School of Earth Sciences - Theses
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ItemHydrological extremes and consequences of climate change( 2013)In the design of infrastructure, risk has been – and often still is – assessed on the basis of long-term averages. Information on variation in hydrological extremes is required as the basis for informed decision-making, preparedness and possible adaptation. Long-term trends are fairly well understood for temperature but less well for precipitation. While climate models have become sophisticated tools for projecting future changes in our climate, their ability to replicate observed variations in precipitation is limited and it is therefore prudent to complement climate models through analysis of historical observations. Design rainfall is used as one of the required inputs for hydrological models in the design of structures such as dams and bridges. Design rainfall estimates are supplied in form of intensity-frequency-duration curves. Rainfall frequency analysis is almost invariably based on the assumption of a stationary climate. Sub-daily durations are of particular interest for urban applications. This thesis was strongly driven by the motivation to provide guidance to decision makers who have to account for non-stationarity in rainfall extremes. Non-stationarity in rainfall extremes comes about as a conflation of climate change and climate variability. Unlike for temperature extremes, rainfall extremes for Australia as a whole exhibit no clear increase or decrease in intensity over time but strong association with the El Niño-Southern Oscillation (ENSO). This has implications for the choice of suitable analysis techniques, e.g. sophisticated non-parametric techniques. Depending on the planning horizons both climate change and climate variability may have to be accounted for. The association of rainfall extremes with ENSO leads to an opportunity to develop statistical models to support decision-making on shorter time scales. Analysis of seasonality in frequency and magnitude of rainfall extremes revealed considerable variation across a set of sites in the southeast of Australia, implying different dominating rainfall-producing mechanisms and/or interactions with local topography. The strongest signal for an increase in extreme precipitation is found for short durations. Changes in rainfall extremes come about through a combination of changes in thermodynamical and dynamical variables. To assess large-scale changes in circulation, a classification technique (self-organising maps, SOM) was applied and synoptic types were identified. Rainfall extremes were then related to the synoptic type under which they occurred, to assess observed changes in the frequency of rainfall extremes. Rainfall extremes are typically preceded by conditions that are much wetter (both in absolute and relative terms) and warmer than the climatological average. These anomalies tend to be larger for shorter durations, and for rarer events. Given that increase in humidity exhibits strong regional variability and that it may be counteracted by changes in dynamics, it appears simplistic to state categorically that climate change will lead to an increase in extreme rainfall events and observed trends in rainfall extremes show a picture that is more complex. In summary, the combination of changes in thermodynamic and dynamic variables will define the change in frequency and intensity of rainfall extremes. The factors that are most relevant for the effect of climate change on rainfall extremes depend on geographical location.
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ItemExtending the instrumental climate record of southeastern Australia( 2013)Southeastern Australia (SEA) is the most highly populated and agriculturally productive area of the Australian continent. The region also experiences one of the most variable climates in the world, particularly in terms of interannual rainfall. To understand the influence that anthropogenic climate change will have on future SEA climate, it is important to identify the full range of natural climate variability in the region. However, the current instrumental datasets used for SEA climate research only begin in the early 20th century, restricting efforts to identify long-term climate changes and low-frequency variability. This thesis describes the first instrumental climate record for SEA to extend from European settlement in 1788 to the end of 2012. Historical instrumental observations of air temperature, atmospheric pressure and rainfall over SEA have been located and homogenised for the period 1788 to 1909. The historical observations have then been combined with existing high-quality SEA climate data for 1910 to 2012 to examine interannual SEA climate variability over the past 225 years. The extended climate record includes a number of previously unpublished observations during 1788–1859, providing new insight into the climate experienced by early European settlers in Australia. The interannual climate variability identified using the extended record is in good agreement with SEA documentary records, palaeoclimate reconstructions and a historical reanalysis product, verifying the quality of the homogenised pre-1910 SEA climate data. Assessing rainfall variability during 1788–2012 identifies the most recent droughts in 1935–1942 and 1997–2009 as the longest periods of rainfall deficit in SEA since at least 1832, when continuous rainfall observations begin. Conversely, prolonged wet periods during the 1870s and 1890s appear to be more extreme than more recent wet conditions experienced in the 1950s and 1970s. Analysis of the extended SEA temperature record reveals that the current positive temperature trend seen in the region is the strongest and most significant since at least 1860. Long-term stability of teleconnections associated with climate variations in the SEA region are also examined, with a focus on the influence of El Niño–Southern Oscillation (ENSO) on SEA rainfall. Breakdowns in the ENSO–SEA rainfall relationship are identified during 1835–1850 and 1920–1959, in agreement with previous observational and palaeoclimate studies. The decrease in ENSO–SEA rainfall correlations appear to be associated with changes in the Southern Hemisphere mid-latitude meridional pressure gradient, possibly linked to prolonged negative phases of the Southern Annular Mode. The extended instrumental climate record developed in this thesis makes a significant contribution to the emerging field of historical climatology in Australia. It offers valuable new data for historians, climatologists and palaeoclimatologists exploring SEA’s past and present climate. As the regional impacts of anthropogenic climate change become an increasing reality, improved understanding of past climate variability is vital for future climate research.
