Zhengyao Lu
Forskare
Seasonal Cycle of Background in the Tropical Pacific as a Cause of ENSO Spring Persistence Barrier
Författare
Summary, in English
Statistical model results suggest that the declining growth rate from autumn to spring is the key to cause El Niño-Southern Oscillation (ENSO) spring persistence barrier (SPB). Using a dynamical approach, we develop the physical mechanisms responsible for ENSO SPB in the framework of recharge oscillator by adding a seasonally varying Bjerknes (BJ) stability index and linking it with ENSO growth rate. By decomposing BJ index, it is indicated that seasonal thermodynamic damping and thermocline positive feedback play an important role in determining the ENSO SPB. We further show that the increasing/decreasing upper-level cloud/low-level cloud and the deepening thermocline from autumn to spring are the main factors to control the SPB of ENSO. Our proposed mechanisms also have useful implications for the understanding of ENSO prediction.
Avdelning/ar
- Institutionen för naturgeografi och ekosystemvetenskap
- MERGE: ModElling the Regional and Global Earth system
Publiceringsår
2019-11-12
Språk
Engelska
Sidor
13371-13378
Publikation/Tidskrift/Serie
Geophysical Research Letters
Volym
46
Issue
22
Dokumenttyp
Artikel i tidskrift
Förlag
American Geophysical Union (AGU)
Ämne
- Meteorology and Atmospheric Sciences
Nyckelord
- Bjerknes stability index
- cloud
- El Niño-Southern Oscillation
- seasonal persistence barrier
- thermocline
Status
Published
ISBN/ISSN/Övrigt
- ISSN: 0094-8276