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    <title>UTas ePrints - Control of Biological Exposure to UV Radiation in the Arctic Ocean: Comparison of the Roles of Ozone and Riverine Dissolved Organic Matter</title>
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    <meta content="Gibson, John A.E." name="eprints.creators_name" />
<meta content="Vincent, Warwick F." name="eprints.creators_name" />
<meta content="Nieke, Barbara" name="eprints.creators_name" />
<meta content="Pienitz, Reinhard" name="eprints.creators_name" />
<meta content="John.Gibson@utas.edu.au" name="eprints.creators_id" />
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<meta content="Control of Biological Exposure to UV Radiation in the Arctic Ocean: Comparison of the Roles of Ozone and Riverine Dissolved Organic Matter" name="eprints.title" />
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<meta content="260403" name="eprints.subjects" />
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<meta content="Arctic, CDOM, DNA, global change, ozone depletion, phytoplankton, Siberia, transparency, ultraviolet radiation" name="eprints.keywords" />
<meta content="Reports of severe stratospheric ozone depletion over the Arctic have heightened concern about the potential impact
of rising ultraviolet-B (UV-B) radiation on north polar aquatic ecosystems. Our optical measurements and modelling results indicate that the ozone-related UV-B influence on food web processes in the Arctic Ocean is likely to be small relative to the effects caused by variation in the concentrations of natural UV-absorbing compounds, known as chromophoric dissolved organic matter(CDOM), that enter the Arctic basin via its large river inflows. The aim of our present study was to develop and apply a simple
bio-optical index that takes into account the combined effects of attenuation by atmospheric ozone and water column CDOM, and photobiological weighting for high-latitude environments such as the Arctic Ocean. To this end, we computed values for a biologically effective UV dose rate parameter ('weighted transparency' or T*) based on underwater UV measurements in highlatitude
lakes and rivers that discharge into the Arctic Ocean; measured incident UV radiation at Barrow, Alaska; and published biological weighting curves for UV-induced DNA damage and UV photoinhibition of photosynthesis. The results underscore how strongly the Arctic Ocean is influenced by riverine inputs: shifts in CDOM loading (e.g., through climate change, land-use practices, or changes in ocean circulation) can cause variations in biological UV exposure of much greater magnitude than ozone related
effects." name="eprints.abstract" />
<meta content="2000-12" name="eprints.date" />
<meta content="published" name="eprints.date_type" />
<meta content="Arctic" name="eprints.publication" />
<meta content="53" name="eprints.volume" />
<meta content="4" name="eprints.number" />
<meta content="372-382" name="eprints.pagerange" />
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<meta content="AAGAARD, K., and CARMACK, E.C. 1989. The role of sea ice
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studies of hydrocarbons. Organic Geochemistry 28:571–583." name="eprints.referencetext" />
<meta content="Gibson, John A.E. and Vincent, Warwick F. and Nieke, Barbara and Pienitz, Reinhard (2000) Control of Biological Exposure to UV Radiation in the Arctic Ocean: Comparison of the Roles of Ozone and Riverine Dissolved Organic Matter. Arctic, 53 (4). pp. 372-382." name="eprints.citation" />
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<meta content="Reports of severe stratospheric ozone depletion over the Arctic have heightened concern about the potential impact
of rising ultraviolet-B (UV-B) radiation on north polar aquatic ecosystems. Our optical measurements and modelling results indicate that the ozone-related UV-B influence on food web processes in the Arctic Ocean is likely to be small relative to the effects caused by variation in the concentrations of natural UV-absorbing compounds, known as chromophoric dissolved organic matter(CDOM), that enter the Arctic basin via its large river inflows. The aim of our present study was to develop and apply a simple
bio-optical index that takes into account the combined effects of attenuation by atmospheric ozone and water column CDOM, and photobiological weighting for high-latitude environments such as the Arctic Ocean. To this end, we computed values for a biologically effective UV dose rate parameter ('weighted transparency' or T*) based on underwater UV measurements in highlatitude
