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Title: Subsurface Nonlinear Dynamical Heating and ENSO Asymmetry

Journal Article · · Geophysical Research Letters
DOI:https://doi.org/10.1002/2017GL075771· OSTI ID:1413794

Abstract This study presents evidence of interannual to interdecadal variabilities residing in the subsurface nonlinear dynamical heating (NDH) along the equatorial Pacific thermocline based on ocean reanalysis products. In association with a flattened thermocline and drastic halt of the Equatorial Undercurrent, the NDH increases sharply right after a peak of the strong El Niño, reducing the linear anomalous advective subsurface cooling by 30%. As the result, subsurface cold signals in the west are significantly weakened as it reaches the easternmost Pacific, causing less surface cooling in the east and thus weakening the subsequent La Niña. Therefore, the subsurface NDH contributes to asymmetry in both the magnitude and structure between El Niño and La Niña. The acute positive subsurface NDH associated with strong El Niño events leads to substantial variations in its decadal means and serves as a potential source for tropical Pacific decadal to interdecadal variabilities.

Sponsoring Organization:
USDOE
Grant/Contract Number:
DESC005110
OSTI ID:
1413794
Journal Information:
Geophysical Research Letters, Journal Name: Geophysical Research Letters Vol. 44 Journal Issue: 24; ISSN 0094-8276
Publisher:
American Geophysical Union (AGU)Copyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 18 works
Citation information provided by
Web of Science

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