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The Impacts of a Weakened Atlantic Meridional Overturning Circulation on ENSO in a Warmer Climate

Journal Article · · Geophysical Research Letters
DOI:https://doi.org/10.1029/2023gl103025· OSTI ID:2422201
 [1];  [2];  [3];  [4]
  1. Univ. of California, Riverside, CA (United States); OSTI
  2. Univ. of California, Riverside, CA (United States)
  3. Yale Univ., New Haven, CT (United States); Sorbonne Univ., Paris (France)
  4. National Center for Atmospheric Research (NCAR), Boulder, CO (United States)

This study quantifies the impacts of the Atlantic Meridional Overturning Circulation (AMOC) on the El Niño–Southern Oscillation (ENSO) under anthropogenic warming by comparing climate change model simulations with declining and fixed strengths of the overturning. After the 1980s, a weakened AMOC is shown to reduce the strength of the annual cycle of sea surface temperature (SST) in the eastern equatorial Pacific and induce anomalous cross-equatorial northerly winds there, which strengthens ENSO variability by about 11%. An analysis of the Bjerknes stability index reveals that this intensification of ENSO results mainly from enhanced Ekman upwelling feedback due to amplified atmospheric wind response to SST anomalies and oceanic upwelling response to equatorial wind stress anomalies. The weakened AMOC also promotes the occurrence of Central Pacific El Niño events and reduces ENSO skewness. These AMOC impacts on ENSO magnitude and complexity throughout the twenty-first century are however smaller than ENSO variations expected from internal climate variability.

Research Organization:
Yale Univ., New Haven, CT (United States)
Sponsoring Organization:
USDOE Office of Science (SC)
Grant/Contract Number:
SC0023134
OSTI ID:
2422201
Journal Information:
Geophysical Research Letters, Journal Name: Geophysical Research Letters Journal Issue: 8 Vol. 50; ISSN 0094-8276
Publisher:
American Geophysical Union (AGU)Copyright Statement
Country of Publication:
United States
Language:
English

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