ENSO-Unrelated Variability in Indo–Northwest Pacific Climate Regional Coupled Ocean–Atmospheric Feedback

• Published in: Journal of climate Vol. 33; no. 10; pp. 4095 - 4108
• Main Authors: Wang, Chuan-Yang, Xie, Shang-Ping, Kosaka, Yu
• Format: Journal Article
• Language: English
• Published: Boston American Meteorological Society 15.05.2020
• Subjects: Anomalies; Atmosphere; Atmospheric circulation; Atmospheric convection; Atmospheric models; Atmospheric variability; Circulation anomalies; Computer simulation; Coupling; El Nino; El Nino phenomena; El Nino-Southern Oscillation event; Feedback; Heat flux; Heat transfer; Kelvin waves; Negative feedback; Oceans; Positive feedback; Precipitation; Pressure; Rain; Rainfall; Rainfall variability; Regional climates; Sea level; Sea level pressure; Sea surface; Sea surface temperature; Sea surface temperature anomalies; Southern Oscillation; Studies; Summer; Summer monsoon; Surface temperature; Surgical implants; Tropical atmosphere; Tropical climate; Variability; Variables; Westerlies; Winds; Pacific Ocean
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/jcli-d-19-0426.1

Regional ocean–atmospheric interactions in the summer tropical Indo–northwest Pacific region are investigated using a tropical Pacific Ocean–global atmosphere pacemaker experiment with a coupled ocean–atmospheric model (cPOGA) and a parallel atmosphere model simulation (aPOGA) forced with sea surface temperature (SST) variations from cPOGA. Whereas the ensemble mean features pronounced influences of El Niño–Southern Oscillation (ENSO), the ensemble spread represents internal variability unrelated to ENSO. By comparing the aPOGA and cPOGA, this study examines the effect of the ocean–atmosphere coupling on the ENSO-unrelated variability. In boreal summer, ocean–atmosphere coupling induces local positive feedback to enhance the variance and persistence of the sea level pressure and rainfall variability over the northwest Pacific and likewise induces local negative feedback to suppress the variance and persistence of the sea level pressure and rainfall variability over the north Indian Ocean. Anomalous surface heat fluxes induced by internal atmosphere variability cause SST to change, and SST anomalies feed back onto the atmosphere through atmospheric convection. The local feedback is sensitive to the background winds: positive under the mean easterlies and negative under the mean westerlies. In addition, north Indian Ocean SST anomalies reinforce the low-level anomalous circulation over the northwest Pacific through atmospheric Kelvin waves. This interbasin interaction, along with the local feedback, strengthens both the variance and persistence of atmospheric variability over the northwest Pacific. The response of the regional Indo–northwest Pacific mode to ENSO and influences on the Asian summer monsoon are discussed.