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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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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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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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The early 20th century warming: Anomalies, causes, and consequences

Wiley interdisciplinary reviews. Climate change, 2018-07, Vol.9 (4), p.e522-n/a

2018

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Using the evaporative stress index to monitor flash drought in Australia

Environmental research letters, 2019-06, Vol.14 (6), p.64016

2019

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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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Projected response of the Indian Ocean Dipole to greenhouse warming

Nature geoscience, 2013-12, Vol.6 (12), p.999-1007

2013

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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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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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Causes of climate change over the historical record

Environmental research letters, 2019-12, Vol.14 (12), p.123006

2019

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An Asymmetry in the IOD and ENSO Teleconnection Pathway and Its Impact on Australian Climate

Journal of climate, 2012-09, Vol.25 (18), p.6318-6329

2012

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Groundwater storage trends in the Loess Plateau of China estimated from streamflow records

Journal of hydrology (Amsterdam), 2015-11, Vol.530, p.281-290

2015

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SAM and regional rainfall in IPCC AR4 models: Can anthropogenic forcing account for southwest Western Australian winter rainfall reduction?

Geophysical research letters, 2006-12, Vol.33 (24), p.L24708-n/a

2006

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Trends in Southern Hemisphere Circulation in IPCC AR4 Models over 1950–99: Ozone Depletion versus Greenhouse Forcing

Journal of climate, 2007-02, Vol.20 (4), p.681-693

2007

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Multi-week prediction of livestock chill conditions associated with the northwest Queensland floods of February 2019

Scientific reports, 2022-04, Vol.12 (1), p.5907-5907, Article 5907

2022

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Factors Contributing to Record-Breaking Heat Waves over the Great Plains during the 1930s Dust Bowl

Journal of climate, 2017-04, Vol.30 (7), p.2437-2461

2017

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Autumn Precipitation Trends over Southern Hemisphere Midlatitudes as Simulated by CMIP5 Models

Journal of climate, 2013-11, Vol.26 (21), p.8341-8356

2013

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Improving the seasonal prediction of Northern Australian rainfall onset to help with grazing management decisions

Climate services, 2020-08, Vol.19, p.100182, Article 100182

2020

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Disentangling the causes of the 1816 European year without a summer

Environmental research letters, 2019-09, Vol.14 (9), p.94019

2019

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Forcing of anthropogenic aerosols on temperature trends of the sub-thermocline southern Indian Ocean

Scientific reports, 2013-07, Vol.3 (1), p.2245, Article 2245

2013

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Shoaling of the off-equatorial south Indian Ocean thermocline: Is it driven by anthropogenic forcing?

Geophysical research letters, 2008-06, Vol.35 (12), p.L12711-n/a

2008

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Impacts of increasing anthropogenic aerosols on the atmospheric circulation trends of the Southern Hemisphere: An air-sea positive feedback

Geophysical research letters, 2007-12, Vol.34 (23), p.L23709-n/a

2007

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More Frequent, Longer, and Hotter Heat Waves for Australia in the Twenty-First Century

Journal of climate, 2014-08, Vol.27 (15), p.5851-5871

2014

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Seasonal climate forecast-an important tool in managing the risk of extreme weather events in Australia's wheat industry

Agricultural and forest meteorology, 2024-05, Vol.351, p.110005, Article 110005

2024

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

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

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

The early 20th century warming: Anomalies, causes, and consequences

Using the evaporative stress index to monitor flash drought in Australia

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

Projected response of the Indian Ocean Dipole to greenhouse warming

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

Dynamics of late autumn rainfall reduction over southeastern Australia

Causes of climate change over the historical record

An Asymmetry in the IOD and ENSO Teleconnection Pathway and Its Impact on Australian Climate

Groundwater storage trends in the Loess Plateau of China estimated from streamflow records

SAM and regional rainfall in IPCC AR4 models: Can anthropogenic forcing account for southwest Western Australian winter rainfall reduction?

Trends in Southern Hemisphere Circulation in IPCC AR4 Models over 1950–99: Ozone Depletion versus Greenhouse Forcing

Multi-week prediction of livestock chill conditions associated with the northwest Queensland floods of February 2019

Factors Contributing to Record-Breaking Heat Waves over the Great Plains during the 1930s Dust Bowl

Autumn Precipitation Trends over Southern Hemisphere Midlatitudes as Simulated by CMIP5 Models

Improving the seasonal prediction of Northern Australian rainfall onset to help with grazing management decisions

Disentangling the causes of the 1816 European year without a summer

Forcing of anthropogenic aerosols on temperature trends of the sub-thermocline southern Indian Ocean

Shoaling of the off-equatorial south Indian Ocean thermocline: Is it driven by anthropogenic forcing?

Impacts of increasing anthropogenic aerosols on the atmospheric circulation trends of the Southern Hemisphere: An air-sea positive feedback

More Frequent, Longer, and Hotter Heat Waves for Australia in the Twenty-First Century

Seasonal climate forecast-an important tool in managing the risk of extreme weather events in Australia's wheat industry

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