Abstract

Abstract. Extreme temperature and precipitation events occurring in Australia in recent decades have caused significant socio-economic and environmental impacts, and thus determining the factors contributing to these extremes is an active area of research. Many recently occurring record-breaking temperature and rainfall events have now been examined from an extreme event attribution (EEA) perspective. This paper describes a set of studies that have examined the causes of extreme climate events using various general circulation models (GCMs), presenting a comprehensive methodology for GCM-based attribution of extremes of temperature and precipitation observed on large spatial and temporal scales in Australia. First, we review how Coupled Model Intercomparison Project Phase 5 (CMIP5) models have been used to examine the changing odds of observed extremes. Second, we review how a large perturbed initial condition ensemble of a single climate model (CESM) has been used to quantitatively examine the changing characteristics of Australian heat extremes. For each approach, methodological details and applications are provided and limitations highlighted. The conclusions of this methodological review discuss the limitations and uncertainties associated with this approach and identify key unexplored applications of GCM-based attribution of extremes. Ideally, this information will be useful for the application of the described extreme event attribution approaches elsewhere.

Highlights

  • 1.1 Australian weather and climate extremesSince around the year 2000, many high-impact extreme and record-breaking temperature and precipitation events have occurred over Australian regions (Bureau of Meteorology, 2013a, b, c, 2016a)

  • The fraction of attributable risk (FAR) value provides a quantification of the change in probability of the defined event occurring that can be attributed to a particular cause, the difference between the model experiments

  • Coupled Model Intercomparison Project Phase 5 (CMIP5) models were selected for analysis based on (1) their representation of monthly surface air temperature variability in the NINO3.4 region, (2) their representation of Australian rainfall variability and (3) rainfall amount associated with El Niño– Southern Oscillation (ENSO) conditions

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Summary

Australian weather and climate extremes

Since around the year 2000, many high-impact extreme and record-breaking temperature and precipitation events have occurred over Australian regions (Bureau of Meteorology, 2013a, b, c, 2016a). Record-breaking extremes were observed on subdaily to multi-year timescales and on spatial scales ranging from single stations to Australia-wide (Bureau of Meteorology, 2016b) Many of these events were the most extreme since high-quality national records began in 1910. Lewis et al.: Approaches to attribution of extreme temperature and precipitation events ern Annular Mode (SAM), the Subtropical Ridge (STR), and the Madden Julian Oscillation (MJO) (King et al, 2014; Maher and Sherwood, 2014; Min et al, 2013) These large-scale modes may interact with local- and regional-scale processes, such as soil moisture feedbacks, to impact the severity, duration or likelihood of extreme events such as heatwaves (Perkins et al, 2015). Understanding the influences of both these anthropogenic forcings and/or natural climatic variability on recent temperature and rainfall extremes affecting Australia, as well as elsewhere, has become an active research avenue

Extreme event attribution
Model descriptions
Other model ensembles
Specifics of EEA approaches
Model evaluation
FAR calculation and uncertainty assessment
Examples of application to Australian extremes
Expansion to future extremes under varying levels of global mean warming
Ideal applications and specific limitations
Recommendations for future application of GCM-based approaches
Findings
Future directions
Full Text
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