• 제목/요약/키워드: Cold Pixel

검색결과 12건 처리시간 0.027초

Dead Pixel Detection Method by Different Response at Hot & Cold Images for Infrared Camera

  • Ye, Seong-Eun;Kim, Bo-Mee
    • 한국컴퓨터정보학회논문지
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    • 제23권11호
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    • pp.1-7
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    • 2018
  • In this paper, we propose soft dead pixels detection method by analysing different response at hot and cold images. Abnormal pixels are able to effect detecting a small target. It also makes confusing real target or not cause of changing target size. Almost exist abnormal pixels after image signal processing even if dead pixels are removed by dead pixel compensation are called soft dead pixels. They are showed defect in final image. So removing or compensating dead pixels are very important for detecting object. The key idea of this proposed method, detecting dead pixels, is that most of soft deads have different response characteristics between hot image and cold image. General infrared cameras do NUC to remove FPN. Working 2-reference NUC must be needed getting data, hot & cold images. The way which is proposed dead pixel detection is that we compare response, NUC gain, at each pixel about two different temperature images and find out dead pixels if the pixels exceed threshold about average gain of around pixels.

모바일 카메라 화질 개선을 위한 실시간 불량 화소 검출 및 보정 시스템의 설계 (Design of Real-Time Dead Pixel Detection and Compensation System for Image Quality Enhancement in Mobile Camera)

  • 송진근;하주영;박정환;최원태;강봉순
    • 융합신호처리학회논문지
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    • 제8권4호
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    • pp.237-243
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    • 2007
  • 본 논문은 모바일 카메라 화질 개선을 위한 실시간 불량 화소(Dead pixel) 검출 및 보정 시스템에 대해 제안하고 있다. 영상 입력장치인 CIS(CMOS Image Sensor)는 소형화, 저전력, 비용절감의 효과로 각광받고 있다. 하지만 이미지 센서와 결합된 불량 화소 보정 장치에 관한 기존 방법에 있어서, 연속된 불량 화소들을 검출하지 못 하거나, 정상화소임에도 불구하고 불량 화소로 분류하여 영상이 훼손되는 경우가 발생한다. 제안된 알고리즘은 불량 화소를 핫 픽셀(Hot pixel)과 콜드 픽셀(Cold pixel)로 분류하여, 라인 검출방법과 $5{\times}5$ 창 검출 방법을 순차적으로 처리하여, 불량화소의 특성에 따라 검출 및 보정하는 방법을 제안한다. 라인 검출 알고리즘은 수평 저주파 영역의 불량화소를 검출한다. 그리고 $5{\times}5$창 검출 알고리즘은 수직, 대각 저주파 영역과 고주파 영역에 대한 불량 화소를 검출한다. 제안된 알고리즘은 시뮬레이션 결과, 99%의 높은 검출율을 보여주고 있다. 그리고 Verilog-HDL를 사용하여 구현하였고 Synopsys의 Design Analyzer와 TSMC 0.25um ASIC library로 합성하였으며, 총 Gate counts는 23K로 낮은 하드웨어 복잡도를 가진다.

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Brightness Temperature Retrieval using Direct Broadcast Data from the Passive Microwave Imager on Aqua Satellite

  • Kim, Seung-Bum;Im, Yong-Jo;Kim, Kum-Lan;Park, Hye-Sook;Park, Sung-Ok
    • 대한원격탐사학회지
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    • 제20권1호
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    • pp.47-55
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    • 2004
  • We have constructed a level-1 processor to generate brightness temperatures using the direct-broadcast data from the passive microwave radiometer onboard Aqua satellite. Although 50-minute half-orbit data, called a granule, are being routinely produced by global data centers, to our knowledge, this is the first attempt to process 10-minute long direct-broadcast (DB) data. We found that the processor designed for a granule needs modification to apply to the DB data. The modification includes the correction to path number, the selection of land mask and the manipulation of dummy scans. Pixel-to-pixel comparison with a reference indicates the difference in brightness temperature of about 0.2 K rms and less than 0.05 K mean. The difference comes from the different length of data between 50-minute granule and about 10-minute DB data. In detail, due to the short data length, DB data do not always have correct cold sky mirror count. The DB processing system is automated to enable the near-real time generation of brightness temperatures within 5 minutes after downlink. Through this work, we would be able to enhance the use of AMSR-E data, thus serving the objective of direct-broadcast.

