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Tropical Indo-Pacific Monitoring

 

Data Source:

The monthly mean OI-SST (NOAA Optimum Interpolation (OI) Sea Surface Temperature) (http://www.cdc.noaa.gov/cdc/data.noaa.oisst.v2.html) anomalies are used to monitor the current condition of ENSO and IOD. It covers from December 1981 to the latest. Base period for climatology is 1982~2007.

References:

Ashok, K., S. K. Behera, S. A. Rao, H. Weng and T. Yamagata, 2007. El Nino Modoki and its possible teleconnection. J. Geophys. Res., 112, C11007, doi:10.1029/2006JC003798.

Saji, N. H., B. N. Goswami, P. N. Vinayachandran and T. Yamagata, 1999. A Dipole Mode in the tropical Indian Ocean. Nature, 401 (23): 360363.

Saji, N. H., and Yamagata, T., 2003. Possible impacts of Indian Ocean dipole mode events on global climate. Climate Research, 25, 151-169.

 

Data Source:

The monthly mean OI-SST (NOAA Optimum Interpolation (OI) Sea Surface Temperature) (http://www.cdc.noaa.gov/cdc/data.noaa.oisst.v2.html) anomalies are used to monitor the current condition of ENSO and IOD. It covers from December 1981 to the latest. Base period for climatology is 1982~2007.

References:

Ashok, K., S. K. Behera, S. A. Rao, H. Weng and T. Yamagata, 2007. El Nino Modoki and its possible teleconnection. J. Geophys. Res., 112, C11007, doi:10.1029/2006JC003798.

Saji, N. H., B. N. Goswami, P. N. Vinayachandran and T. Yamagata, 1999. A Dipole Mode in the tropical Indian Ocean. Nature, 401 (23): 360363.

Saji, N. H., and Yamagata, T., 2003. Possible impacts of Indian Ocean dipole mode events on global climate. Climate Research, 25, 151-169.

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