14 November 2014 Monitoring of COMS MI visible channel degradation based on Moon observations
Author Affiliations +
Most of the current space-borne visible imagers on a geosynchronous orbit (GEO), which do not have onboard calibration devices, use a vicarious calibration. For a meteorological payload on a GEO satellite, lunar calibration is often used. The meteorological imager (MI) on the communication, ocean, and meteorological satellite (COMS) has been successfully operated for half of its entire mission lifetime (∼7  years). The visible channel of the MI uses the lunar calibration to monitor its degradation. The degradation rate of the instrument was monitored using the ratio between the calculated radiance of the Moon from the Robotic Lunar Observatory (ROLO) model and the observed radiance from the MI. Analyses of the 42-month Moon image data showed that the instrument’s mean degradation rate was about 1.88%. These values confirmed the outstanding performance of the COMS MI visible channel compared with that of the GOES-10 imager.



The visible channels of most of the operating meteorological imagers (MIs) on geosynchronous (GEO) satellites do not have onboard calibration targets and use a vicarious calibration.1 Homogeneous and stable targets such as the Moon, Dome-C (in a polar region), a desert, and deep convective clouds are used for vicarious calibration.2,3 Among these targets, Dome-C and desert sites have an advantage in that they can be used for both visible and near-infrared channels.2 However, there are some limitations: the revisit time for the low Earth orbit satellite measurements and nonaccessible areas for the GEO-based observations. Deep convective cloud targets require both infrared and visible channels data.3 On the other hand, lunar calibration has many advantages. In particular, the Moon surface plays the role of a robust calibration target due to its similar brightness to the land of Earth except for the cloudy regions.4 In addition, the Moon does not have an atmospheric effect, which accounts for an erroneous impact on the measurement from the imager.

The International Satellite Cloud Climatology Project (ISCCP), led by the US, the EU, Japan, and China (1983 to present), gathers Earth radiance data and conducts a routine vicarious calibration on the visible channels of the various GEO satellites. Moon measurement data acquired from the advanced very high-resolution radiometer and the moderate resolution imaging spectrometer (MODIS) are used. Moon observations from a total of 10 satellites (from a minimum of 5 to maximum of 27 Moon image data per satellite) are usually used for the vicarious calibrations.5 For the trend of monitoring the visible instrument of sea-viewing wide field-of-view sensor, a lunar calibration method was also adopted.1 The lunar calibration overcomes an intrinsic limitation of comparing data with different temporal and spatial characteristics driven by the satellite viewing geometries.6 The measured relative calibration accuracy regarding the GOES-10 was 0.1% compared with the vicarious calibration result of MODIS.7 At least one Moon image acquisition per month is recommended.5 Usually two to four times Moon observations per month are available for space-borne visible imagers.7

The MI on the COMS has been operating successfully since its launch (June 27, 2010). It monitors meteorological phenomena 24/7 using one visible and four infrared channels.8 Lunar calibration has been implemented on the MI based on a robotic lunar observatory (ROLO) model to monitor MI visible-channel degradation. Forty-two months of Moon images acquired from the MI were investigated.


Visible Channel Performance-Degradation Analysis Based on a Robotic Lunar Observatory Model

The Moon can be used to monitor the degradation of satellite instruments with sufficient accuracy. The stable lunar surface provides a reliable means for calibration of Earth-viewing imagers. For the calibration of space-borne imagers with a reliable “ground truth,” the United States Geological Survey developed a model known as ROLO,9 which uses the Moon images to analyze the in-orbit response characteristics of the NASA Earth observing system satellite payloads.

Computed radiances of the Moon based on a ROLO model, which uses the Sun/Moon/satellite distances, play a role in reference values. However, the observed radiances of the Moon from the imager contain actual degradation information on the instrument for the visible channel. Therefore, the degradation of the visible channel can be computed simply by using the ratio between two radiances (irradiance from a statistical model and one from the imager).7 In this section, we describe how the visible channel degradation rate is computed.


