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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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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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Weather conditions conducive to Beijing severe haze more frequent under climate change

Nature climate change, 2017-04, Vol.7 (4), p.257-262

2017

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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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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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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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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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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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Increasing frequency of extreme El Niño events due to greenhouse warming

Nature climate change, 2014-02, Vol.4 (2), p.111-116

2014

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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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Anthropogenic Aerosols Cause Recent Pronounced Weakening of Asian Summer Monsoon Relative to Last Four Centuries

Geophysical research letters, 2019-05, Vol.46 (10), p.5469-5479

2019

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Continued increase of extreme El Niño frequency long after 1.5 °C warming stabilization

Nature climate change, 2017-08, Vol.7 (8), p.568-572

2017

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The asymmetric influence of the positive and negative IOD events on China's rainfall

Scientific reports, 2014-05, Vol.4 (1), p.4943-4943, Article 4943

2014

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Future Slower Reduction of Anthropogenic Aerosols Enhances Extratropical Ocean Surface Warming Trends

Geophysical research letters, 2024-04, Vol.51 (8), p.n/a

2024

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Rainfall reductions over Southern Hemisphere semi-arid regions: the role of subtropical dry zone expansion

Scientific reports, 2012-10, Vol.2 (1), p.702-702, Article 702

2012

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Role of external forcing in the time-varying trends of global-mean surface temperature under current and future climates

Environmental research letters, 2024-04, Vol.19 (4), p.44038

2024

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Asymmetry in ENSO Teleconnection with Regional Rainfall, Its Multidecadal Variability, and Impact

Journal of climate, 2010-09, Vol.23 (18), p.4944-4955

2010

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Evidence for link between modelled trends in Antarctic sea ice and underestimated westerly wind changes

Nature communications, 2016-02, Vol.7 (1), p.10409-9, Article 10409

2016

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Polar amplification dominated by local forcing and feedbacks

Nature climate change, 2018-12, Vol.8 (12), p.1076-1081

2018

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Dynamics of late autumn rainfall reduction over southeastern Australia

Geophysical research letters, 2008-05, Vol.35 (9), p.L09708-n/a

2008

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The 2011 southeast Queensland extreme summer rainfall: A confirmation of a negative Pacific Decadal Oscillation phase?

Geophysical research letters, 2012-04, Vol.39 (8), p.n/a

2012

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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

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

Weather conditions conducive to Beijing severe haze more frequent under climate change

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

Increased variability of the western Pacific subtropical high 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

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

Nonlinear El Niño impacts on the global economy under climate change

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

Increasing frequency of extreme El Niño events due to greenhouse 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?

Anthropogenic Aerosols Cause Recent Pronounced Weakening of Asian Summer Monsoon Relative to Last Four Centuries

Continued increase of extreme El Niño frequency long after 1.5 °C warming stabilization

The asymmetric influence of the positive and negative IOD events on China's rainfall

Future Slower Reduction of Anthropogenic Aerosols Enhances Extratropical Ocean Surface Warming Trends

Rainfall reductions over Southern Hemisphere semi-arid regions: the role of subtropical dry zone expansion

Role of external forcing in the time-varying trends of global-mean surface temperature under current and future climates

Asymmetry in ENSO Teleconnection with Regional Rainfall, Its Multidecadal Variability, and Impact

Evidence for link between modelled trends in Antarctic sea ice and underestimated westerly wind changes

Polar amplification dominated by local forcing and feedbacks

Dynamics of late autumn rainfall reduction over southeastern Australia

The 2011 southeast Queensland extreme summer rainfall: A confirmation of a negative Pacific Decadal Oscillation phase?

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