New SST Image

2011/10/08
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Outline of the NGSST-O products
Satellite SST observations from infrared radiometers (AVHRR, MODIS) and a microwave radiometer (AMSR-E) are objectively merged to generate the SST product, which is quality-controlled, cloud-free, high-spatial resolution (0.05 degree-grided), wide-covering (50 degree x 50 degree), and daily SST digital map. Using the satellite-derived SSTs, a first guess (mean SST weighted by the auto-correlations in an observational window) is calculated, and then the grid SSTs are produced through an optimum interpolation scheme with de-correlation scales of 200km in latitude/longitude directions and 5 days in time. In order to represent the small-scale and high-frequency SST variations, these processes have been tested and established.
The analyzed area of new SST13-63N, 116-166E covers the whole areas of the Okhotk Sea, Bohai/Yellow Sea and East China Sea as well as the western North Pacific Ocean. Since the grid size is 0.05 degree, the pixel and line numbers of SST map are both 1000. The todays SST product is generated at around 16:00 LST (7:00 UT) in the next day. Digital values of the mapped SST can be obtained through the FTP. For processing of the digital data, computing information is given in Format.
Quality control of the satellite SSTs prior to the merging process is essentially important. Abnormal values of the infrared 0.01-degree grided SSTs mostly affected by clouds are eliminated through comparison with the cloud-free AMSR-E SSTs, which are the merged SSTs formed by the 10-days AMSR-E observations. The quality control of the infrared measurements in coastal seas, where no AMSR-E observation is available, is conducted using the merged SST product of previous day and the spatially-interpolated coastal SSTs.
In order to produce the todays SST map, the satellite-derived SSTs of today and of previous four days (five days in total) are used. Since we need one day for collecting the todays SSTs, the generation of todays SST maps is delayed one day. If, for a given grid point, there is no SST observation in the 200km spatial and 5day temporal windows, the grid is treated as observational blank.
Validation of the new SST products was carried out using the in situ SSTs of buoy drifting in the analyzed area for August 2003. Match-ups of 18,845 points show that the bias of SST products is -0.31 K against the buoy observations and the root-mean square error 0.79 K.
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