A Review of Paleo El Niño-Southern Oscillation

• Published in: Atmosphere
• Main Authors: Zhengyao Lu, Zhengyu Liu, Jiang Zhu, Kim M. Cobb
• Format: Article in Journal/Newspaper
• Language: English
• Published: MDPI AG 2018
• Subjects: ENSO; paleoclimate; proxy data; climate model; Meteorology. Climatology; QC851-999; Ice Sheet
• Online Access: https://doi.org/10.3390/atmos9040130; https://doaj.org/article/c8e3da8dc2424afaab89a20548a98dde

The Earth has seen El Niño-Southern Oscillation (ENSO)—the leading mode of interannual climate variability—for at least millennia and likely over millions of years. This paper reviews previous studies from perspectives of both paleoclimate proxy data (from traditional sediment records to the latest high-resolution oxygen isotope records) and model simulations (including earlier intermediate models to the latest isotope-enabled coupled models). It summarizes current understanding of ENSO’s past evolution during both interglacial and glacial periods and its response to external climatic forcings such as volcanic, orbital, ice-sheet and greenhouse gas forcings. Due to the intrinsic irregularity of ENSO and its complicated relationship with other climate phenomena, reconstructions and model simulations of ENSO variability are subject to inherent difficulties in interpretations and biases. Resolving these challenges through new data syntheses, new statistical methods, more complex climate model simulations as well as direct model-data comparisons can potentially better constrain uncertainty regarding ENSO’s response to future global warming.