Related Experiment Video
Updated: Dec 25, 2025

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
Published on: August 7, 2017
No consistent ENSO response to volcanic forcing over the last millennium
Sylvia G Dee1, Kim M Cobb2, Julien Emile-Geay3
1Rice University, Department of Earth, Environmental, and Planetary Sciences, Houston, TX 77005, USA. sylvia.dee@rice.edu.
This study found that large volcanic eruptions have a weak, insignificant impact on the El Niño-Southern Oscillation (ENSO). Climate models may overestimate ENSO's sensitivity to volcanic forcing.
Area of Science:
- Paleoclimatology
- Climate Science
- Ocean-Atmosphere Dynamics
Background:
- The El Niño-Southern Oscillation (ENSO) significantly influences global climate patterns.
- ENSO's sensitivity to external climate forcing, like volcanic eruptions, is not well understood.
- Previous modeling studies suggest a link between volcanic sulfate aerosols and ENSO, but observational evidence is inconclusive.
Purpose of the Study:
- To investigate the impact of major volcanic eruptions on ENSO during the last millennium.
- To provide observational data to validate climate model predictions of ENSO's response to volcanic forcing.
Main Methods:
- Utilized absolutely dated fossil corals from the central tropical Pacific as paleoclimate archives.
- Applied superposed epoch analysis to assess ENSO's state in the year following large volcanic eruptions.
Main Results:
- A slight tendency towards an El Niño-like ENSO response was observed in the year after volcanic eruptions.
- This observed tendency was not statistically significant.
- No significant ENSO response was detected even after the exceptionally large 1257 Samalas eruption.
Conclusions:
- The study's findings suggest that the ENSO response to volcanic forcing might be weaker than predicted by some climate models.
- Observed ENSO variability may mask or be larger than the forced response to volcanic eruptions.
- Further research is needed to refine climate models and better understand the interplay between volcanism and ENSO.
Related Concept Videos
Global Climate Change
Isothermal Processes
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
Transient and Steady-state Response
These test signals are integral in designing control systems to exhibit two key performance aspects: transient response and steady-state...
Magnetostatic Boundary Conditions
General External Flow Characteristics
Forced Oscillations

