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Highly variable El Niño-Southern Oscillation throughout the Holocene
Kim M Cobb1, Niko Westphal, Hussein R Sayani
1School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332, USA. kcobb@eas.gatech.edu
Summary
The El Niño-Southern Oscillation (ENSO) shows high variability over 7000 years. Current climate models may struggle to detect forced ENSO changes due to natural climate variability.
Area of Science:
- Paleoclimatology
- Climate dynamics
- Oceanography
Background:
- The El Niño-Southern Oscillation (ENSO) significantly impacts global climate patterns annually.
- The ENSO's sensitivity to anthropogenic greenhouse gas emissions remains uncertain.
- Understanding ENSO's response to forcings is crucial for climate change projections.
Purpose of the Study:
- To analyze long-term ENSO variability using fossil coral records.
- To assess ENSO's response to past natural forcings and compare it with model predictions.
- To investigate the potential detectability of anthropogenic impacts on ENSO.
Main Methods:
- Utilized fossil coral reconstructions of ENSO activity spanning the last 7000 years.
- Focused analysis on data from the Northern Line Islands, a key ENSO region.
- Compared paleoclimatic ENSO variance with instrumental records and climate model outputs.
Main Results:
- Fossil corals reveal highly variable ENSO activity over the past 7000 years.
- No systematic trend in ENSO variance was found, contradicting some insolation-driven models.
- Twentieth-century ENSO variance, while high, is not unprecedented in the paleoclimatic record.
Conclusions:
- Long-term ENSO variability is substantial, potentially masking forced climate change signals.
- Detecting anthropogenic influences on ENSO may be challenging against a backdrop of high internal variability.
- Past ENSO behavior suggests resilience and complex responses to external forcings.
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