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  5. <title>UTas ePrints - Assessment of mangrove response to projected relative sea-level rise and recent historical reconstruction of shoreline position</title>
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  13. <meta content="Gilman, E." name="eprints.creators_name" />
  14. <meta content="Ellison, J.C." name="eprints.creators_name" />
  15. <meta content="Coleman, Richard" name="eprints.creators_name" />
  16. <meta content="egilman@utas.edu.au" name="eprints.creators_id" />
  17. <meta content="Joanna.Ellison@utas.edu.au" name="eprints.creators_id" />
  18. <meta content="Richard.Coleman@utas.edu.au" name="eprints.creators_id" />
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  20. <meta content="2008-01-28T23:13:01Z" name="eprints.datestamp" />
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  23. <meta content="Assessment of mangrove response to projected relative
  24. sea-level rise and recent historical reconstruction
  25. of shoreline position" name="eprints.title" />
  26. <meta content="pub" name="eprints.ispublished" />
  27. <meta content="300803" name="eprints.subjects" />
  28. <meta content="restricted" name="eprints.full_text_status" />
  29. <meta content="American Samoa . Coastal . Erosion .
  30. Mangrove . Sea-level rise . Wetland" name="eprints.keywords" />
  31. <meta content="The original publication is available at www.springerlink.com
  32. " name="eprints.note" />
  33. <meta content="We predict the decadal change in position of
  34. three American Samoa mangroves from analysis of a
  35. time series of remotely sensed imagery, a geographic
  36. information system, tide gauge data, and projections
  37. for change in sea-level relative to the mangrove surface.
  38. Accurate predictions of changes to coastal ecosystem
  39. boundaries, including in response to projected relative
  40. sea-level rise, enable advanced planning to minimize
  41. and offset anticipated losses and minimize social disruption
  42. and cost of reducing threats to coastal development
  43. and human safety. The observed mean landward
  44. migration of three mangroves’ seaward margins
  45. over four decades was 25, 64, and 72mma−1, 12 to
  46. 37 times the observed relative sea-level rise rate. Two
  47. of the sites had clear trends in reductions in mangrove
  48. area, where there was a highly significant correlation
  49. between the change in position of the seaward mangrove
  50. margin and change in relative sea-level. Here
  51. it can be inferred that the force of sea-level rise relative
  52. to the mangrove surface is causing landward migration.
  53. Shoreline movement was variable at a third
  54. site and not significantly correlated with changing sealevel,
  55. where it is likely that forces other than change in
  56. relative sea-level are predominant. Currently, 16.5%,23.4%, and 68.0% of the three mangroves’ landward
  57. margins are obstructed by coastal development from
  58. natural landward migration. The three mangroves could
  59. experience as high as a 50.0% reduction in area by
  60. the year 2100. A 12% reduction in mangrove area
  61. by the year 2100 is possible in the Pacific islands
  62. region." name="eprints.abstract" />
  63. <meta content="2007-01" name="eprints.date" />
  64. <meta content="published" name="eprints.date_type" />
  65. <meta content="Environmental Monitoring Assessment" name="eprints.publication" />
  66. <meta content="124" name="eprints.volume" />
  67. <meta content="1- 3" name="eprints.number" />
  68. <meta content="105-130" name="eprints.pagerange" />
  69. <meta content="10.1007/s10661-006-9212-y" name="eprints.id_number" />
  70. <meta content="TRUE" name="eprints.refereed" />
  71. <meta content="0167-6369" name="eprints.issn" />
  72. <meta content="http://dx.doi.org/10.1007/s10661-006-9212-y" name="eprints.official_url" />
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  409. Woodroffe, C.D. (1995). Response of tide-dominated mangrove
  410. shorelines in Northern Australia to anticipated sea-level
  411. rise. Earth Surface Processes and Landforms, 20, 65–85.
  412. Woodworth, P.L.,&amp;Blackman, D.L. (2004) Evidence for systematic
  413. changes in extreme high waters since the mid-1970s.
  414. Journal of Climate, 17(6), 1190–1197." name="eprints.referencetext" />
  415. <meta content="Gilman, E. and Ellison, J.C. and Coleman, Richard (2007) Assessment of mangrove response to projected relative sea-level rise and recent historical reconstruction of shoreline position. Environmental Monitoring Assessment, 124 (1- 3). pp. 105-130. ISSN 0167-6369" name="eprints.citation" />
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  418. <meta content="Assessment of mangrove response to projected relative
  419. sea-level rise and recent historical reconstruction
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  421. <meta content="Gilman, E." name="DC.creator" />
  422. <meta content="Ellison, J.C." name="DC.creator" />
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  424. <meta content="300803 Natural Resource Management" name="DC.subject" />
  425. <meta content="We predict the decadal change in position of
  426. three American Samoa mangroves from analysis of a
  427. time series of remotely sensed imagery, a geographic
  428. information system, tide gauge data, and projections
  429. for change in sea-level relative to the mangrove surface.
  430. Accurate predictions of changes to coastal ecosystem
  431. boundaries, including in response to projected relative
  432. sea-level rise, enable advanced planning to minimize
  433. and offset anticipated losses and minimize social disruption
  434. and cost of reducing threats to coastal development
  435. and human safety. The observed mean landward
  436. migration of three mangroves’ seaward margins
  437. over four decades was 25, 64, and 72mma−1, 12 to
  438. 37 times the observed relative sea-level rise rate. Two
  439. of the sites had clear trends in reductions in mangrove
  440. area, where there was a highly significant correlation
  441. between the change in position of the seaward mangrove
  442. margin and change in relative sea-level. Here
  443. it can be inferred that the force of sea-level rise relative
  444. to the mangrove surface is causing landward migration.
