• Title/Summary/Keyword: NOAA/AVHRR data

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INVESTIGATION OF CLOUD COVERAGE OVER ASIA WITH NOAA AVHRR TIME SERIES

  • Takeuchit Wataru;Yasuokat Yoshifumi
    • Proceedings of the KSRS Conference
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    • 2005.10a
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    • pp.26-29
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    • 2005
  • In order to compute cloud coverage statistics over Asian region, an operational scheme for masking cloud-contaminated pixels in Advanced Very High Resolution Radiometer (AVHRR) daytime data was developed, evaluated and presented. Dynamic thresholding was used with channell, 2 and 3 to automatically create a cloud mask for a single image. Then the IO-day cloud coverage imagery was generated over the whole Asian region along with cloud-free composite imagery. Finally the monthly based statistics were computed based on the derived cloud coverage imagery in terms of land cover and country. As a result, it was found that 20-day is required to acquire the cloud free data over the whole Asia using NOAA AVHRR. The to-day cloud coverage and cloud-free composite imagery derived in this research is available via the web-site http://webpanda.iis.u-tokyo.ac.jp/CloudCover/.

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Geometric Correction of the NOAA/AVHRR Imagery (NOAA/AVHRR 영상의 기하학적 보정)

  • 서명석;신경섭;박경윤
    • Korean Journal of Remote Sensing
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    • v.6 no.1
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    • pp.25-37
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    • 1990
  • Methods of geometric correction for the Advanced Very High Resolution Radiometer imagery of NOAA satellites were developed and applied to the software for image processing of meteorological satellite data. The software for finding the earth location of each scan position and the software for gridding on original imagery were dedigned. On the assumption of circular orbits and the spherical earth, the methods developed were sufficiently accurate in the purpose of most meteorological data analyses.

Land-cover Change detection on Korean Peninsula using NOAA AVHRR data (NOAA AVHRR 자료를 이용한 한반도 토지피복 변화 연구)

  • 김의홍;이석민
    • Spatial Information Research
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    • v.4 no.1
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    • pp.13-20
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    • 1996
  • This study has been on detection of land-cover change on Korean peninsula (including the area of north Korean territory) between May of 1990 year and that of 1995 year using NOAA AVHRR data. It was necessary that imagery data should be registered to each other and should not be deviated much in seasonal variation in order to recognize land - cover change. Atmosphic effect such as clould and dirt was erased by maximum NDVI(Normalized Difference Vegetation Index) method the equation of which was as following $$NDVI(i,j,d)=\frac{ch2(j,j,d)-ch1(i,j,d)}{ch2(i,j,d)+ch1(i.j,d)}$$ Each image of maximum NDVI of '90 year and '95 year was c1assifed onto 8 categories ,using iso-clustering method each of which was water, wet barren and urban, crop field, field, mixed vegetation, shrub, forest and evergreen.

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The research evaluation of shadow influence in NOAA AVHRR data (NOAA AVHRR 자료에서 구름으로 인한 그림자 영향에 관한 조사)

  • Kim, Dong-Hee;Ryutaro, Tateishi;Choi, Seung-Pil;Choi, Chul-Soon
    • Proceedings of the Korean Society of Surveying, Geodesy, Photogrammetry, and Cartography Conference
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    • 2004.11a
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    • pp.281-284
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    • 2004
  • 광범위한 면적의 토지피복분류를 관찰하는데 유용하게 사용되고 있는 NOAA AVHRR 자료는 자료의 방대한 양과 구름에 의한 영향을 없애기 위하여 일반적으로 MVC(Maximum Value Composite) 처리를 하여 사용한다. 그러나 수신당시의 여러 가지 환경인자(구름, 저주파 노이즈, 산란, 구름의 그림자 등)에 의하여 각 채널의 패턴이 변화하여 오독을 할 위험성이 있다. 특히 그림자의 영향에 의해 측정치가 변화하는 NOAA 위성의 채널2영역에서는 이러한 특징이 두드러진다. 따라서 본 연구에서는 지상에서 실제로 측정한 자료를 기초로 하여 NOAA 영상자료에서 구름으로 인한 그림자의 영향에 관하여 조사하였고, 한 픽셀안에서 그림자의 영향이 60%이상이 될 경우에는 오독의 가능성이 높은 것으로 나타났다.

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Remote Sensing Data receiving and research activities using NOAA-AVHRR and Terra/Aqua-MODIS at ACRoRS, AIT

  • PHONEKEO Vivarad;SAMARAKOON Lal;YOKOYAMA Ryuzo
    • Proceedings of the KSRS Conference
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    • 2004.10a
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    • pp.31-33
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    • 2004
  • Two receiving systems were established at the Asian Center for Research on Remote Sensing (ACRoRS) to receive remote sensing data from NOAA AVHRR and Terra/Aqua MODIS sensors in October 1997 and May 2001, respectively. The data, which has been received in the research center, are very important to support and promote the remote sensing research activities for global environmental issues in Asia. Since the day of the establishment, many research and applications, which used these data, have been conducted. The data sets have been provided to researchers and users in many countries in the region to conduct research, to strengthen the research collaboration and education.