SEBAL 모형과 Terra MODIS 영상을 이용한 혼효림, 논 지역에서의 공간증발산량 산정 연구 (Estimation of spatial evapotranspiration using Terra MODIS satellite image and SEBAL model in mixed forest and rice paddy area)

  • 이용관;정충길;안소라;김성준
    • 한국수자원학회논문집
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    • 제49권3호
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    • pp.227-239
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    • 2016
  • 본 연구는 Surface Energy Balance Algorithm for Land (SEBAL) 모형을 이용해 국내의 혼효림(설마천)과 논(청미천) 유역에 대해 일 증발산량을 산정하고 각 유역의 플럭스 타워 실측 증발산량과 비교하였다. SEBAL 모형의 입력 자료로 위성자료는 2개년(2012-2013)의 Terra MODIS product 중 Albedo, Land Surface Temperature (LST), Normalized Difference Vegetation Index (NDVI)를 활용하였으며, 기상자료는 유역 인근에 위치한 기상청 기상관측소로부터 풍속, 일사량 자료를 제공받아 공간 내삽(Interpolation)하여 활용하였다. 모의결과 플럭스 타워의 연평균 증발산량은 설마천에서 302.8 mm, 청미천에서 482.0 mm, SEBAL 모의 증발산량은 각각 183.3 mm, 371.5 mm로 산정되었다. 전체 모의기간에 대한 SEBAL 모의 증발산량의 실측 증발산량과의 결정계수는 설마천 플럭스 타워에서 0.54, 청미천 플럭스 타워에서 0.79로 나타났다. 두지점에서 SEBAL 모의 증발산량이 과소 추정된 주된 이유로는 일별 hot pixel과 cold pixel로부터 산정한 현열 플럭스의 과대추정으로 인한 것으로 판단된다.

DETECTION AND MASKING OF CLOUD CONTAMINATION IN HIGH-RESOLUTION SST IMAGERY: A PRACTICAL AND EFFECTIVE METHOD FOR AUTOMATION

  • Hu, Chuanmin;Muller-Karger, Frank;Murch, Brock;Myhre, Douglas;Taylor, Judd;Luerssen, Remy;Moses, Christopher;Zhang, Caiyun
    • 대한원격탐사학회:학술대회논문집
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    • 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume II
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    • pp.1011-1014
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    • 2006
  • Coarse resolution (9 - 50 km pixels) Sea Surface Temperature satellite data are frequently considered adequate for open ocean research. However, coastal regions, including coral reef, estuarine and mesoscale upwelling regions require high-resolution (1-km pixel) SST data. The AVHRR SST data often suffer from navigation errors of several kilometres and still require manual navigation adjustments. The second serious problem is faulty and ineffective cloud-detection algorithms used operationally; many of these are based on radiance thresholds and moving window tests. With these methods, increasing sensitivity leads to masking of valid pixels. These errors lead to significant cold pixel biases and hamper image compositing, anomaly detection, and time-series analysis. Here, after manual navigation of over 40,000 AVHRR images, we implemented a new cloud filter that differs from other published methods. The filter first compares a pixel value with a climatological value built from the historical database, and then tests it against a time-based median value derived for that pixel from all satellite passes collected within ${\pm}3$ days. If the difference is larger than a predefined threshold, the pixel is flagged as cloud. We tested the method and compared to in situ SST from several shallow water buoys in the Florida Keys. Cloud statistics from all satellite sensors (AVHRR, MODIS) shows that a climatology filter with a $4^{\circ}C$ threshold and a median filter threshold of $2^{\circ}C$ are effective and accurate to filter clouds without masking good data. RMS difference between concurrent in situ and satellite SST data for the shallow waters (< 10 m bottom depth) is < $1^{\circ}C$, with only a small bias. The filter has been applied to the entire series of high-resolution SST data since1993 (including MODIS SST data since 2003), and a climatology is constructed to serve as the baseline to detect anomaly events.