Computation of the Moon’s Irradiance Based on the Robotic Lunar Observatory Model

When the distances among the Sun, Moon, and satellite are known, the irradiance of the Moon is computed as10



When the locations of the Sun, Moon, and satellite are determined, the Moon-satellite distance [dMC(km)] and Moon-Sun distance [dMS(AU)] are computed. The irradiance based on the ROLO model [IROLO(Wm2μm1)] is computed by integrating all the individual irradiances, I, over the entire spectral range of the visible channel (550 to 800 nm). Then it is normalized by the instrument’s spectral response function, as shown in Eq. (2):6



The ROLO irradiance as a function of the effective disk reflectance A(λ) for a given wavelength is calculated as6



Here, A(λ) is the disk-equivalent reflectance, ΩM is the solid angle of the Moon at a standard distance (6.4236×105sr),7 and ESUN(λ) is the solar spectral irradiance (Wm2μm1). The disk-equivalent reflectance A(λ) in Eq. (3) is defined as10

where g is the absolute phase angle (rad), θ and φ are the selenographic latitude and longitude of the satellite (deg), and Φ is the selenographic longitude of the Sun (rad). To determine the disk-equivalent reflectance, the observation times of the Sun, Moon, and satellite are required and Earth-centered Earth-fixed (ECEF) coordinates need to be converted to Moon-centered Moon-fixed (MCMF) coordinates.11


Irradiance Computation Based on the Acquired Moon Images

The instrumental irradiance [Iinst(Wm2μm1)] based on the observed Moon image in which the radiometric correction process has been completed is computed as5


where ΩP is the solid angle (sr) of a pixel corresponding to one visible detector (28μrad), i is the pixel in the Moon image, and NMoon is the total number of pixels in the lunar disk image. Li is an individual pixel radiance measurement of the Moon (Wm2μm1), τ(=16/18) is the ratio corresponding to the oversampling by the MI along the E-W axis, S is the slope value in a radiometric calibration equation of the visible channel, Xi is the raw number of counts from the detector, and X¯SP is the average raw number of counts from space-look observations.


Degradation Rate Computation

It is assumed that the degradation of the instrument is reflected in the Earth- and space-look observation data from the imager. The ratio P between the Moon irradiance measured from the imager and the model-based reference irradiance7


shows the degradation trend over time.7

Here, Iinst is the Moon irradiance measured by the MI and Iref is the Moon irradiance computed from the ROLO model under the same conditions. Therefore, the long-term time series of P can be interpreted as a linear trend of the visible channel degradation.


Implementation for the COMS MI

The procedures of lunar calibration implemented in the COMS MI visible channel are described.


Moon Observation Time and Estimation of the Sun/Moon/Satellite Locations

The flight dynamic subsystem (FDS) of COMS generates the predicted locations of the Sun/Moon/satellite system at 30/30/15-s intervals, respectively. The duration of Moon measurement time from the COMS MI is about 47 s. The UTC time when the center of the Moon is scanned by the MI is used as the reference time. With this reference time, the positions of Sun/Moon/satellite are determined using the predicted data from the FDS.11 The reference time must be converted to Julian Century (t) to compute the ROLO model-based location of the Moon.11,12


Effective Moon Image Cropping and Direct Histogram Specification Process

The original pixel size of the Moon image acquired from the MI visible channel is 2080×1200. This image includes many parts of the space area observations. In the calibration process, the reduced effective image (560×352pixels) on which the Moon is centered is used. The COMS MI images were acquired from the repetitive motions of the scanner with the eight detectors located vertically.8 The performances of the eight detectors were slightly different from the initial operation period; hence, the degradation rates also differ from each other. The Moon images compensated (normalized) by the best detector based on the direct histogram specification (DHS) were used in the analyses (Fig. 1).13

Fig. 1

Compensation of the relative difference between detectors using direct histogram specification (DHS).


