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QA_Vol 24_No 1_July 2007 - Australasian Quaternary Association

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Conference ReportThe 2nd International Young Scientists’Global Change Conference, ANDThe 2nd Earth System Science Partnership’sOpen Science ConferenceGlobal Environmental Change: Regional Challenges<strong>No</strong>vember 2006 Beijing ChinaJoëlle GergisSchool of Creative Media, RMIT University, Melbourne Victoria 3001Email: jgergis@gmail.comIn <strong>No</strong>vember 2006, I had the privilege of representingAustralian palaeoclimatology at two internationalmeetings on global change research held in Beijing,China. They profoundly challenged my views on the threatposed by global warming. Climate change is very real,happening now, and the rate of change is accelerating. Iwas struck by the urgency for direct and immediate actionneeded - at every level, in every nation.The first conference I attended was the InternationalYoung Scientists’ Global Change Conference (YSC)(Figure 1). The YSC took place <strong>No</strong>vember 5–8, 2006 theChina Meteorological Administration campus in Beijing,China. The conference was sponsored by the EarthSystem Science Partnership (ESSP) and was organised bythe global change SysTem for Analysis, Research andTraining (START) and the China MeteorologicalAdministration. START is a capacity building initiative forglobal change researchers funded by the ESSP program(detailed below). It targets developing countries andcollaborations that conduct research on regionalenvironmental change, the assessment of impacts andvulnerabilities to such changes, and information topolicy-makers.It brought together 100 young scientists from 35 countriesto discuss some of the key challenges facing ourscientific discipline, and the implications they hold forthe future of global sustainability. Four people attendedthe meeting from our region, including three Australians(Ben Preston (CSIRO), Anna Richards (University ofQueensland) and myself) and one New Zealander (OliviaWarrick (Victoria University)). I was the only Australian(and palaeoclimatologist) to address the congress.The conference was an excellent platform for youngscientists to present their research findings to both peersand leading scientists in the environmental change field.Keynote speakers included distinguished climatologistand numerical modeller Prof. Congbin Fu (China) andProf. Paul Crutzen (USA), who received the <strong>No</strong>bel Prize in1995 for his research on atmospheric ozone. The meetingwas organised into six themes:• Earth system variability and modelling• Ocean, freshwater and coastal systems• Land ecosystem and biodiversity• Biogeochemical cycles; cryospheric studies• Human vulnerability and risk management• Global change and agricultural systemsMy talk addressed uncertainties surrounding late 20thcentury El Niño-Southern Oscillation (ENSO) extremes(Gergis and Fowler, 2005). This involved reconstructingthe long-term history of ENSO using high-resolutionpalaeoarchives including tree-rings, corals, ice-cores anddocumentary records (Gergis et al., 2006). Previous ENSOreconstructions have been geographically biased towardEast Pacific teleconnection regions, with little representationof sites influenced by the Western Pacific warmpool. I presented the first large-scale Southern Hemisphereeffort to reconstruct ENSO using an expandednetwork of recently developed Western Pacific palaeoarchives.Of the total number of extreme El Niño/La Niña eventyears reconstructed since A.D. 1525, 43% occur in the 20thcentury. Strikingly, 30% of all reconstructed ENSO eventyears occur post-1940 alone, suggesting that recent ENSOvariability appears anomalous in the context of the pastfive centuries (Gergis and Fowler, 2005). These resultssuggest it is likely that ENSO operates differently undernatural (pre-industrial) and human-influenced backgroundstates. Given the large-scale socio-economicimpacts of ENSO events, investigations into how continuedglobal warming will influence future ENSObehaviour are vital.Over the course of the conference, we were encouragedto informally discuss the question “What are the bigquestions in global change science?” This lead to somevery interesting conversations, as it is not often you getphysical and social scientists from 35 countries in thesame room! Collectively, we identified three main areas:• Detection and attribution of physical climate cyclesand their forcing mechanisms;• Improved inter-disciplinary communication of sciencewithin and beyond the scientific communities;40 | <strong>Quaternary</strong> AUSTRALASIA <strong>24</strong> (2)

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