skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Understanding the El Niño-like Oceanic Response in the Tropical Pacific to Global Warming

Journal Article · · Climate Dynamics

The enhanced central and eastern Pacific SST warming and the associated ocean processes under global warming are investigated using the ocean component of the Community Earth System Model (CESM), Parallel Ocean Program version 2 (POP2). The tropical SST warming pattern in the coupled CESM can be faithfully reproduced by the POP2 forced with surface fluxes computed using the aerodynamic bulk formula. By prescribing the wind stress and/or wind speed through the bulk formula, the effects of wind stress change and/or the wind-evaporation-SST (WES) feedback are isolated and their linearity is evaluated in this ocean-alone setting. Result shows that, although the weakening of the equatorial easterlies contributes positively to the El Niño-like SST warming, 80% of which can be simulated by the POP2 without considering the effects of wind change in both mechanical and thermodynamic fluxes. This result points to the importance of the air-sea thermal interaction and the relative feebleness of the ocean dynamical process in the El Niño-like equatorial Pacific SST response to global warming. On the other hand, the wind stress change is found to play a dominant role in the oceanic response in the tropical Pacific, accounting for most of the changes in the equatorial ocean current system and thermal structures, including the weakening of the surface westward currents, the enhancement of the near-surface stratification and the shoaling of the equatorial thermocline. Interestingly, greenhouse gas warming in the absence of wind stress change and WES feedback also contributes substantially to the changes at the subsurface equatorial Pacific. Further, this warming impact can be largely replicated by an idealized ocean experiment forced by a uniform surface heat flux, whereby, arguably, a purest form of oceanic dynamical thermostat is revealed.

Research Organization:
Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
Sponsoring Organization:
USDOE
DOE Contract Number:
AC05-76RL01830
OSTI ID:
1225146
Report Number(s):
PNNL-SA-104684; KP1703010
Journal Information:
Climate Dynamics, Vol. 45, Issue 7; ISSN 0930-7575
Publisher:
Springer-Verlag
Country of Publication:
United States
Language:
English

Similar Records

Response of the tropical Pacific Ocean to El Niño versus global warming
Journal Article · Fri Apr 15 00:00:00 EDT 2016 · Climate Dynamics · OSTI ID:1225146

The Role of Ocean Dynamical Thermostat in Delaying the El Niño–Like Response over the Equatorial Pacific to Climate Warming
Journal Article · Mon Mar 27 00:00:00 EDT 2017 · Journal of Climate · OSTI ID:1225146

Warm Phase of AMV Damps ENSO Through Weakened Thermocline Feedback
Journal Article · Tue Dec 07 00:00:00 EST 2021 · Geophysical Research Letters · OSTI ID:1225146