2008/10/23 by S. Iwasaki, Shinsuke Iwasaki, Masahisa Kubota +3
Environmental Science · Earth and Planetary Sciences · #Climate variability and models #Oceanographic and Atmospheric Processes #Arctic and Antarctic ice dynamics
paper · doi:10.1080/01431160802175363
Abstract To clarify the characteristics of global sea surface temperature (SST) products, we have compared the Reynolds product with four other products: the Center for Atmospheric and Oceanic Studies (CAOS) SST, the microwave optimum interpolation (MWOI) SST, the merged satellite and in‐situ data global daily (MGD) SST and the real time global (RTG) SST. Furthermore, we have validated these five products with SST data observed by moored buoys. The CAOS SST and the MWOI SST show significant underestimation in several regions. The underestimation is related to the characteristics of the original microwave data. It should be noted that the MGD SST provides the best statistics, although the high‐frequency variations are removed by a low‐pass filter. Moreover, we have investigated the impact of the differences between the SST products on estimated latent heat flux. In regions with strong SST gradients, the average differences are significantly large. Acknowledgements The authors would like to thank Dr Tsurane Kuragano and Dr Yoshimi Kawai (JAMSTEC) for their helpful comments and for providing the CAOS SST data from CAOS and the MGD SST data from JMA, respectively. This research was funded by JAXA and Category 7 of the MEXT RR2002 Project for Sustainable Coexistence of Human, Nature and the Earth.