Figure 1 illustrates a method for compensating the relative degradation differences among the eight detectors: (1) Separation of the Moon image according to each detector, (2) selection of the best (reference) detector d2, (3) application of the DHS to the remaining detectors, and (4) generation of the Moon image normalized by the reference detector.


Refinement of the Moon Image Samples Based on the Absolute Phase Angles

Figure 2 shows the computed reference irradiance Iref and the absolute phase angle g of the Moon.11 On a daily basis, these two values (red; right Y-axis and blue; left Y-axis) are computed using the Analytical Graphics Inc., satellite tool kit based on the geolocation information of the Sun/Moon/COMS satellite system with ECEF coordinates at 00:00:00 (UTC). The coordinates of the Sun and Moon were obtained from the DE405 ephemeris data of the Jet Propulsion Laboratory.14 A two-body motion equation was employed by assuming that there were some maneuvers (e.g., station keeping) of the COMS spacecraft for an orbit adjustment.

Fig. 2

Moon irradiance and absolute phase angles computed from satellite tool kit (January to March 2010).


Figure 2 indicates that there is a cycle in the values: Iref, g. Meaningful irradiances of the Moon are represented in certain ranges. Therefore, only data within 5 deg to 45 deg were selected for the Moon’s irradiance computation. Since the monthly lunar observation times were not consistent and some measurement data were excluded due to the phase-angle criteria, the Moon observation time was converted into Julian Century format to remove this dependence on the time interval.


Computation of the Individual Detector’s Degradation

When the relative degradation of the eight detectors was compensated using the DHS technique, the detector, which shows the lowest degradation rate, was selected as a baseline detector.13 Consequently, the radiometric characteristics of the entire Moon image were transformed to that of the baseline detector. The entire procedure for computing the degradation of the COMS MI visible channel based on the optimized Moon data, which are described in Secs. 2 and 3, is summarized in Fig. 3.

Fig. 3

Visible channel degradation monitoring method using the Moon image.


The COMS MI visible channel degradation is represented by P, which is a ratio between two irradiances: the Moon irradiance based on the ROLO model and the observed irradiance from the MI. In the computation, only data that meet the absolute phase angle criteria (5 deg to 45 deg) were used.

During the computation of the Moon’s irradiances, conversion of the Julian Century for the Moon measurement time tMC and matrices for MCMF conversion are required. During the Moon irradiance computation using the observed Moon image, P was computed using the relative degradation compensation technique, DHS, for all eight detectors (repeat eight times for * in Fig. 3). Finally, the first-order linear trend was obtained for the COMS MI visible channel with the computed P over the COMS mission period (2010 to present).



Implementation of the computation of Moon irradiance based on the COMS MI is described in this section.


Data for the MI Lunar Calibration

For the MI visible channel degradation analyses, a total of 42 months of Moon observation (July 2010 to December 2013) data from the COMS MI were used. Moon image acquisition was not performed for two cases (October 2010 and January 2011). The total number of Moon image samples was 40, and the intervals of the acquisitions were a minimum of 14 days and a maximum of 55 days. The available opportunity for effective Moon observations at a geostationary orbit was from two to four times per month.7 However, due to constraints on the lunar observations such as a full-disk observation time interval (every 3 h) and the station-keeping maneuvers, at least one lunar measurement per month from the COMS routine operation is not guaranteed. As a result, a special Moon measurement planning using a local area (LA) observation mode was applied in the MI during the COMS normal operation (starting from April 1, 2011).15 Monthly Moon image acquisition using the MI LA mode was conducted twice for a 1-h duration. Either of the two images was appropriate for the analyses because the Sun/Moon/satellite location change is negligible during this period. However, when space-look (for calibration) was performed during the Moon image acquisition, inconsistency between the line-by-line measurements from the MI scanning occurred (Fig. 4).

