‘It is well known that Australia displays marked climate variability ranging from long and destructive droughts to sudden and pervading flooding, interspersed with severe life and property threatening bushfires. Therefore, in order to minimise the impacts on the social and economic security and well-being of Australians, the quantification and understanding of climatological and hydrological variability is of considerable importance for properly estimating the risk of climate related emergencies (e.g. floods, bushfires) occurring in an upcoming season or year. At present, risk estimation methods are largely empirical in that observed histories It is well known that Australia displays marked climate variability ranging from long and destructive droughts to sudden and pervading flooding, interspersed with severe life and property threatening bushfires. Therefore, in order to minimise the impacts on the social and economic security and well-being of Australians, the quantification and understanding of climatological and hydrological variability is of considerable importance for properly estimating the risk of climate related emergencies (e.g. floods, bushfires) occurring in an upcoming season or year. At present, risk estimation methods are largely empirical in that observed histories of climate extremes are analysed under the assumption that the chance of an extreme event occurring is the same from one year to the next (Franks and Kuczera, 2002). Traditionally, physical climatological mechanisms that actually deliver climate extremes have not been taken into account.
Despite the development of rigorous frameworks to assess the uncertainty of risk estimates, these techniques have not previously acknowledged the possibility of distinct periods of elevated or reduced risk. However, recent research has highlighted the existence of multi-decadal epochs of enhanced/reduced flood risk across NSW (Franks, 2002a, b; Franks and Kuczera, 2002; Kiem et al., 2003). In particular, Franks and Kuczera (2002) demonstrated that a major shift in flood frequency (from low to high) occurred around 1945. Previous authors have noted that the mid-1940’s also corresponded to a change in both sea surface temperature anomalies as well as atmospheric circulation patterns (Allan et al., 1995), suggesting large-scale ocean-atmospheric circulation patterns are linked to the Australian climate.’ http://www.em.gov.au/Documents/Climate%20variability%20in%20the%20land%20of%20fire%20and%20flooding%20rain.pdf
The rainfall patterns were ‘discovered’ in the 1980′s by a couple of fluvial geomorphologists from the University of Newcastle – at which both Daniele Verdon and Anthony Kiems work. They are part of a group formed around Stewart Franks who developed the idea. The link to ocean patterns was made possible by the description of the PDO by Steven Hare – who was chasing fisheries patterns in North America – in 1996.
Rainfall means vary considerably over multi decadal periods – so it is a non-stationary times series. The US has some of the same influences but is influenced by the Arctic as we are by the Antarctic.
http://s1114.photobucket.com/user/Chief_Hydrologist/media/USdrought_zps2629bb8c.jpg.html?sort=3&o=9
Fisheries, rainfall, global temperature and these patterns of global ocean and atmospheric variability share a temporal signature and the question as always is what drives it.
‘The work presented here is consistent with the interpretation of a recently reported effect [25] of solar variability on the North Atlantic Oscillation (NAO) and European winter temperatures over the interval 1659–2010 in terms of top-down modulation of the blocking phenomenon [52, 53]. ‘ http://iopscience.iop.org/1748-9326/5/3/034008/fulltext/
You can be assured that Australian scientists are hard at work understanding equivalent processes in the SH.
It was the penguins what done it.