Why is the amplitude of the Indian Ocean Dipole overly large in CMIP3 and CMIP5 climate models?WENJU CAI; COWAN, Tim.Geophysical research letters. 2013, Vol 40, Num 6, pp 1200-1205, issn 0094-8276, 6 p.Article

Dynamics of late autumn rainfall reduction over southeastern AustraliaWENJU CAI; COWAN, Tim.Geophysical research letters. 2008, Vol 35, Num 9, issn 0094-8276, L09708.1-L09708.5Article

Trends in Southern Hemisphere circulation in IPCC AR4 models over 1950-99: Ozone depletion versus greenhouse forcingWENJU CAI; COWAN, Tim.Journal of climate. 2007, Vol 20, Num 4, pp 681-692, issn 0894-8755, 12 p.Article

Impacts of increasing anthropogenic aerosols on the atmospheric circulation trends of the Southern Hemisphere : An air-sea positive feedbackWENJU CAI; COWAN, Tim.Geophysical research letters. 2007, Vol 34, Num 23, issn 0094-8276, L23709.1-L23709.5Article

Southeast Australia Autumn Rainfall Reduction: A Climate-Change-Induced Poleward Shift of Ocean―Atmosphere CirculationWENJU CAI; COWAN, Tim.Journal of climate. 2013, Vol 26, Num 1, pp 189-205, issn 0894-8755, 17 p.Article

Evidence of impacts from rising temperature on inflows to the Murray-Darling BasinWENJU CAI; COWAN, Tim.Geophysical research letters. 2008, Vol 35, Num 7, issn 0094-8276, L07701.1-L07701.5Article

SAM and regional rainfall in IPCC AR4 models : Can anthropogenic forcing account for southwest western australian winter rainfall reduction?WENJU CAI; COWAN, Tim.Geophysical research letters. 2006, Vol 33, Num 24, issn 0094-8276, L24708.1-L24708.5Article

Rainfall Teleconnections with Indo-Pacific Variability in the WCRP CMIP3 ModelsWENJU CAI; SULLIVAN, Arnold; COWAN, Tim et al.Journal of climate. 2009, Vol 22, Num 19, pp 5046-5071, issn 0894-8755, 26 p.Article

Shoaling of the off-equatorial south Indian Ocean thermocline : Is it driven by anthropogenic forcing?WENJU CAI; SULLIVAN, Arnold; COWAN, Tim et al.Geophysical research letters. 2008, Vol 35, Num 12, issn 0094-8276, L12711.1-L12711.5Article

Influence of Global-Scale Variability on the Subtropical Ridge over Southeast AustraliaWENJU CAI; RENSCH, Peter Van; COWAN, Tim et al.Journal of climate. 2011, Vol 24, Num 23, pp 6035-6053, issn 0894-8755, 19 p.Article

Impacts of precipitation and temperature changes on annual streamflow in the Murray-Darling Basin : The effects of changing rainfall on watershedsJINGJIE YU; GUOBIN FU; WENJU CAI et al.Water international. 2010, Vol 35, Num 3, pp 313-323, issn 0250-8060, 11 p.Article

Rising temperature depletes soil moisture and exacerbates severe drought conditions across southeast AustraliaWENJU CAI; COWAN, Tim; BRIGGS, Peter et al.Geophysical research letters. 2009, Vol 36, Num 21, issn 0094-8276, L21709.1-L21709.5Article

Interactions of ENSO, the IOD, and the SAM in CMIP3 ModelsWENJU CAI; SULLIVAN, Arnold; COWAN, Tim et al.Journal of climate. 2011, Vol 24, Num 6, pp 1688-1704, issn 0894-8755, 17 p.Article

More Frequent, Longer, and Hotter Heat Waves for Australia in the Twenty-First CenturyCOWAN, Tim; PURICH, Ariaan; PERKINS, Sarah et al.Journal of climate. 2014, Vol 27, Num 15, pp 5851-5871, issn 0894-8755, 21 p.Article

Autumn Precipitation Trends over Southern Hemisphere Midlatitudes as Simulated by CMIP5 ModelsPURICH, Ariaan; COWAN, Tim; MIN, Seung-Ki et al.Journal of climate. 2013, Vol 26, Num 21, pp 8341-8356, issn 0894-8755, 16 p.Article

Asymmetry in ENSO Teleconnection with Regional Rainfall, Its Multidecadal Variability, and ImpactWENJU CAI; VAN RENSCH, Peter; COWAN, Tim et al.Journal of climate. 2010, Vol 23, Num 18, pp 4944-4955, issn 0894-8755, 12 p.Article

The Association of Tropical and Extratropical Climate Modes to Atmospheric Blocking across Southeastern AustraliaCOWAN, Tim; VAN RENSCH, Peter; PURICH, Ariaan et al.Journal of climate. 2013, Vol 26, Num 19, pp 7555-7569, issn 0894-8755, 15 p.Article

An Asymmetry in the IOD and ENSO Teleconnection Pathway and Its Impact on Australian ClimateWENJU CAI; VAN RENSCH, Peter; COWAN, Tim et al.Journal of climate. 2012, Vol 25, Num 18, pp 6318-6329, issn 0894-8755, 12 p.Article

Teleconnection Pathways of ENSO and the IOD and the Mechanisms for Impacts on Australian RainfallWENJU CAI; VAN RENSCH, Peter; COWAN, Tim et al.Journal of climate. 2011, Vol 24, Num 15, pp 3910-3923, issn 0894-8755, 14 p.Article

Are Anthropogenic Aerosols Responsible for the Northwest Australia Summer Rainfall Increase? A CMIP3 Perspective and ImplicationsWENJU CAI; COWAN, Tim; SULLIVAN, Arnold et al.Journal of climate. 2011, Vol 24, Num 10, pp 2556-2564, issn 0894-8755, 9 p.Article

Annual sea surface temperature lag as an indicator of regional climate variabilityLI, Chung-Leong; BYE, John A. T; GALLAGHER, Stephen J et al.International journal of climatology. 2013, Vol 33, Num 10, pp 2309-2317, issn 0899-8418, 9 p.Article

Variability and Trend of North West Australia Rainfall : Observations and Coupled Climate ModelingGE SHI; WENJU CAI; COWAN, Tim et al.Journal of climate. 2008, Vol 21, Num 12, pp 2938-2959, issn 0894-8755, 22 p.Article

Did Climate Change-Induced Rainfall Trends Contribute to the Australian Millennium Drought?WENJU CAI; PURICH, Ariaan; COWAN, Tim et al.Journal of climate. 2014, Vol 27, Num 9, pp 3145-3168, issn 0894-8755, 24 p.Article

Anthropogenic aerosol forcing and the structure of temperature trends in the southern Indian OceanWENJU CAI; COWAN, Tim; DIX, Martin et al.Geophysical research letters. 2007, Vol 34, Num 14, issn 0094-8276, L14611.1-L14611.5Article

More extreme swings of the South Pacific convergence zone due to greenhouse warmingCAVI, Wenju; LENGAIGNE, Matthieu; NGARI, Arona et al.Nature (London). 2012, Vol 488, Num 7411, pp 365-369, issn 0028-0836, 5 p.Article