Antenna System
NOAA
- - Data Period : Nov 1989 - present
- - Receiving NOAA satellite data
MTSAT
- - Data Period : Sep 2012 - Dec 2015(discussing later utilization of MTSAT-2)
- - Receiving MTSAT satellite data
COMS
- - Data Period : Sep 2012 - present
- - Receiving COMS satellite data
Satellite Data Processing System
TeraScan
- - Data Period : Nov 1989 - present
- - Program for satellite data processing
- - Product of SeaSpace (http://www.seaspace.com/software.php)
Image Processing System
GOCI Data Processing System (GDPS)
Surface Temperature Sensor
Surface Temperature Sensor
- - Located at ESOROB
- - Operated by Seoul National University (http://www.curl.snu.ac.kr/home/cesrob)
- - Real-time observation
- - Since April 1999
- - Smpling interval : 10 minutes
- - Setting depth : 10, 20, 40 cm (SBE56), 82 cm (SBE39)
Spectroradiometer
Spectroradiometer
Spectral range : 350-2500 nm
- - Spectral resolution : 3 nm @700 nm
30 nm @ 1400/2100 nm
- - Scanning time : 100 milliseconds
- - Wavelength accuracy : 0.5 nm
Hyperspectral camera
Senop-2 hyperspectral camera
Frame-based snapshot system
Spectral range: 500-900 nm
Up to 1,000 freely selectable spectral bands
Up to 149 frames per seconds
Easy to integrate and attach
Senop HSC-2 Hyperspectral camera is a frame-based spectral system that provides snapshot images in the VNIR spectral range (500-900nm)
with up to one thousand narrow bands.
This unique snapshot camera provides exclusively true image pixels with 1-megapixel resolution without using interpolation.
The frame-based approach with integrated positioning and IMU allows easy image stitching for mosaics with high resolution images.
Infrared Sea surface temperature Autonomous Radiometer (ISAR)
Measurement of sea surface temperature (skin SST)
Infrared emission from the sea surface and atmosphere are measured
Accuracy: ± 0.1 K
Waveband: 9.8 - 11 µm
Measurement range: 173 - 373 K (-100~100℃)
Satellite SST validation
Figure. A schematic diagram of radiation rays penetrated into the ISAR installed on a ship, where h is a height of the ISAR from the sea surface,
Lsky is the sky incident radiation, Ldown is the downwelling radiance incident on the sea surface, Lup is the upwelling radiance from the sea
surface, and Lsea is the radiance originating from the sea surface, θ is an angle between the nadir of the ISAR and the ray of Lsea into the ISAR.
Others
Analytical Balance
Generator of Coriolis Force
Generator of Seismic Sea Wave