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Stronger Increase in the Frequency of Extreme Convective than Extreme Warm El Niño Events under Greenhouse Warming
Abstract
Since 1979, three extreme El Niño events occurred, in 1982/83, 1997/98, and 2015/16, with pronounced impacts that disrupted global weather patterns, agriculture, fisheries, and ecosystems. Although all three episodes are referred to as strong equatorial eastern Pacific (EP) El Niño events, the 2015/16 event is considered a mixed regime of both EP and central Pacific (CP) El Niño. During such extreme events, sea surface temperature (SST) anomalies peak over the EP region, hereafter referred to as an extreme warm El Niño (ExtWarmEN) event. Simultaneously, the intertropical convergence zone (ITCZ) moves southward to the usually dry and cold Niño-3 region, resulting in dramatic rainfall increases to more than 5 mm day−1 averaged over boreal winter, referred to as an extreme convective El Niño (ExtConEN) event. However, in climate models from phase 5 of the Coupled Model Intercomparison Project (CMIP5) that are able to simulate both types of events, ExtConEN events are found not to always coincide with ExtWarmEN events and the disassociation becomes more distinct under greenhouse warming when the increased frequency of ExtConEN events is notably larger than that of ExtWarmEN events. The disassociation highlights the role of eastward migration of western Pacific convection and equatorward shift of the South Pacific convergence zone associated with the faster warming over the EP region as a result of greenhouse warming.
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Ongoing anthropogenic climate change impacts the thermocline that influences ENSO, making extreme rainfall events more likely and exacerbating drought conditions in an already arid Manabí.
“Our ongoing anthropogenic climate change impacts the delicate thermocline that influences ENSO (Cai et al. 2014(Cai et al. , 2015(Cai et al. , 2018;;Wang, Cai, and Santoso 2020), making extreme rainfall events more likely and exacerbating drought conditions in an already arid Manabí (Campos Cedeño and Mendoza Álava 2018).”
From In between the sites: understanding late holocene manteño agricultural contexts in the chongón-colonche mountains of coastal ecuador through UAV-lidar and excavation (2025) · cites this paper as Wang, Cai, and Santoso 2020
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Increasing frequency of extreme El Niño events due to greenhouse warming.
Cai, W., Borlace, S., Lengaigne, M., van Rensch, P., Collins, M., Vecchi, G., Timmermann, A., Santoso, A., McPhaden, M. J., Wu, L., et al. (2014) · Nature Climate Change · doi:10.1038/nclimate2100 · Cited by 2,198
Self-citationCai, W., Santoso, A., Wang, G., Yeh, S.-W., An, S.-I., Cobb, K. M., Collins, M., Guilyardi, E., Jin, F.-F., Kug, J.-S., et al. (2015) · Nature Climate Change · doi:10.1038/nclimate2743 · Cited by 891
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Garzón-Oechsle, A., Johanson, E., Nagarajan, S., & Martínez, V. (2025) · Journal of Field Archaeology · doi:10.1080/00934690.2024.2439223 · Cited by 3
Metadata
- Authors
- Wang, G., Cai, W., & Santoso, A.
- Affiliations
- Key Laboratory of Physical Oceanography, Institute for Advanced Ocean Studies, Ocean University of China, and Qingdao National Laboratory for Marine Science and Technology, Qingdao, China, and Centre for Southern Hemisphere Oceans Research, CSIRO Oceans and Atmosphere, Hobart, Tasmania, Australia
- Centre for Southern Hemisphere Oceans Research, CSIRO Oceans and Atmosphere, Hobart, Tasmania, and Australian Research Council Centre of Excellence for Climate Extremes, University of New South Wales, Sydney, New South Wales, Australia
- Venue
- Journal of Climate
- Publisher
- American Meteorological Society
- Published
- 2020-01-15
- Volume
- 33
- Issue
- 2
- Pages
- 675-690
- ISSN
- 0894-8755
- 1520-0442
- Cited by
- 22
- References
- 2
- Funders
- Centre for Southern Hemisphere Oceans Research, a joint research centre between QNLM and CSIRO
- Earth Systems and Climate Change Hub of the Australian Government’s National Environmental Science Program
- a CSIRO Office of Chief Executive Science Leader award
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