Climate Change Science articles for Australia

Time frame: 1 May 2025 - 30 April 2026

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Count: 39

Article ‘Count’ for Climate Change Science.

Journal Count Share
1 0.25
Spatiotemporal patterns and drivers of carbon emissions from on-site wastewater treatment: Evidence from a city-wide long-term network 0.25
1 0.06
Sustained Decline in CFC-12 Emissions from China: Evidence for Successful Phase-out under the Montreal Protocol and Global Implications 0.06
12 4.17
Revealing the Mechanisms of Heat Extremes Using an AI Enabled Diagnostic Framework 0.10
Robust Yet Diverse Tropical Responses to Antarctic Meltwater Across Models 0.25
Understanding CMIP6 Multi‐Model Ensemble Projected Pacific Warming Pattern Variability 0.83
Growth in Production and Environmental Deposition of Trifluoroacetic Acid Due To Long‐Lived CFC Replacements and Anesthetics 0.06
Notable Influence of Internal Variability on the Perceived Difference Between Central and Eastern Pacific El Niño Teleconnections 0.17
A Late Pleistocene-Holocene Record of Tropical Monsoon Climate from Groundwater Noble Gases and Isotopes in the Leizhou Peninsula, Southern China 0.07
Apparent Changes in Pacific Decadal Variability Caused by Anthropogenically Induced Mean State Modulations 0.14
A Diachronic Assessment of Advances in Seasonal Forecasting: Evolution of the APCC Multi‐Model Ensemble Prediction System Over the Last Two Decades 0.05
Time of Emergence of Record‐Shattering Compound Heatwave‐Extreme Precipitation Events and Their Socio‐Economic Exposures 0.25
Observed Increase in Tropical Pacific Ocean Surface Cold-Warm Contrast Is Well Outside Model-Simulated Range 1.00
Changes in Hail Damage Potential in Major Australian Cities With Global Warming 1.00
Contraction of the World's Storm‐Cloud Zones the Primary Contributor to the 21st Century Increase in the Earth's Sunlight Absorption 0.25
1 0.25
Disentangling the relative impacts of precipitation metrics on global crop yields 0.25
3 3.00
Trends in Annual Maximum Sub‐Daily to Daily Precipitation Over Australia 1.00
Improving Methane Emission Estimates in Gippsland: Insights From Bayesian Inversion and In Situ Observations 1.00
Evaluating ERA5 Downscaled Simulations Using CCAM: Large‐Scale Circulation Processes and Teleconnections 1.00
2 0.56
Neglecting land–atmosphere feedbacks overestimates climate-driven increases in evapotranspiration 0.50
Extreme weather event attribution predicts climate policy support across the world 0.06
10 3.07
Deadly heat stress conditions are already occurring for submission to Nature Communications 0.29
Recurring marine phosphorus spikes during major palaeozoic mass extinctions and climate change 0.22
Anthropogenic climate change drives rising global heat stress and its spatial inequality 0.17
Emergence of the enhanced equatorial Atlantic warming as a fingerprint of global warming 0.07
Increased interannual variability of Sahel rainfall under greenhouse warming 0.43
Modulation of inter-hemispheric temperature gradients on the Holocene Asian-Australian summer monsoon 0.19
Temperature variability projections remain uncertain after constraining them to best performing Large Ensembles of individual Climate Models 0.50
Loss of vegetation functions during the Paleocene–Eocene Thermal Maximum 0.17
Scientific literature on carbon dioxide removal revealed as much larger through AI-enhanced systematic mapping 0.04
Learning dynamical systems with hit-and-run random feature maps 1.00
2 0.41
Synchronous bipolar retreat of mid-latitude ice masses during Heinrich Stadials 0.14
Westerly wind shifts drove Southern Hemisphere mid-latitude peat growth since the last glacial 0.28
3 0.28
A speleothem record from the Fertile Crescent covering the last deglaciation better contextualizes neolithization 0.08
Multiple sources of atmospheric CO2 activated by AMOC recovery at the onset of interglacial MIS 9 0.17
Suborbital- and millennial-scale monsoon variability during Pleistocene interglacials 0.03
1 0.03
Why methane surged in the atmosphere during the early 2020s 0.03
3 0.56
Atmospheric systems drive spatiotemporal divergence of dust and moisture changes across Asia over the past 130,000 years 0.03
Present-day tropical precipitation and cloud feedbacks determine future equatorial Pacific trends 0.29
Nonlinear increase of compound drought-heatwave events since the early 2000s 0.25

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