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Optimal site selection for a high-resolution ice core record in East Antarctica

dc.contributor.authorVance, Tessa R.
dc.contributor.authorRoberts, Jason L.
dc.contributor.authorMoy, Andrew D.
dc.contributor.authorCurran, Mark A. J.
dc.contributor.authorTozer, Carly R.
dc.contributor.authorGallant, Ailie J. E.
dc.contributor.authorAbram, Nerilie
dc.contributor.authorvan Ommen, Tas
dc.contributor.authorYoung, Duncan A.
dc.contributor.authorGrima, Cyril
dc.contributor.authorBlankenship, Don D.
dc.contributor.authorSiegert, Martin J.
dc.date.accessioned2018-05-23T05:30:07Z
dc.date.available2018-05-23T05:30:07Z
dc.date.issued2016
dc.description.abstractIce cores provide some of the best-dated and most comprehensive proxy records, as they yield a vast and growing array of proxy indicators. Selecting a site for ice core drilling is nonetheless challenging, as the assessment of potential new sites needs to consider a variety of factors. Here, we demonstrate a systematic approach to site selection for a new East Antarctic high-resolution ice core record. Specifically, seven criteria are considered: (1) 2000-year-old ice at 300 m depth; (2) above 1000 m elevation; (3) a minimum accumulation rate of 250 mm years−1 IE (ice equivalent); (4) minimal surface reworking to preserve the deposited climate signal; (5) a site with minimal displacement or elevation change in ice at 300 m depth; (6) a strong teleconnection to midlatitude climate; and (7) an appropriately complementary relationship to the existing Law Dome record (a high-resolution record in East Antarctica). Once assessment of these physical characteristics identified promising regions, logistical considerations (for site access and ice core retrieval) were briefly considered. We use Antarctic surface mass balance syntheses, along with ground-truthing of satellite data by airborne radar surveys to produce all-of-Antarctica maps of surface roughness, age at specified depth, elevation and displacement change, and surface air temperature correlations to pinpoint promising locations. We also use the European Centre for Medium-Range Weather Forecast ERA 20th Century reanalysis (ERA-20C) to ensure that a site complementary to the Law Dome record is selected. We find three promising sites in the Indian Ocean sector of East Antarctica in the coastal zone from Enderby Land to the Ingrid Christensen Coast (50–100° E). Although we focus on East Antarctica for a new ice core site, the methodology is more generally applicable, and we include key parameters for all of Antarctica which may be useful for ice core site selection elsewhere and/or for other purposes.en_AU
dc.format.mimetypeapplication/pdfen_AU
dc.identifier.issn1814-9332en_AU
dc.identifier.urihttp://hdl.handle.net/1885/143578
dc.publisherEuropean Geosciences Unionen_AU
dc.relationhttp://purl.org/au-research/grants/arc/DP140102059en_AU
dc.rights© Author(s) 2016. CC Attribution 3.0 License.en_AU
dc.sourceClimate of the Pasten_AU
dc.titleOptimal site selection for a high-resolution ice core record in East Antarcticaen_AU
dc.typeJournal articleen_AU
dcterms.accessRightsOpen Accessen_AU
local.bibliographicCitation.issue3en_AU
local.bibliographicCitation.lastpage610en_AU
local.bibliographicCitation.startpage595en_AU
local.contributor.affiliationAbram, N. J., Research School of Earth Sciences, The Australian National Universityen_AU
local.contributor.authoruidU9718469en_AU
local.identifier.ariespublicationU3488905xPUB11760
local.identifier.citationvolume12en_AU
local.identifier.doi10.5194/cp-12-595-2016en_AU
local.publisher.urlhttps://www.egu.eu/en_AU
local.type.statusPublished Versionen_AU

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