Skip all navigation and jump to content Jump to site navigation
About MODIS News Data Tools /images2 Science Team Science Team Science Team

   + Home
MODIS Publications Link
MODIS Presentations Link
MODIS Biographies Link
MODIS Science Team Meetings Link



Li, AH; Bo, YC; Zhu, YX; Guo, P; Bi, J; He, YQ (2013). Blending multi-resolution satellite sea surface temperature (SST) products using Bayesian maximum entropy method. REMOTE SENSING OF ENVIRONMENT, 135, 52-63.

Integrating multiple satellite sea surface temperature (SST) products is one of the ways to improve the accuracy, spatial resolution and completeness of satellite SST products. In this paper, The Bayesian Maximum Entropy (BME), a nonlinear geostatistical methodology, is used for blending the satellite SST datasets (SSTs) derived from the Moderate Resolution Imaging Spectroradiometer (MODIS) and the Advanced Microwave Scanning Radiometer for Earth Observing System (AMSR-E) on EOS Aqua satellite. An error model is developed to link the MODIS SST and the AMSR-E SST at different resolutions. The AMSR-E SSTs are processed as probability soft data by this error model to take into account the uncertainty associated with coarser resolution pixels. The MODIS SSTs are taken as hard data. The soft AMSR-E SSTs and hard MODIS SSTs are then merged in the BME paradigm to produce 8-day average and spatially continuous SSTs with 4 km spatial resolution. The Merged SSTs are validated by using the drifting buoy SST records. The local variance is used to evaluate the ability of the BME method in preserving the original fine spatial structure of the 4 km resolution MODIS SSTs in the blended SSTs. The validation results show that the RMSE and Bias for the BME blended SSTs over the whole study area in 2003 are 0.653 degrees C and -0.146 degrees C, respectively. These values are a bit larger than those for AMSR-E SST (the RMSE and Bias are 0.504 degrees C and 0.0392 degrees C, respectively) and MODIS SST (the RMSE and Bias are 0.635 degrees C and -0.102 degrees C, respectively). The estimations of SST pixels where both of MODE and AMSR-E have missing data have a Bias of -0.255 degrees C and an RMSE of 0.826 degrees C. The difference in local variance between the Merged SSTs and MODIS SSTs is less than 0.01 degrees C-2, and the difference between the Merged SSTs and AMSR-E SSTs is about 0.19 degrees C-2. The blended 4-km SST data set is equal to MODIS SST in revealing the fine scale structures of SST spatial variation. In addition, the blended SST dataset has the complete spatial coverage. The results demonstrate the blending potential of BME for multiple scales satellite derived products integration. (C) 2013 Elsevier Inc. All rights reserved.



NASA Home Page Goddard Space Flight Center Home Page