Sea Surface Temperature derived from FY-2 Geostationary Meteorological Satellite
SST processing system
The SST processing procedure include five
components: SST retrieval everyday 8-time,
calculating daily mean, five-day mean, ten-day
mean monthly mean SST, products
verification, and output of products.
Processing procedure is shown Fig.1.
Fig.1 FY-2 SST Processing Procedure
SST retrieval everyday 8-time
SST is retrieved at each 0.5° latitude /
longitude grid point within the area from 50° S
to 50° N and from 55° E to 155° E every 3 hours.
This component includes, 1) image coordinate
transform, 2) Calculating satellite zenith and
solar zenith angle, 3) Converting digital count
values of IR to brightness temperatures with
calibration table, 4) Performing Cloud
detection and Atmospheric Attenuation
correction.
Calculating daily mean SST
The step is SST comparison test everyday 8
times, 8-time SST Merged and calculating
daily mean SST
Calculating five-day mean, ten-day mean and monthly mean SST
Five-day mean SST are calculated from daily
mean SST, ten-day mean SST are calculated
from five-day mean values, and monthly mean
SST are calculated from ten-day mean values.
Products verification
Product verification is to determine the
accuracy of satellite-derived SST products.
The SST retrievals from the above processing
are compared with the conventional SST
measurements from GTS. Calculating root
mean square (RMS) and bias.
Output of products
Archival tape, print, image display, contour
chart, and Distributing
Calculation result
Daily mean, five-day mean, ten-day mean SST
products were obtained, covering the area
from 50° N to 50° S and 55° E to 155° E.
Fig.2 shows Ten-day SST pseudo color image
in April, 1999.

Fig.2 Ten mean SST pseudo color image of FY-2 in April, 1999
Discussion
FY-2 SST processing system can obtain more
frequently SST, so that probability of
obtaining cloud-free data is enhance. But the
radiometer aboard FY-2 satellite has only one
IR channel, the accuracy of Atmospheric
Attenuation correction is not higher. The same
results show RMS is about 0.9° C-2.2°C, we
will improve algorithm.
References
- McClain, E. P., Pichel, W. G., and Walton,
C. C., 1985, Comparative performance of
AVHRRbased multi-channel sea surface
temperature, Journal of Geophysical Research,
Vol. 90, No. C6, 1158711602.
- Qiu Kangmu, 1987, statistical estimation
method for retrieval sea surface temperature,
Atmospheric Radiation progress and prospects,
p.699.
- Chen Weiying, 1998, Sea Surface
Temperature Retrieval From Geostetionary
Meteorological Satellite (GMS-5) Infrared
Split-Window Channels, Proceedings of SPIE
Optical Remote Sensing of the Atmosphere
and Clouds. , Vol.3501.p484.