Abstract
AbstractThis study investigates the effect of parameterized westerly wind bursts (WWBs) on the diversity of El Niño–Southern Oscillation (ENSO) warm events, namely, eastern Pacific (EP) and central Pacific (CP) ENSO in Community Climate System Model version 3 (CCSM3) and version 4 (CCSM4). The parameterization includes the possibility of state‐independent (SI) and state‐dependent (SD) WWBs. The inclusion of WWBs enhances the overall tropical Pacific variability. This is accompanied by an increased in the so‐called thermocline and advective feedback mechanisms. The SI WWB results present some model discrepancies, with CCSM3 (CCSM4) having enhanced CP (EP) ENSO variability. For the SD WWB case, both models show enhanced EP variability relative to CP variability.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
