<mets:mets OBJID="oai:utas.edu.au:4011" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:mods="http://www.loc.gov/mods/v3" LABEL="Eprints Item" xsi:schemaLocation="http://www.loc.gov/METS/ http://www.loc.gov/standards/mets/mets.xsd http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-0.xsd" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mets="http://www.loc.gov/METS/"><mets:metsHdr CREATEDATA="2009-01-08T01:37:59Z"><mets:agent TYPE="ORGANIZATION" ROLE="CUSTODIAN"><mets:name>UTas ePrints</mets:name></mets:agent></mets:metsHdr><mets:dmdSec ID="DMD_oai:utas.edu.au:4011_mods"><mets:mdWrap MDTYPE="mods"><mets:xmlData><mods:titleInfo><mods:title>Antarctic iceberg distribution and dissolution from ship-based observations</mods:title></mods:titleInfo><mods:name type="personal"><mods:namePart type="given">TH</mods:namePart><mods:namePart type="family">Jacka</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:name type="personal"><mods:namePart type="given">AB</mods:namePart><mods:namePart type="family">Giles</mods:namePart><mods:role><mods:roleTerm type="text">author</mods:roleTerm></mods:role></mods:name><mods:abstract>The Australian Antarctic Program’s iceberg dataset (from ship-based observations),&#13;
including information from the austral summer seasons 1984/85 to 1999/2000, is examined and used&#13;
to extend earlier studies. Using ‘snapshots’ of the iceberg population to provide an idea of the iceberg&#13;
life cycle, the distribution of icebergs between 60 and 1508 E is discussed in terms of calving regions and&#13;
ocean currents. Temporal changes are also examined. The discussion leads us to the point where we can&#13;
define an area, bounded to the north by the maximum sea-ice limit and to the south by the Antarctic&#13;
Divergence, in which icebergs are confined as they drift eastward. This allows estimation of total&#13;
dissolution, in terms of iceberg numbers and volume, within 108 longitudinal sectors and, with&#13;
knowledge of drift speeds, iceberg movement rates and freshwater input across the sector. Iceberg&#13;
dissolution rates are found to be 0.03–0.05md–1 and the total mass contribution of fresh water to the&#13;
ocean as the icebergs traverse our 308 of longitude study sector is 32 Gt. This amounts to a&#13;
contribution equivalent to precipitation of 15.5cm a–1, accounting for 2% of the total iceberg&#13;
discharge from the Antarctic ice sheet.</mods:abstract><mods:classification authority="lcc">260115 Glaciology</mods:classification><mods:originInfo><mods:dateIssued encoding="iso8061">2007</mods:dateIssued></mods:originInfo><mods:originInfo><mods:publisher>International Glaciological Society</mods:publisher></mods:originInfo><mods:genre>Article</mods:genre></mets:xmlData></mets:mdWrap></mets:dmdSec><mets:amdSec ID="TMD_oai:utas.edu.au:4011"><mets:rightsMD ID="rights_oai:utas.edu.au:4011_mods"><mets:mdWrap MDTYPE="mods"><mets:xmlData><mods:useAndReproduction>
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