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Development of the Near Infrared Camera System for Astronomical Application

  • 문봉곤
    • 천문학회보
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    • 제35권1호
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    • pp.39.2-39.2
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    • 2010
  • In this paper, I present the domestic development of near infrared camera systems for the ground telescope and the space satellite. These systems are the first infrared instruments made for astronomical observation in Korea. KASINICS (KASI Near Infrared Camera System) was developed to be installed on the 1.8m telescope of the Bohyunsan Optical Astronomy Observatory (BOAO) in Korea. KASINICS is equipped with a $512{\times}512$ InSb array enable L band observations as well as J, H, and Ks bands. The field-of-view of the array is $3.3'{\times}3.3'$ with a resolution of 0.39"/pixel. It employs an Offner relay optical system providing a cold stop to eliminate thermal background emission from the telescope structures. From the test observation, limiting magnitudes are J=17.6, H=17.5, Ks=16.1 and L(narrow)=10.0 mag at a signal-to-noise ratio of 10 in an integration time of 100 s. MIRIS (Multi-purpose InfraRed Imaging System) is the main payload of the STSAT-3 in Korea. MIRIS Space Observation Camera (SOC) covers the observation wavelength from $0.9{\mu}m$ to $2.0{\mu}m$ with a wide field of view $3.67^{\circ}{\times}3.67^{\circ}$. The PICNIC HgCdTe detector in a cold box is cooled down below 100K by a micro Stirling cooler of which cooling capacity is 220mW at 77K. MIRIS SOC adopts passive cooling technique to chill the telescope below 200K by pointing to the deep space (3K). The cooling mechanism employs a radiator, a Winston cone baffle, a thermal shield, MLI of 30 layers, and GFRP pipe support in the system. Opto-mechanical analysis was made in order to estimate and compensate possible stresses from the thermal contraction of mounting parts at cryogenic temperatures. Finite Element Analysis (FEA) of mechanical structure was also conducted to ensure safety and stability in launching environments and in orbit. MIRIS SOC will mainly perform the Galactic plane survey with narrow band filters (Pa $\alpha$ and Pa $\alpha$ continuum) and CIB (Cosmic Infrared Background) observation with wide band filters (I and H) driven by a cryogenic stepping motor.

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RETRIEVAL OF LAND SURFACE TEMPERATURE FROM MTSAT-1R

  • Kwak, Seo-Youn;Suh, Myoung-Seok;Kang, Jeon-Ho;Kwak, Chong-Heum;Kim, Chan-Soo
    • 대한원격탐사학회:학술대회논문집
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    • 대한원격탐사학회 2006년도 Proceedings of ISRS 2006 PORSEC Volume I
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    • pp.250-252
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    • 2006
  • The land surface temperature (LST) can be defined as a weighted average temperature of components which constitute a pixel. The coefficients of split-window algorithm for MTSAT-1R were obtained by means of a statistical regression analysis from radiative transfer simulations using MODTRAN 4.0 for a wide range of atmospheric, satellite viewing angle (SVA) and lapse rate conditions. 6 types of atmospheric profile data imbedded in the MODTRAN 4 are used for the radiative transfer simulations. The RMSE is clearly larger on warm and humid profiles than cold and dry profiles, especially when the satellite viewing angle and lapse rate are large. The derivation of LST equations according to the atmospheric profiles clearly decreased the RMSE without regard to the SVA and lapse rate. The bias and RMSE are decreased as the more controls factors included. This preliminary result indicates that the characteristics of atmosphere, SVA and lapse rate should be included in the LST equation.