Fig. 4

Space-look measurement performed during Moon image acquisition (July 28, 2010, 05:26:03 UTC).


During the whole COMS operation period (July 2010 to present), only one case (July 28, 2010, 05:26:03 UTC), which contains the space-look observation, was found. In this case, an alternative observation (04:15:23 UTC) was used. The size of images taken for the lunar calibration was reduced to focus only on the Moon-centered area (560×352pixels; Fig. 5).

Fig. 5

Extracted 560×352-pixel image (with the Moon centered) for the analysis.



Selected Data Using the Phase-Angle Criteria

First, the absolute phase angle of the Moon was calculated based on the observation time. Moon images, which were not attributed to the phase angle criteria (5 deg to 45 deg), were removed from the analyses. Sixteen out of a total of 40 Moon samples were screened out. The phase angles of the eliminated images are indicated in Fig. 6. After this data selection process, the Moon image acquisition intervals were 26 to 122 days.

Fig. 6

Moon samples eliminated based on the phase-angle criteria.



Julian Century Conversion

For the visible channel’s degradation trend analysis with a first-order linear regression, the Moon measurement time was converted to a Julian Century to remove the dependency of the observation interval. In addition, it was normalized by indicating the degradation rate, P, from 0 to 1.


Moon Irradiance Computation Based on the Robotic Lunar Observatory Model

Table 1 shows an example of the Moon irradiance computation (ROLO model-based) intermediate results.11 Data taken on July 28, 2010, (04:16:08 UTC) were used.

Table 1

Intermediate results for the Moon irradiance (July 28, 2010, 04:16:08 UTC) computed based on the ROLO model.

tMCMoon observation time, UTCJuly 28, 2010, 04:16:08
tMoon observation time, Julian Century0.10569
t^Normalized t(0.0  ≤t^≤1.0)0.00000
rSunECEFSun’s position at ECEF coordinate (m)−6.6535×1010, 1.2728×1011, 4.9486×1010
rMoonECEFMoon’s position at ECEF coordinate (m)3.0385×108, −2.6194×108, −6.0353×107
rCOMSECEFCOMS’s position at ECEF coordinate (m)−2.6082×107, 3.3126×107, 1.1623×104
rSunMCMFSun’s position at MCMF coordinate (m)1.4242×1011, −5.3857×1010, −1.7795×109
rCOMSMCMFCOMS’s position at MCMF coordinate (m)4.4408×108, 1.2184×107, −4.6958×107
gMoon’s absolute phase angle (rad)0.39927
dMCDistance between Moon and COMS (km)4.4672×105
dMSDistance between Moon and SUN (AU)1.01791
IROLOROLO irradiance (Wm−2 μm−1)2.5549×10−3
IRefReference lunar irradiance (Wm−2 μm−1)1.8258×10−3


Moon Irradiance Computation Using the Observed Moon Data with DHS

Moon image resizing for a selection of effective Moon regimes and normalization of detectors using the DHS scheme was applied to the Moon irradiance computation using the acquired COMS MI images. Figure 7 shows the result for a selected case (March 7, 2012, 02:58:43 UTC). The stripping effect that is observed in the left image was clearly eliminated by the normalization process with the reference detector (fourth detector).

Fig. 7

Moon images before and after application of the DHS.


Because the radiance of the Moon is sufficiently bright compared with that of deep space (cosmic background), the area of the Moon can be extracted with respect to space (Fig. 8). In Fig. 8, the deep-space region can be contrasted with the Moon. The left image shows the Moon in black, while the right image represents the Moon calibrated with DHS over a white-space background.

Fig. 8

Extracted Moon image.


Computation of the Moon irradiance (acquired from the MI) requires Eq. (4) and the DHS process. In the computation, the ΩP value was 7.84×1010sr, the instantaneous field-of-view was 28μrad of the COMS MI visible channel, and the oversampling ratio τ was 16/28 (horizontal sampling=16μrad and vertical sampling=28μrad).


