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Implications of Climate Change for Australia's World Heritage ...

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IMPLICATIONS OF CLIMATE CHANGE FOR AUSTRALIA’S WORLD HERITAGE PROPERTIES: A PRELIMINARY ASSESSMENT<br />

Rainfall and extreme weather events<br />

Higher temperatures and changes in humidity—as well as extreme weather events including wind, severe rain, lightning and<br />

hail—can have a direct impact on the fabric <strong>of</strong> buildings and culturally significant gardens. <strong>Change</strong>s in rainfall (prolonged<br />

drought or excessive rainfall) can also affect building fabric, vegetation and soil chemistry (UNESCO 2006). Soils containing<br />

high clay content can, potentially, result in serious cracking during prolonged droughts. Timber buildings may become more<br />

vulnerable to an increase in pest and biological infestations. Newer buildings made from concrete, steel and tiles (e.g. Sydney<br />

Opera House) are likely to be more resilient to these climatic factors than older buildings constructed from brick, timber, steel<br />

and slate (e.g. Royal Exhibition Building).<br />

The rock art sites in Kakadu National Park represent ‘a masterpiece <strong>of</strong> human creative genius’, and are considered one<br />

<strong>of</strong> the greatest concentrations <strong>of</strong> rock art in the world. Without doubt, rainwater is the primary agent responsible <strong>for</strong> the<br />

deterioration <strong>of</strong> rock art (Pearson 1978; Pearson & Swartz 1991). Rainwater flowing over rock surfaces can result in extensive<br />

rock art damage, although the destructive impacts <strong>of</strong> water can be lessened through the use <strong>of</strong> silicone drip lines that divert<br />

water away from rock art surfaces.<br />

Historically, extensive flooding has had a devastating impact on rock art and archaeological sites (Rosenfeld 1985). Rock art<br />

values could be at risk from an increase in rainfall in northern Australian sites (such as Kakadu National Park). Extreme fire<br />

events also lead to rock flaking and soot accumulation (Pearson 1978).<br />

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