Previous studies have indicated that the impact of ENSO on the SSTA over the entire NTA tends to be unstable. However, a study recently published in Journal of Climate by researcher at the Institute of Atmospheric Physics, Chinese Academy of Sciences, China, identifies that the decadal variation in the ENSO-NTA connection actually concentrates over the eastern part of NTA (NETA), while the connection between ENSO and the sea surface temperature anomalies over the western part of NTA is stable. The results suggest that the influence of ENSO conveys to the entire NTA before the mid-1980s, but thereafter, the influence hardly arrives the eastern part of NTA and only limits over the western part. 

 

"The decadal changes in the ENSO-NETA connection is due to the westward shift in the ENSO-related convection and teleconnections, resulting from the westward shift of Pacific Walker Circulation, induced by the intensified zonal SST-gradient over the equatorial Pacific after the mid-1980s", The author Dr. CHEN Wei said, "Our result implies a decadal variation in the ENSO-related NETA sea surface temperature anomalies, which may change the climate structures in the surrounding area."