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ItemDrivers of Southern Hemisphere climate change( 2013)The climate of the Southern Hemisphere (SH) has undergone significant changes over recent decades, with additional warming expected under future emission scenarios. However, while temperature increases are robust across models there is more uncertainty around changes in rainfall, atmospheric circulation and extremes, all of which have a large impact on human society and ecosystems. The objective of this thesis was to increase our confidence in future projections by considering the relative importance of various drivers of past and future climate change, with a focus on the Southern Hemisphere. These drivers include sea surface temperatures (SSTs; which may or may not be anthropogenically forced), greenhouse gases and stratospheric ozone. To achieve this objective a hierarchy of model experiments were utilised, from idealised experiments to multimodel datasets. Insights were gained by exploring both the consistencies and the spread across the model results. The main results were: 1) The internal variability of the climate system, such as the El Niño-Southern Oscillation (ENSO), impacts the emerging signals of anthropogenic climate change and characterisations of this noise were explored. Opposite phases of ENSO were found to drive marked contrasts in maximum temperature extremes, with ENSO fidelity crucial in simulating the observed relationships. These patterns are unlikely to change substantially under future climate change. Over the Australian continent, future warming leads to increases in warm temperature extremes and a propensity for longer dry spells interspersed with heavy rainfall events. In general, the magnitude of changes in both temperature and precipitation extremes indices scaled with the strength of emissions. 2) Coupled model simulations were able to reproduce the large-scale features of SH climate trends since 1950, if observed changes in anthropogenic forcings were included. However, atmospheric models driven by observed SSTs and anthropogenic forcings were unable to capture wintertime trends, suggesting either deficiencies in the modelling framework, SSTs or models themselves or that internal variability has been largely responsible for these trends. The improvement of the simulated trends in experiments with partial coupling suggests the modelling framework plays some role in this deficiency. 3) Future changes in the SH atmospheric circulation will be driven by the competing effects of greenhouse gases and stratospheric ozone recovery. Climate sensitivity was found to largely explain the difference in Southern Annular Mode (SAM) projections between two coupled climate models under identical greenhouse gas and stratospheric ozone forcing. This result extended to multimodel simulations under transient carbon dioxide (CO2) conditions in all seasons, with the stronger the warming the larger the trend in the SAM. Tropical upper tropospheric warming was found to be more relevant than polar stratospheric cooling to the model spread in SAM responses to CO2. 4) Idealised SST experiments in two models showed a consistent poleward shift of the SH wintertime westerly jet under Southern Ocean cooling. However, the austral winter response to increased tropical SSTs was found to be model dependent, with opposite latitudinal shifts in the SH westerly jet in the two models. This finding was linked to different tropical rainfall and convective atmospheric heating responses in the models to identical SST increases. These results highlight the reliability of current climate model simulations as well as some of their limitations. Potential deficiencies in forcing datasets, modelling frameworks and the simulation of internal variability were identified. Understanding and improving these deficiencies is crucial for interpreting recent observed change and understanding future projections, particularly at the regional scale.