Degradation Rates of Individual Detectors for the Visible Channels

Table 2 shows the results of the degradation rate and the first-order regression equation of each of the eight detectors. A total of 24 Moon samples within the phase angle range of 5 deg to 45 deg, which were observed from July 2010 to December 2013, were used for the analysis. The mean degradation rate for each Moon sample and the intermediate result are shown in Table 3.

Table 2

Degradation rates for eight individual detectors over a 42-month period (July 2010 to December 2013).

DetectorDegradation (%)Linear trend equation (first order)

Table 3

Mean degradation rates for each lunar observation.

tMC (UTC)dMC (km)dMS (AU)g (deg⁡)IRef (Wm−2 μm−1)NMoonIinst (Wm−2 μm−1)P
July 28, 2010, 04:16:084.4672×1051.0179122.876521.8258×10−3101,1471.6823×10−30.92139
August 24, 2010, 02:23:064.4705×1051.013748.526992.3618×10−3105,8722.4520×10−31.03818
November 18, 2010, 00:43:324.4238×1050.9905542.506559.1584×10−488,9551.1314×10−31.23534
March 20, 2011, 04:28:443.9808×1050.998027.854863.1670×10−3133,7173.0908×10−30.97593
April 17, 2011, 01:43:353.9922×1051.0059116.727922.7529×10−3130,0742.3982×10−30.87115
July 18, 2011, 05:13:324.3830×1051.0184934.551791.3994×10−397,7781.2440×10−30.88894
August 14, 2011, 03:13:334.3793×1051.015716.597922.6849×10−3109,3862.5957×10−30.96676
September 11, 2011, 01:43:344.4146×1051.0094316.386121.9087×10−3105,9721.9814×10−31.03813
October 11, 2011, 01:43:334.4703×1051.0011113.004572.0859×10−3104,9942.1334×10−31.02275
January 12, 2012, 06:28:434.1863×1050.9854637.941721.0894×10−3104,5431.2888×10−31.18300
February 8, 2012, 03:58:424.1596×1050.988806.753573.0702×10−3120,9562.9206×10−30.95130
March 7, 2012, 02:58:434.1198×1050.9947316.993262.5839×10−3121,3672.2284×10−30.86242
April 6, 2012, 02:13:344.0228×1051.0030811.781902.9132×10−3129,2062.6280×10−30.90207
May 4, 2012, 01:58:444.0227×1051.0104328.949611.9904×10−3120,9781.7380×10−30.87323
August 3, 2012, 03:43:354.2018×1051.0171113.801752.3734×10−3117,7492.2435×10−30.94527
September 3, 2012, 05:43:344.3724×1051.0108831.806751.3591×10−399,9291.3263×10−30.97585
October 27, 2012, 00:28:444.3766×1050.9960332.608461.3913×10−399,6881.4208×10−31.02121
January 1, 2013, 05:58:434.3560×1050.9852242.915198.9562×10−492,5291.0472×10−31.16922
March 24, 2013, 00:13:354.3170×1050.9988842.744531.4026×10−394,5231.1158×10−30.79553
May 22, 2013, 00:13:344.1366×1051.0140643.994171.1595×10−3100,9011.1333×10−30.97748
July 24, 2013, 04:13:344.0450×1051.0180520.243952.2320×10−3123,8862.0193×10−30.90469
August 21, 2013, 02:43:374.0668×1051.014045.849173.1874×10−3127,7853.0558×10−30.95872
September 21, 2013, 03:58:454.2328×1051.0063520.220661.9305×10−3114,3761.8861×10−30.97699
October 18, 2013, 01:58:444.2389×1050.9988212.071332.6017×10−3116,3012.3756×10−30.91307

In Table 2, t^ was converted from tMC to Julian Century t. Next, it was normalized by setting the first measurement (July 28, 2010, 04:16:08) to zero and the last measurement (2013.12.22 07:28:41) to one. As a result, the degradation rate of each detector can be determined by applying “t^=1.0” in the regression equation in Table 2. The overall mean degradation rate of the instrument over the 42-month period was 6.59% (1.88% per year).

