover types, which were generated by an unsupervised block clustering algorithm, every pixel was classified into one of the six cover type categories. The classification result was evaluated by both qualitative interpretation and quantitative comparison with existing forest statistics. Considering frequent data acquisition, low data cost and volume, and large area coverage, it is believed that AVHRR data are effective for vegetation cover type mapping at regional scale.

• Proceedings of the Korea Water Resources Association Conference
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• 2008.05a
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• pp.470-474
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• 2008

본 연구에서는 댐 하류하천의 사주와 식생의 면적변화, 변화지수, 변화정도와 경년변화를 분석하였다. 사주면적은 댐 건설후 16.73%가 감소하였으며, 변화지수는 $-0.2599{\sim}-0.9921$이었다. 식생면적은 댐 건설후 12.84%가 증가하였으며, 변화지수는 $0.2699{\sim}12.0736$이었다. 안동, 임하, 합천의 3개 댐의 연 최소 유량과 사주와 식생의 경년 변화를 분석 하였다. 연 최소 유량변화 분석결과, 1일 최소유량은 안동댐이 203%, 임하댐이 167%, 합천댐이 677%가 증가하였으며, 1일 최대유량은 안동댐이 84%, 임하댐이 63%, 합천댐이 81%가 감소하였다. 사주와 식생의 경년변화 분석결과, 사주면적은 연평균 $42,600\;m^2$씩 감소하였으며, 식생면적은 연평균 $51,700\;m^2$ 씩 증가하여 사주면적의 감소 보다 식생면적의 증가가 높은 것으로 분석되었다. 댐이 하류하천의 사주와 식생에 미치는 영향에 가장 중요한 요소는 첨두 홍수량 감소와 저유량 증가 등의 유량변화이다.

• Journal of the Korean Society of Surveying, Geodesy, Photogrammetry and Cartography
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• v.23 no.4
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• pp.393-399
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• 2005

Since vegetations are near the wavelength range in 700nm and have absorbent as well as reflective wavelength ranges, there is a much difference in terms of its reflection rate. There are currently many researches on vegetation index being conducted in order to apply the remote-sensing technology to vegetations rising their characteristics of absorbent and reflective wavelength ranges. Normalized Difference Vegetation Index (NDVI) and Perpendicular Vegetation Index (PVI) have been most commonly used. It is usually the evaporation, carbon-dioxide consumption, and chlorophyll density that represent the activity of vegetation, but chlorophyll density is the most commonly used among them. Since the red wavelength range used to obtain the NDVI and PVI has a strong extinction of chlorophyll, it is also useful to test chlorophyll density. The NDVI, in particular, is used to identify the vegetation conditions summarily, and thus, is suitable for initiative researches. Nevertheless, since these vegetation index produce mixed information of the Vegetation vigor and vegetation cover, it is essential to monitor a wavelength range that is independent from redundancy of the Vegetation vigor and vegetation cover. Although many vegetation indices have evaluated both the vegetation vigor and Vegetation cover simultaneously, this research intends to emphasize the utility of separable evaluations of the Vegetation vigor and Vegetation Cover rate through an experiment with grasses. As a result of evaluating vegetation index using spectral reflectance, a separable evaluation of the vegetation vigor and cover has been found more useful.

• Proceedings of the KSRS Conference
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• 2007.03a
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• pp.37-40
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• 2007

대규모 연안개발은 연안지형의 변화와 함께 다양한 식물상의 변화를 만드는 원인이 되고 있다. 때문에 시화방조제， 새만금방조제， 남양만 방조제 등의 대규모 방조제 공사 이후에 연안갯벌에서 나타나는 식물상의 변화를 관측하는 것은 연안습지환경의 변화를 분석하는 중요한 척도가 된다. 본 연구에서는 아리랑 2호 의 고해상도 자료를 바탕으로 연안습지의 지형변화에 따라 나타나는 생물상의 식생지수를 분석하고 이들의 시-공간적변화가 연안지형의 특성과 공간규모의 대칭적 특성을 나타내고 있음을 제시하였다. 특히，중급해상도에 의해 분석되었던 식생지수를 고해상도 위성관측 자료와 현장조사 자료를 비교하여 이를 검증하였다.

• Journal of the Korean earth science society
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• v.25 no.8
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• pp.754-763
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• 2004

This study was aimed to examine the Landsat Enhanced Thematic Mapper Plus (ETM+) index, which matches well with the field survey data in the wildfire area of Gangneung, Gangweon Province, Korea. In the wildfire area NDVI (Normalized Difference Vegetation Index), SAVI (Soil Adjusted Vegetation Index), and Tasseled Cap Transformation Index (Brightness, Wetness, Greenness) were compared with field survey data. NDVI and SAVI were very useful in detecting the difference between the wildfire and non-wildfire area, but not so in classify the soil types in the wildfire area. The soil plane based on the Tasseled Cap Transformation showed a better result in classifying the soil types in the wildfire areas than NDVI and SAVI, and corresponded well with field survey data. Using a linear function based on greenness and wetness in the Tasseled Cap Transformation is expected to provide a more efficient and quicker method to classify wildfire areas.

• Journal of the Korean Association of Geographic Information Studies
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• v.18 no.4
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• pp.145-157
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• 2015

In 2015, drought was at the worst stage of devastation in Soyanggang Dam watershed. The purpose of this study is to trace the drought area around Soyanggang dam watershed by using Terra MODIS image because it has the ability of spatio-temporal dynamics. The MODIS indices, which included the enhanced vegetation index (NDVI), were extracted from MODIS product MOD13 16-day composite datasets with a spatial resolution of 250m from 2010.01.01 to 2015.06.30. We found that application of Vegetation Condition Index (VCI) and Standardized Vegetation Index (SVI) was suitable for monitoring the drought area. The result can be used to acquire the drought data scattered and demonstrate the potential for the use of MODIS data for temporal and spatial detection of drought effects.