lakes and rivers that discharge into the Arctic Ocean; measured incident UV radiation at Barrow, Alaska; and published biological weighting curves for UV-induced DNA damage and UV photoinhibition of photosynthesis. The results underscore how strongly the Arctic Ocean is influenced by riverine inputs: shifts in CDOM loading (e.g., through climate change, land-use practices, or changes in ocean circulation) can cause variations in biological UV exposure of much greater magnitude than ozone related
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    <h1 class="ep_tm_pagetitle">Control of Biological Exposure to UV Radiation in the Arctic Ocean: Comparison of the Roles of Ozone and Riverine Dissolved Organic Matter</h1>
    <p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Gibson, John A.E.</span> and <span class="person_name">Vincent, Warwick F.</span> and <span class="person_name">Nieke, Barbara</span> and <span class="person_name">Pienitz, Reinhard</span> (2000) <xhtml:em>Control of Biological Exposure to UV Radiation in the Arctic Ocean: Comparison of the Roles of Ozone and Riverine Dissolved Organic Matter.</xhtml:em> Arctic, 53 (4). pp. 372-382.</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 onmouseover="EPJS_ShowPreview( event, 'doc_preview_872' );" href="http://eprints.utas.edu.au/868/1/Arctic53-4-372.pdf" onmouseout="EPJS_HidePreview( event, 'doc_preview_872' );"><img alt="[img]" src="http://eprints.utas.edu.au/style/images/fileicons/application_pdf.png" class="ep_doc_icon" border="0" /></a><div class="ep_preview" id="doc_preview_872"><table><tr><td><img alt="" src="http://eprints.utas.edu.au/868/thumbnails/1/preview.png" class="ep_preview_image" border="0" /><div class="ep_preview_title">Preview</div></td></tr></table></div></td><td valign="top"><a href="http://eprints.utas.edu.au/868/1/Arctic53-4-372.pdf"><span class="ep_document_citation">PDF</span></a> - Requires a PDF viewer<br />1171Kb</td></tr></table><div class="not_ep_block"><h2>Abstract</h2><p style="padding-bottom: 16px; text-align: left; margin: 1em auto 0em auto">Reports of severe stratospheric ozone depletion over the Arctic have heightened concern about the potential impact
of rising ultraviolet-B (UV-B) radiation on north polar aquatic ecosystems. Our optical measurements and modelling results indicate that the ozone-related UV-B influence on food web processes in the Arctic Ocean is likely to be small relative to the effects caused by variation in the concentrations of natural UV-absorbing compounds, known as chromophoric dissolved organic matter(CDOM), that enter the Arctic basin via its large river inflows. The aim of our present study was to develop and apply a simple
bio-optical index that takes into account the combined effects of attenuation by atmospheric ozone and water column CDOM, and photobiological weighting for high-latitude environments such as the Arctic Ocean. To this end, we computed values for a biologically effective UV dose rate parameter ('weighted transparency' or T*) based on underwater UV measurements in highlatitude
lakes and rivers that discharge into the Arctic Ocean; measured incident UV radiation at Barrow, Alaska; and published biological weighting curves for UV-induced DNA damage and UV photoinhibition of photosynthesis. The results underscore how strongly the Arctic Ocean is influenced by riverine inputs: shifts in CDOM loading (e.g., through climate change, land-use practices, or changes in ocean circulation) can cause variations in biological UV exposure of much greater magnitude than ozone related
effects.</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">Keywords:</th><td valign="top" class="ep_row">Arctic, CDOM, DNA, global change, ozone depletion, phytoplankton, Siberia, transparency, ultraviolet radiation</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/260403.html">260000 Earth Sciences &gt; 260400 Oceanography &gt; 260403 Physical Oceanography</a><br /><a href="http://eprints.utas.edu.au/view/subjects/260402.html">260000 Earth Sciences &gt; 260400 Oceanography &gt; 260402 Chemical Oceanography</a></td></tr><tr><th valign="top" class="ep_row">ID Code:</th><td valign="top" class="ep_row">868</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">Dr John A.E. Gibson</span></span></td></tr><tr><th valign="top" class="ep_row">Deposited On:</th><td valign="top" class="ep_row">26 Mar 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=868;">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&amp;eprintid=868">item control page</a></p>
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