  445. Shoreline movement was variable at a third
  446. site and not significantly correlated with changing sealevel,
  447. where it is likely that forces other than change in
  448. relative sea-level are predominant. Currently, 16.5%,23.4%, and 68.0% of the three mangroves’ landward
  449. margins are obstructed by coastal development from
  450. natural landward migration. The three mangroves could
  451. experience as high as a 50.0% reduction in area by
  452. the year 2100. A 12% reduction in mangrove area
  453. by the year 2100 is possible in the Pacific islands
  454. region." name="DC.description" />
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  566. <h1 class="ep_tm_pagetitle">Assessment of mangrove response to projected relative sea-level rise and recent historical reconstruction of shoreline position</h1>
  567. <p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Gilman, E.</span> and <span class="person_name">Ellison, J.C.</span> and <span class="person_name">Coleman, Richard</span> (2007) <xhtml:em>Assessment of mangrove response to projected relative sea-level rise and recent historical reconstruction of shoreline position.</xhtml:em> Environmental Monitoring Assessment, 124 (1- 3). pp. 105-130. ISSN 0167-6369</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/3056/1/Gilman_et_al07_.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/3056/1/Gilman_et_al07_.pdf"><span class="ep_document_citation">PDF</span></a> - Full text restricted - Requires a PDF viewer<br />1497Kb</td><td><form method="get" accept-charset="utf-8" action="http://eprints.utas.edu.au/cgi/request_doc"><input accept-charset="utf-8" value="4191" name="docid" type="hidden" /><div class=""><input value="Request a copy" name="_action_null" class="ep_form_action_button" onclick="return EPJS_button_pushed( '_action_null' )" type="submit" /> </div></form></td></tr></table><p style="margin-bottom: 1em" class="not_ep_block">Official URL: <a href="http://dx.doi.org/10.1007/s10661-006-9212-y">http://dx.doi.org/10.1007/s10661-006-9212-y</a></p><div class="not_ep_block"><h2>Abstract</h2><p style="padding-bottom: 16px; text-align: left; margin: 1em auto 0em auto">We predict the decadal change in position of&#13;
  568. three American Samoa mangroves from analysis of a&#13;
  569. time series of remotely sensed imagery, a geographic&#13;
  570. information system, tide gauge data, and projections&#13;
  571. for change in sea-level relative to the mangrove surface.&#13;
  572. Accurate predictions of changes to coastal ecosystem&#13;
  573. boundaries, including in response to projected relative&#13;
  574. sea-level rise, enable advanced planning to minimize&#13;
  575. and offset anticipated losses and minimize social disruption&#13;
  576. and cost of reducing threats to coastal development&#13;
  577. and human safety. The observed mean landward&#13;
  578. migration of three mangroves’ seaward margins&#13;
  579. over four decades was 25, 64, and 72mma−1, 12 to&#13;
  580. 37 times the observed relative sea-level rise rate. Two&#13;
  581. of the sites had clear trends in reductions in mangrove&#13;
  582. area, where there was a highly significant correlation&#13;
  583. between the change in position of the seaward mangrove&#13;
  584. margin and change in relative sea-level. Here&#13;
  585. it can be inferred that the force of sea-level rise relative&#13;
  586. to the mangrove surface is causing landward migration.&#13;
  587. Shoreline movement was variable at a third&#13;
  588. site and not significantly correlated with changing sealevel,&#13;
  589. where it is likely that forces other than change in&#13;
  590. relative sea-level are predominant. Currently, 16.5%,23.4%, and 68.0% of the three mangroves’ landward&#13;
  591. margins are obstructed by coastal development from&#13;
  592. natural landward migration. The three mangroves could&#13;
  593. experience as high as a 50.0% reduction in area by&#13;
  594. the year 2100. A 12% reduction in mangrove area&#13;
  595. by the year 2100 is possible in the Pacific islands&#13;
  596. region.</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">Additional Information:</th><td valign="top" class="ep_row">The original publication is available at www.springerlink.com&#13;
  597. </td></tr><tr><th valign="top" class="ep_row">Keywords:</th><td valign="top" class="ep_row">American Samoa . Coastal . Erosion .&#13;
  598. Mangrove . Sea-level rise . Wetland</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/300803.html">300000 Agricultural, Veterinary and Environmental Sciences &gt; 300800 Environmental Sciences &gt; 300803 Natural Resource Management</a></td></tr><tr><th valign="top" class="ep_row">Collections:</th><td valign="top" class="ep_row">UNSPECIFIED</td></tr><tr><th valign="top" class="ep_row">ID Code:</th><td valign="top" class="ep_row">3056</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 Joanna Ellison</span></span></td></tr><tr><th valign="top" class="ep_row">Deposited On:</th><td valign="top" class="ep_row">29 Jan 2008 10:13</td></tr><tr><th valign="top" class="ep_row">Last Modified:</th><td valign="top" class="ep_row">29 Jan 2008 10:13</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=3056;">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=3056">item control page</a></p>
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