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Two-year consecutive concurrences of positive Indian Ocean Dipole and Central Pacific El Niño preconditioned the 2019/2020 Australian “black summer” bushfires

Geoscience letters, 2020-11, Vol.7 (1), p.1-9, Article 19

2020

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Historical change of El Niño properties sheds light on future changes of extreme El Niño

Proceedings of the National Academy of Sciences - PNAS, 2019-11, Vol.116 (45), p.22512-22517

2019

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The Defining Characteristics of ENSO Extremes and the Strong 2015/2016 El Niño

Reviews of geophysics (1985), 2017-12, Vol.55 (4), p.1079-1129

2017

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Why is the amplitude of the Indian Ocean Dipole overly large in CMIP3 and CMIP5 climate models?

Geophysical research letters, 2013-03, Vol.40 (6), p.1200-1205

2013

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Realism of the Indian Ocean Dipole in CMIP5 Models: The Implications for Climate Projections

Journal of climate, 2013-09, Vol.26 (17), p.6649-6659

2013

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Rising temperature depletes soil moisture and exacerbates severe drought conditions across southeast Australia

Geophysical research letters, 2009-11, Vol.36 (21), p.np-n/a

2009

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Indian Ocean Dipole in CMIP5 and CMIP6: characteristics, biases, and links to ENSO

Scientific reports, 2020-07, Vol.10 (1), Article 11500

2020

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A Unique Feature of the 2019 Extreme Positive Indian Ocean Dipole Event

Geophysical research letters, 2020-09, Vol.47 (18), p.n/a

2020

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Increased variability of the western Pacific subtropical high under greenhouse warming

Proceedings of the National Academy of Sciences - PNAS, 2022-06, Vol.119 (23), p.e2120335119-e2120335119

2022

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Increased variability of eastern Pacific El Niño under greenhouse warming

Nature (London), 2018-12, Vol.564 (7735), p.201-206

2018

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Southeast Australia Autumn Rainfall Reduction: A Climate-Change-Induced Poleward Shift of Ocean–Atmosphere Circulation

Journal of climate, 2013-01, Vol.26 (1), p.189-205

2013

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Evidence of impacts from rising temperature on inflows to the Murray-Darling Basin

Geophysical research letters, 2008-04, Vol.35 (7), p.L07701-n/a

2008

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Asymmetry in the IOD and ENSO Teleconnection in a CMIP5 Model Ensemble and Its Relevance to Regional Rainfall

Journal of climate, 2013-07, Vol.26 (14), p.5139-5149

2013

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Variability of the Indian Ocean Dipole post-2100 reverses to a reduction despite persistent global warming

Nature communications, 2024-06, Vol.15 (1), p.5023-6

2024

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Thermocline Warming Induced Extreme Indian Ocean Dipole in 2019

Geophysical research letters, 2020-09, Vol.47 (18), p.n/a

2020

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Decreased ENSO post-2100 in response to formation of a permanent El Niño-like state under greenhouse warming

Nature communications, 2024-07, Vol.15 (1), p.5810-10, Article 5810

2024

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A New Type of the Indian Ocean Dipole since the Mid-1970s

Journal of climate, 2013-02, Vol.26 (3), p.959-972

2013

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Teleconnection Pathways of ENSO and the IOD and the Mechanisms for Impacts on Australian Rainfall

Journal of climate, 2011-08, Vol.24 (15), p.3910-3923

2011

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Increased frequency of extreme Indian Ocean Dipole events due to greenhouse warming

Nature (London), 2014-06, Vol.510 (7504), p.254-258

2014

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Interactions of ENSO, the IOD, and the SAM in CMIP3 Models

Journal of climate, 2011-03, Vol.24 (6), p.1688-1704

2011

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Nonlinear El Niño impacts on the global economy under climate change

Nature communications, 2023-09, Vol.14 (1), p.5887-5887, Article 5887

2023

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Severe heat waves in Southern Australia: synoptic climatology and large scale connections

Climate dynamics, 2012, Vol.38 (1-2), p.209-224

2012

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Butterfly effect and a self-modulating El Niño response to global warming

Nature (London), 2020-09, Vol.585 (7823), p.68-73

2020

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Climate-change impact on the 20th-century relationship between the Southern Annular Mode and global mean temperature

Scientific reports, 2013-06, Vol.3 (1), p.2039, Article 2039

2013

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Did Climate Change–Induced Rainfall Trends Contribute to the Australian Millennium Drought?

Journal of climate, 2014-05, Vol.27 (9), p.3145-3168

2014

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Two-year consecutive concurrences of positive Indian Ocean Dipole and Central Pacific El Niño preconditioned the 2019/2020 Australian “black summer” bushfires

Historical change of El Niño properties sheds light on future changes of extreme El Niño

The Defining Characteristics of ENSO Extremes and the Strong 2015/2016 El Niño

Why is the amplitude of the Indian Ocean Dipole overly large in CMIP3 and CMIP5 climate models?

Realism of the Indian Ocean Dipole in CMIP5 Models: The Implications for Climate Projections

Rising temperature depletes soil moisture and exacerbates severe drought conditions across southeast Australia

Indian Ocean Dipole in CMIP5 and CMIP6: characteristics, biases, and links to ENSO

A Unique Feature of the 2019 Extreme Positive Indian Ocean Dipole Event

Increased variability of the western Pacific subtropical high under greenhouse warming

Increased variability of eastern Pacific El Niño under greenhouse warming

Southeast Australia Autumn Rainfall Reduction: A Climate-Change-Induced Poleward Shift of Ocean–Atmosphere Circulation

Evidence of impacts from rising temperature on inflows to the Murray-Darling Basin

Asymmetry in the IOD and ENSO Teleconnection in a CMIP5 Model Ensemble and Its Relevance to Regional Rainfall

Variability of the Indian Ocean Dipole post-2100 reverses to a reduction despite persistent global warming

Thermocline Warming Induced Extreme Indian Ocean Dipole in 2019

Decreased ENSO post-2100 in response to formation of a permanent El Niño-like state under greenhouse warming

A New Type of the Indian Ocean Dipole since the Mid-1970s

Teleconnection Pathways of ENSO and the IOD and the Mechanisms for Impacts on Australian Rainfall

Increased frequency of extreme Indian Ocean Dipole events due to greenhouse warming

Interactions of ENSO, the IOD, and the SAM in CMIP3 Models

Nonlinear El Niño impacts on the global economy under climate change

Severe heat waves in Southern Australia: synoptic climatology and large scale connections

Butterfly effect and a self-modulating El Niño response to global warming

Climate-change impact on the 20th-century relationship between the Southern Annular Mode and global mean temperature

Did Climate Change–Induced Rainfall Trends Contribute to the Australian Millennium Drought?

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