Figure 9 shows the mean degradation trend of the COMS MI visible channel as a function of the time (normalized).

Fig. 9

Mean degradation rate of the meteorological imager (MI) visible-channel instrument.



Discussion and Conclusion

To quantitatively monitor the degradation of the COMS MI visible channel, a vicarious calibration using 42 months of Moon image data from the MI was conducted. Twenty-four Moon samples, which considered the effective Moon phase angles, were used. The Julian Century was used to remove the dependency on the measurement interval, and the DHS scheme was used to compensate a relative variation among the eight detectors.

The mean degradation rate of the MI visible channel instrument (Fig. 9) has a large fluctuation driven by the following reasons: (1) the reference irradiance (Iref) has a periodicity which has different shapes and maximum values,11 (2) the reference irradiance’s periodicity is about 29 days (Fig. 2), but the COMS MI obtains only one Moon image per 26 to 122 days (>14.5days). As a result, the mean degradation rate trend cannot be extracted in the shape of the reference irradiance due to aliasing characteristics, (3) the reference irradiance has a large variability at the time of COMS spacecraft’s orbit adjustment (wheel off-loading or station keeping), and (4) the measured irradiances by the MI (Iinst) contains errors driven by the pixel number on the boundary area between the Moon and Space,7 which is related to the shapes of the Moon.

The results showed that the overall degradation rate over half of the COMS mission lifetime (7years) was 6.59%, resulting in an annual degradation rate of 1.88%. This performance was much better than that of the GOES-10 imager (4.5%/year degradation based on a lunar calibration method7). In addition, the individual degradation rates of eight detectors were from 3.79% to 8.19% (σ=4.4%). This indicates that the difference between the best- and worst-performing detectors was about 1.26% per year.

The results of our study can be applied in two parts. First, radiometric calibration for the COMS MI could be conducted by compensating the S value with the difference (P1P8) in Eq. (4). Second, input values for Earth observations X and space-look measurements X¯SP in the radiometric calibration equation can be tuned based only on the degradation rate (average of 1.26% per year) of the baseline detector with the DHS process. Because this approach is performed for each measurement cycle, the radiometric calibration process, which is used for any space-borne visible imager with multiple detectors, can be improved.


The authors acknowledge J. Degremont and J.-L. Duquesne of Airbus Defense & Space (former EADS Astrium), Y.-R. Lee and D.-S. Kim of Satrec-Intiative, and the Korean Meteorological Administration, National Meteorological Satellite Center for their cooperation during the development of the COMS MI preprocessing system.



Eplee R. E. et al., “Comparison of SeaWiFS on-orbit lunar and vicarious calibrations,” Proc. SPIE, 6296 629610 (2006). http://dx.doi.org/10.1117/12.679168 PSISDG 0277-786X Google Scholar


Uprety S., Cao C., “Radiometric and spectral characterization and comparison of the Antarctic Dome C and Sonoran Desert sites for the calibration and validation of visible and near-infrared radiometers,” J. Appl. Remote Sens., 6 063541 (2012). http://dx.doi.org/10.1117/1.JRS.6.063541 1931-3195 Google Scholar


Doelling D. R. et al., “The characterization of deep convective cloud albedo as a calibration target using MODIS reflectances,” Proc. SPIE, 7862 78620I (2010). http://dx.doi.org/10.1117/12.869577 PSISDG 0277-786X Google Scholar


Cramer C. E. et al., “Precise measurement of lunar spectral irradiance at visible wavelengths,” J. Res. Natl. Inst. Stand. Technol., 118 (2013). http://dx.doi.org/10.6028/jres.118.020 JRITEF 1044-677X Google Scholar


