Super El Niños in response to global warming in a climate model

Extraordinarily strong El Niño events, such as those of 1982/1983 and 1997/1998, cause havoc with weather around the world, adversely influence terrestrial and marine ecosystems in a number of regions and have major socio-economic impacts. Here we show by means of climate model integrations that El...

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Veröffentlicht in:Climatic change 2015-10, Vol.132 (4), p.489-500
Hauptverfasser: Latif, Mojib, Semenov, Vladimir A., Park, Wonsun
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container_issue 4
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container_title Climatic change
container_volume 132
creator Latif, Mojib
Semenov, Vladimir A.
Park, Wonsun
description Extraordinarily strong El Niño events, such as those of 1982/1983 and 1997/1998, cause havoc with weather around the world, adversely influence terrestrial and marine ecosystems in a number of regions and have major socio-economic impacts. Here we show by means of climate model integrations that El Niño events may be boosted by global warming. An important factor causing El Niño intensification is warming of the western Pacific warm pool, which strongly enhances surface zonal wind sensitivity to eastern equatorial Pacific sea surface temperature anomalies. This in conjunction with larger and more zonally asymmetric equatorial Pacific upper ocean heat content supports stronger and longer lasting El Niños. The most intense events, termed Super El Niños, drive extraordinary global teleconnections which are associated with exceptional surface air temperature and rainfall anomalies over many land areas.
doi_str_mv 10.1007/s10584-015-1439-6
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subjects 21st century
Air temperature
Amplification
Anomalies
Atmospheric models
Atmospheric Sciences
Climate change
Climate Change/Climate Change Impacts
Climate models
Earth and Environmental Science
Earth Sciences
Economic impact
El Nino
Equatorial regions
Global warming
Hypotheses
Land
Marine
Marine ecosystems
Ocean currents
Ocean-atmosphere interaction
Rainfall
Sea surface temperature
Standard deviation
Upper ocean
Wind
title Super El Niños in response to global warming in a climate model
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