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Retrieval of land Surface Temperature from MTSAT-1R

  • Kwak, Seo-Youn;Suh, Myoung-Seok;Kang, Jeon-Ho;Kwak, Chong-Heum;Kim, Chan-Soo
    • 대한원격탐사학회지
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    • 제22권5호
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    • pp.385-388
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    • 2006
  • The land surface temperature (LST) can be defined as a weighted average temperature of components which constitute a pixel. The coefficients of split-window algorithm for MTSAT-1R were obtained by means of a statistical regression analysis from radiative transfer simulations using MODTRAN 4.0 for a wide range of atmospheric, satellite viewing angle (SVA) and lapse rate conditions. 6 types of atmospheric profile data imbedded in the MODTRAN 4 are used for the radiative transfer simulations. The RMSE is clearly larger on warm and humid profiles than cold and dry profiles, especially when the satellite viewing angle and lapse rate are large. The derivation of LST equations according to the atmospheric profiles clearly decreased the RMSE without regard to the SVA and lapse rate. The bias and RMSE are decreased as the more controls factors included. This preliminary result indicates that the characteristics of atmosphere, SVA and lapse rate should be included in the LST equation.

A Improved Scene based Non-uniformity Correction Algorithm for Infrared Camera

  • Hyun, Ho-Jin;Choi, Byung-In
    • 한국컴퓨터정보학회논문지
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    • 제23권1호
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    • pp.67-74
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    • 2018
  • In this paper, we propose an efficient scene based non-uniformity correction algorithm which performs the offset correction using the uniform obtained from input scenes for Infrared camera. In general, pixel outputs of a infrared detector can not be uniform. Therefore, the non-uniformity correction procedure need to be performed to make the image outputs uniform. A typical non-uniformity correction method uses a black body at the laboratory to obtain the output of the infrared detector's pixels for two temperatures, HOT and COLD, and calculates the non-uniformity correction parameters. However, output characteristics of the Infrared detector changes while the Infrared camera is operated, the fixed pattern noise of the Infrared detector and dead pixels are generated. To remove the noise, the offset correction is generally performed. The offset correction procedure usually need the additional device such as a thermo-electric cooler, shutter, or non-uniformity correction lens. Therefore, we introduce a general scene based non-uniformity correction technique without additional equipment, and then we propose an improved non-uniformity correction algorithm based on image to solve the problem of the existing technique.

IKONOS 스테레오 영상의 매칭사이즈 결정연구 (A Study on Determination of the Matching Size of IKONOS Stereo Imagery)

  • 이효성;안기원;이창노;서두천
    • 한국측량학회:학술대회논문집
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    • 한국측량학회 2007년도 춘계학술발표회 논문집
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    • pp.201-205
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    • 2007
  • In the post-Cold War era, acquisition technique of high-resolution satellite imagery (HRSI) has begun to commercialize. IKONOS-2 satellite imaging data is supplied for the first time in the 21st century. Many researchers testified mapping possibility of the HRSI data instead of aerial photography. It is easy to renew and automate a topographical map because HRSI not only can be more taken widely and periodically than aerial photography, but also can be directly supplied as digital image. In this study matching size of IKONOS Geo-level stereo image is presented lot production of digital elevation model (DEM). We applied area based matching method using correlation coefficient of pixel brightness value between the two images. After matching line (where "matching line" implies straight line that is approximated to complex non-linear epipolar geometry) is established by exterior orientation parameters (EOPs) to minimize search area, the matching is tarried out based on this line. The experiment on matching size is performed according to land cover property, which is divided off into four areas (water, urban land, forest land and agricultural land). In each of the test areas, window size for the highest correlation coefficient is selected as propel size for matching. As the results of experiment, the proper size was selected as $123{\times}123$ pixels window, $13{\times}13$ pixels window, $129{\times}129$ pixels window and $81{\times}81$ pixels window in the water area, urban land, forest land and agricultural land, respectively. Of course, determination of the matching size by the correlation coefficient may be not absolute appraisal method. Optimum matching size using the geometric accuracy therefore, will be presented by the further work.

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