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An Approach to Measurement of Water Quality Factors and its Application Using NOAA satellite Data

  • Jang, Dong-Ho;Jo, Gi-Ho;Chi, Kwang-Hoon
    • Proceedings of the KSRS Conference
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    • 1999.11a
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    • pp.363-370
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    • 1999
  • Remotely sensed data is regarded as a potentially effective data source for the measurement of water quality and for the environmental change of water bodies. In this study, we measured the spectral reflectance by using multi-spectral image of low resolution camera(LRC) which will be loaded in the OSMI multi-purpose satellite(KOMPSAT) scheduled to be launched on 1999 to use the data in analyzing water pollution. We also investigated the possibility of extraction of water quality factors in water bodies by using remotely sensed low resolution data such as NOAA/AVHRR. In this study, Shiwha-District and Sang-Sam Lake was set up as the subject areas for the study. In this part of the study, we measured the spectral reflectance of the water surface to analyze the radiance of the water bodies in low resolution spectral band and tried to analyze the water quality factors in water bodies by using radiance feature from another remotely sensed data such as NOAA/AVHRR. As the method of this study, first, we measured the spectral reflectance of the water surface by using SFOV( Single Field of View) to measure the reflectance of water quality analysis from every channel in LRC spectral band(0.4~O.9${\mu}{\textrm}{m}$). Second, we investigated the usefulness of ground truth data and the LRC data by measuring every spectral reflectance of water quality factors. Third, we analyzed water quality factors by using the radiance feature from another remotely sensed data such as NOAA/AVHRR. We carried out ratio process of what we selected Chlorophyll-a and suspended sediments as the first factors of the water quality. The results of the analysis are below. First, the amount of pollutants of Shiwha-Lake has been increasing every you since 1987 by factors of eutrophication. Second, as a result of the reflectance, Chlorophyll-a represented high spectral reflectance mainly around 0.52${\mu}{\textrm}{m}$ of green spectral band, and turbidity represented high spectral reflectance at 0.57${\mu}{\textrm}{m}$. But suspended sediments absorbed high at 0.8${\mu}{\textrm}{m}$. Third, Chlorophyll-a and suspended sediments could have a distribution chart as a result of the water quality analysis by using NOAA/AVHRR data.

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Relations NOAA/AVHRR SST between Migratory Fishes in the Korean Seas (NOAA/AVHRR SST 자료를 이용한 한반도 주변해역에서의 수온과 어장변화특성 연구)

  • Seo, Won-Chan;Yoon, Hong-Joo
    • Journal of the Korea Institute of Information and Communication Engineering
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    • v.12 no.12
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    • pp.2265-2270
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    • 2008
  • It was studied to the displacement and the amount of catch for migratory fishes with NOAA/AVHRR SST(Sea Surface Temperature) from 1988 to 2000 in the Korean Seas. The analyzed results from SST data showed generally the oceanic warming trend in the Korean Seas. On the increasement of SST, the distributed areas of migratory fishes which living in the warm waters were displaced gradually to the northward directions(high latitude) and then the amount of catch was increased during this studied periods against to migratory fishes which living in the cold waters.

Estimation of Transparency from the AVHRR Channel 1 Digital Number of NOAA Satellite in the southeastern Yellow Sea (NOAA 원격자료에 의한 황해 남동부 투명도의 추정)

  • 서영상;한상복;강용균
    • Korean Journal of Remote Sensing
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    • v.9 no.2
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    • pp.1-5
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    • 1993
  • Real time transparency estimation method was studied using AVHRR Channel 1 (Visible band, 0.58 - 0.68 $\mu\textrm{m}$) digital number (DN) of NOAA Satellite. The relationshop between the measured transparency and the digital number shows following exponential equation in the southeastern Yellow Sea : Tr = 4820 $\times$ exp (-0.082 $\times$ DN), 77 $\leq$ DN < 105 where Tr is the transparency in meters and DN is the digital number of AVHRR Channel 1. From this equation, real time transparency can be simply estimated using data from the NOAA Ground Station of National Fisheries Research and Development Agency.

Analysis of Drought Detection and Propagation Using Satellite Data (인공위성 영상 정보를 이용한 가뭄상황 및 징후분석)

  • Shin, Sha-Chul;Eoh, Min-Sun
    • Journal of the Korean Society of Hazard Mitigation
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    • v.4 no.2 s.13
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    • pp.61-69
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    • 2004
  • Drought is one of the mai or environmental disasters. Weather data, particularity rainfall, are currently the primary source of information widely used for drought monitoring. However, weather data are often from a very sparse meteorological network. Therefore, data obtained from the Advanced Very High Resolution Radiometer(AVHRR) sensor boarded on the NOAA polar-orbiting satellites have been studied as a tool for drought monitoring. The normalized difference vegetation index(NDVI) and vegetation condition index(VCI) were used in this study. Also, a simple method to detect drought Is Proposed based on climatic water balance using NOAA/AVHRR data. The results clearly show that temporal and spatial characteristics of drought in Korea can be detected and mapped by the moisture index.

Monitoring of Agriculture land in Egypt using NOAA-AVHRR and SPOT Vegetation data

  • Shalaby, A.;Ghar, M. Aboel;Tateishi, R.
    • Proceedings of the KSRS Conference
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    • 2003.11a
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    • pp.18-20
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    • 2003
  • Land cover change detection is one of the most important trends in which remote sensing data could be used to assist strategists and the planners to decide the best land use policy. Two images of NOAA-AVHRR and SPOT vegetation acquired in November 1992 and 2002 were used to assess the changes of Agricultural lands in Egypt. A supervised classification together with two change images derived from classification result and NDVI were used to evaluate the trend and form of the change. It was found that agricultural areas increased by about 14.3 % during the study period in particular around the River Nile Delta and near the Northern Lakes of Egypt. The new cultivated lands were extracted mainly from the desert and from the salt marches areas. At the same time, parts of the agricultural lands were turned into non-cultivated land because of the urban expansion and soil degradation.

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