4.8 Article

Stabilised frequency of extreme positive Indian Ocean Dipole under 1.5°C warming

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NATURE COMMUNICATIONS
卷 9, 期 -, 页码 -

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NATURE PUBLISHING GROUP
DOI: 10.1038/s41467-018-03789-6

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  1. Centre for Southern Hemisphere Oceans Research
  2. Earth Science and Climate Change Hub of the Australian Government's National Environmental Science Programme
  3. CSIRO Office of Chief Executive Science Leader award
  4. Australian Research Council

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Extreme positive Indian Ocean Dipole (pIOD) affects weather, agriculture, ecosystems, and public health worldwide, particularly when exacerbated by an extreme El Nino. The Paris Agreement aims to limit warming below 2 degrees C and ideally below 1.5 degrees C in global mean temperature (GMT), but how extreme pIOD will respond to this target is unclear. Here we show that the frequency increases linearly as the warming proceeds, and doubles at 1.5 degrees C warming from the pre-industrial level (statistically significant above the 90% confidence level), underscored by a strong intermodel agreement with 11 out of 13 models producing an increase. However, in sharp contrast to a continuous increase in extreme El Nino frequency long after GMT stabilisation, the extreme pIOD frequency peaks as the GMT stabilises. The contrasting response corresponds to a 50% reduction in frequency of an extreme El Nino preceded by an extreme pIOD from that projected under a business-as-usual scenario.

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