Distinct Growth Rates of the Two ENSO Types

El Niño‐Southern Oscillation (ENSO) events can be grouped into two types based on their sea surface temperature anomaly spatial patterns, that is, eastern Pacific (EP) and central Pacific (CP) types. In this study, we propose a new method to empirically diagnose linear growth rates of the EP and CP...

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Vydáno v:Geophysical research letters Ročník 47; číslo 16
Hlavní autoři: Ren, Hong‐Li, Wang, Run
Médium: Journal Article
Jazyk:angličtina
Vydáno: Washington John Wiley & Sons, Inc 28.08.2020
Témata:
central Pacific (CP) ENSO
eastern Pacific (EP) ENSO
El Nino
El Nino phenomena
El Nino-Southern Oscillation event
empirical method
ENSO growth rate
Growth rate
Heat budget
Intercomparison
Oceanic heat budget
Sea surface
Sea surface temperature
Sea surface temperature anomalies
Southern Oscillation
Stability
Surface temperature
Temperature anomalies
ISSN:0094-8276, 1944-8007
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Shrnutí:El Niño‐Southern Oscillation (ENSO) events can be grouped into two types based on their sea surface temperature anomaly spatial patterns, that is, eastern Pacific (EP) and central Pacific (CP) types. In this study, we propose a new method to empirically diagnose linear growth rates of the EP and CP ENSO types due to a limitation of applying the traditional Bjerknes stability index method simply to these two types. We spatially project the peak‐time symmetric component of the mixed‐layer oceanic heat budget terms onto the ENSO‐related sea surface temperature anomaly patterns to estimate the ENSO grow rate. After validating the method by comparing it with the Bjerknes stability index, we show that the growth rate is positive for the CP ENSO type and weakly negative for the EP ENSO type, contributed by different feedback terms. The Coupled Model Intercomparison Project Phase 5‐based multimodel ensemble mean shows similar characteristics as the reanalysis for the EP ENSO type rather than the CP ENSO type. Key Points A new method of empirically diagnosing the ENSO linear growth rate (GR) is proposed and validated by comparing it with the dynamical BJ index The eastern Pacific ENSO has a weakly negative GR while the central Pacific one has a positive, where the thermocline feedback plays key roles The GR of the eastern Pacific rather than central Pacific ENSO can be reasonably reproduced by the CMIP5 models with their ensemble mean
Bibliografie:ObjectType-Article-1
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ISSN:0094-8276
1944-8007
DOI:10.1029/2020GL088179