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<title>UTas ePrints - Changes in alpine vegetation related to geomorphological processes and climate change on Hill One, Southern Range, Tasmania, 1989 - 2000</title>
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<meta content="Bridle, K." name="eprints.creators_name" />
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<meta content="Photographs of 84 plots in alpine vegetation, largely consisting of fjaeldmark and bolster heath, on Hill One, Southern Range, Tasmania, were taken in both 1989 and 2000 to compare cover characteristics. Between these two observations, vegetation cover declined in the fjaeldmark, largely as a result of erosion. Declines also occurred on the active depositional lobes, through burial of bolster heath. Within the parts of Hill One where vegetation cover was not lost, graminoids decreased and Pterygopappus lawrencei increased in the bolster heath and tall shrubs displaced bolster heath. Thirty-six per cent of the rocks visible in the 1989 photographs had moved by 2000, the mean area of the individual rocks that moved being 95 cm2. Larger rocks were moved on the exposed western slope than on the leeward eastern slope. Analyses of climatic data from nearby stations for 1979 - 2000 indicated a decline in both precipitation and temperatures and an increase in the frequency of the highest wind speeds, all of which are consistent with the nature of vegetation and geomorphological changes that occurred on the mountain, although a climatic cause is far from proven. Localised cooling and drying, in the two hottest and wettest decades recorded for the globe, emphasises the importance of local data in determining the possible impacts of climatic change on biota.
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<meta content="Photographs of 84 plots in alpine vegetation, largely consisting of fjaeldmark and bolster heath, on Hill One, Southern Range, Tasmania, were taken in both 1989 and 2000 to compare cover characteristics. Between these two observations, vegetation cover declined in the fjaeldmark, largely as a result of erosion. Declines also occurred on the active depositional lobes, through burial of bolster heath. Within the parts of Hill One where vegetation cover was not lost, graminoids decreased and Pterygopappus lawrencei increased in the bolster heath and tall shrubs displaced bolster heath. Thirty-six per cent of the rocks visible in the 1989 photographs had moved by 2000, the mean area of the individual rocks that moved being 95 cm2. Larger rocks were moved on the exposed western slope than on the leeward eastern slope. Analyses of climatic data from nearby stations for 1979 - 2000 indicated a decline in both precipitation and temperatures and an increase in the frequency of the highest wind speeds, all of which are consistent with the nature of vegetation and geomorphological changes that occurred on the mountain, although a climatic cause is far from proven. Localised cooling and drying, in the two hottest and wettest decades recorded for the globe, emphasises the importance of local data in determining the possible impacts of climatic change on biota.
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<h1 class="ep_tm_pagetitle">Changes in alpine vegetation related to geomorphological processes and climate change on Hill One, Southern Range, Tasmania, 1989 - 2000</h1>
<p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Kirkpatrick, J.B.</span> and <span class="person_name">Bridle, K.</span> and <span class="person_name">Lynch, A.J.J.</span> (2002) <xhtml:em>Changes in alpine vegetation related to geomorphological processes and climate change on Hill One, Southern Range, Tasmania, 1989 - 2000.</xhtml:em> Australian Journal of Botany, 50 . pp. 753-759.</p><p style="margin-bottom: 1em" class="not_ep_block"></p><table style="margin-bottom: 1em" class="not_ep_block"><tr><td valign="top" style="text-align:center"><a href="http://eprints.utas.edu.au/1705/1/03.01.17.pdf"><img alt="[img]" src="http://eprints.utas.edu.au/style/images/fileicons/application_pdf.png" class="ep_doc_icon" border="0" /></a></td><td valign="top"><a href="http://eprints.utas.edu.au/1705/1/03.01.17.pdf"><span class="ep_document_citation">PDF</span></a> - Full text restricted - Requires a PDF viewer<br />1797Kb</td></tr></table><p style="margin-bottom: 1em" class="not_ep_block">Official URL: <a href="http://dx.doi.org/10.1071/BT02039">http://dx.doi.org/10.1071/BT02039</a></p><div class="not_ep_block"><h2>Abstract</h2><p style="padding-bottom: 16px; text-align: left; margin: 1em auto 0em auto">Photographs of 84 plots in alpine vegetation, largely consisting of fjaeldmark and bolster heath, on Hill One, Southern Range, Tasmania, were taken in both 1989 and 2000 to compare cover characteristics. Between these two observations, vegetation cover declined in the fjaeldmark, largely as a result of erosion. Declines also occurred on the active depositional lobes, through burial of bolster heath. Within the parts of Hill One where vegetation cover was not lost, graminoids decreased and Pterygopappus lawrencei increased in the bolster heath and tall shrubs displaced bolster heath. Thirty-six per cent of the rocks visible in the 1989 photographs had moved by 2000, the mean area of the individual rocks that moved being 95 cm2. Larger rocks were moved on the exposed western slope than on the leeward eastern slope. Analyses of climatic data from nearby stations for 1979 - 2000 indicated a decline in both precipitation and temperatures and an increase in the frequency of the highest wind speeds, all of which are consistent with the nature of vegetation and geomorphological changes that occurred on the mountain, although a climatic cause is far from proven. Localised cooling and drying, in the two hottest and wettest decades recorded for the globe, emphasises the importance of local data in determining the possible impacts of climatic change on biota.
</p></div><table style="margin-bottom: 1em" cellpadding="3" class="not_ep_block" border="0"><tr><th valign="top" class="ep_row">Item Type:</th><td valign="top" class="ep_row">Article</td></tr><tr><th valign="top" class="ep_row">Subjects:</th><td valign="top" class="ep_row"><a href="http://eprints.utas.edu.au/view/subjects/270700.html">270000 Biological Sciences > 270700 Ecology and Evolution</a><br /><a href="http://eprints.utas.edu.au/view/subjects/270704.html">270000 Biological Sciences > 270700 Ecology and Evolution > 270704 Landscape Ecology</a></td></tr><tr><th valign="top" class="ep_row">ID Code:</th><td valign="top" class="ep_row">1705</td></tr><tr><th valign="top" class="ep_row">Deposited By:</th><td valign="top" class="ep_row"><span class="ep_name_citation"><span class="person_name">Professor J.B. Kirkpatrick</span></span></td></tr><tr><th valign="top" class="ep_row">Deposited On:</th><td valign="top" class="ep_row">30 Aug 2007</td></tr><tr><th valign="top" class="ep_row">Last Modified:</th><td valign="top" class="ep_row">09 Jan 2008 02:30</td></tr><tr><th valign="top" class="ep_row">ePrint Statistics:</th><td valign="top" class="ep_row"><a target="ePrintStats" href="/es/index.php?action=show_detail_eprint;id=1705;">View statistics for this ePrint</a></td></tr></table><p align="right">Repository Staff Only: <a href="http://eprints.utas.edu.au/cgi/users/home?screen=EPrint::View&eprintid=1705">item control page</a></p>
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