Stone T. C. et al., “Evaluation of ISCCP multisatellite radiance calibration for geostationary imager visible channels using the Moon,” IEEE Trans. Geosci. Remote Sens., 51 (3), 1255 –1266 (2013). http://dx.doi.org/10.1109/TGRS.2012.2237520 IGRSD2 0196-2892 Google Scholar


Kieffer H. H. et al., “On-orbit radiometric calibration over time and between spacecraft using the Moon,” Proc. SPIE, 4881 287 –298 (2003). http://dx.doi.org/10.1117/12.462611 PSISDG 0277-786X Google Scholar


Wu X. et al., “Vicarious calibration of GOES Imager visible channel using the Moon,” Proc. SPIE, 6296 62960Z (2006). http://dx.doi.org/10.1117/12.681591 PSISDG 0277-786X Google Scholar


National Meteorological Satellite Center, “Introduction of COMS,” (2014) http://nmsc.kma.go.kr/html/homepage/en/chollian/choll_info.do ( October ). 2014). Google Scholar


U.S. Geological Survey, “Irradiance Model,” (2014) http://www.moon-cal.org/modeling/irradiance.php ( October ). 2014). Google Scholar


Kieffer H. H., Stone T. C., “The spectral irradiance of the Moon,” Astron. J., 129 2887 –2901 (2005). http://dx.doi.org/10.1086/430185 ANJOAA 0004-6256 Google Scholar


Seo S. B., Yong S. S., “Moon ROLO irradiance calculation with coordinate transforms for detectors’ performance analysis of geostationary visible channel imagers,” in International Symposium on Remote Sensing, P069 (2014). Google Scholar


Astronomical Applications Department of the US Naval Observatory, “Julian Date Converter,” (2014) http://aa.usno.navy.mil/data/docs/JulianDate.php ( October ). 2014). Google Scholar


Seo S. B., “Relative compensation method for the degradation of visible channel detectors using an improved histogram specification,” Electron. Lett., 50 (6), 446 –447 (2014). http://dx.doi.org/10.1049/el.2013.3900 ELLEAK 0013-5194 Google Scholar


Standish E. M., “An approximation to the errors in the planetary ephemerides of the Astronomical Almanac,” Astron. Astrophys., 417 1165 –1171 (2004). http://dx.doi.org/10.1051/0004-6361:20035663 AAEJAF 0004-6361 Google Scholar


Cho Y. M., “COMS normal operation for Earth Observation mission,” Proc. SPIE, 8533 85331S (2012). http://dx.doi.org/10.1117/12.974495 PSISDG 0277-786X Google Scholar


Seok-Bae Seo is involved in the field of algorithm and software development for the satellite ground segment. He has been working in developing and validating the image preprocessing system of COMS. He is currently working for the Geostationary Environment Monitoring Spectrometer. Since 2001, he has been working in Korea Aerospace Research Institute after his MS degree and received his PhD degree in electronics engineering from the Dong-A University of Republic of Korea in 2010.

Kyoung-Wook Jin received his BS degree from Seoul National University, Seoul, Republic of Korea, in 1994, and the MS and PhD degrees from Texas A&M University, College Station, Texas, USA, in 2001 and 2005, respectively. He has been working at the Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA, from 2005 to 2008. He is currently working on the AMI and KSEM payload development projects of the GK2 program at Korea Aerospace Research Institute, Daejeon, Republic of Korea, since 2008.

© The Authors. Published by SPIE under a Creative Commons Attribution 3.0 Unported License. Distribution or reproduction of this work in whole or in part requires full attribution of the original publication, including its DOI.
Seok-Bae Seo, Seok-Bae Seo, Kyoung-Wook Jin, Kyoung-Wook Jin, "Monitoring of COMS MI visible channel degradation based on Moon observations," Journal of Applied Remote Sensing 8(1), 083518 (14 November 2014). https://doi.org/10.1117/1.JRS.8.083518 . Submission:

Back to Top