{"id":2,"date":"2017-09-29T17:51:21","date_gmt":"2017-09-29T17:51:21","guid":{"rendered":"http:\/\/blogs.oregonstate.edu\/icecores\/?page_id=2"},"modified":"2018-04-26T17:49:12","modified_gmt":"2018-04-26T17:49:12","slug":"researchprojects","status":"publish","type":"page","link":"https:\/\/dev.blogs.oregonstate.edu\/icecores\/researchprojects\/","title":{"rendered":"Research Projects"},"content":{"rendered":"<h2><\/h2>\n<p><span style=\"font-weight: 400\">Most of our research investigates the interlinked history of greenhouse gases and climate, and related topics like ice core dating, method development, and various other things.<\/span><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"alignleft wp-image-51 size-medium\" src=\"http:\/\/blogs.oregonstate.edu\/icecores\/files\/2018\/01\/ws6-199x300.jpg\" alt=\"\" width=\"199\" height=\"300\" srcset=\"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/3000\/files\/2018\/01\/ws6-199x300.jpg 199w, https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/3000\/files\/2018\/01\/ws6-768x1157.jpg 768w, https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/3000\/files\/2018\/01\/ws6-680x1024.jpg 680w, https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/3000\/files\/2018\/01\/ws6.jpg 850w\" sizes=\"auto, (max-width: 199px) 100vw, 199px\" \/><\/p>\n<p><b>Current projects include:<\/b><\/p>\n<p><b>Holocene carbon dioxide and nitrous oxide dynamics from the South Pole Ice Core (<\/b><a href=\"http:\/\/spicecore.org\/\"><b>SPICE<\/b><\/a><b>).<\/b><span style=\"font-weight: 400\">\u00a0\u00a0We are using carbon, nitrogen, and oxygen isotopes to try to understand why these two gases change during the last 10,000 years and to constrain the role of early human activities on their abundance.\u00a0\u00a0This follows earlier late Holocene CO<\/span><span style=\"font-weight: 400\">2<\/span><span style=\"font-weight: 400\">work on the WAIS Divide ice core (<\/span><a href=\"http:\/\/www.nature.com\/ngeo\/journal\/v8\/n5\/abs\/ngeo2422.html\"><span style=\"font-weight: 400\">Bauska et al., 2014<\/span><\/a><span style=\"font-weight: 400\">).<\/span><\/p>\n<p><b>Atmospheric records from the Taylor Glacier ablation zone.<\/b><span style=\"font-weight: 400\">\u00a0With collaborators at University of Rochester and Scripps Institution of Oceanography we are mapping ancient ice outcrops on Taylor Glacier in Antarctica, and using large samples taken from the glacier near surface for high precision measurements of gases and their isotopic composition.\u00a0\u00a0Recent work reconstructs the\u00a0<\/span><span style=\"font-weight: 400\">\u03b4<\/span><span style=\"font-weight: 400\">13<\/span><span style=\"font-weight: 400\">C of atmospheric CO<\/span><span style=\"font-weight: 400\">2<\/span><span style=\"font-weight: 400\">\u00a0(<\/span><a href=\"http:\/\/www.pnas.org\/content\/early\/2016\/03\/08\/1513868113.abstract\"><span style=\"font-weight: 400\">Bauska et al., 2016<\/span><\/a><span style=\"font-weight: 400\">) and the isotopic composition of N<\/span><span style=\"font-weight: 400\">2<\/span><span style=\"font-weight: 400\">O (<\/span><a href=\"http:\/\/www.nature.com\/nature\/journal\/v516\/n7530\/abs\/nature13971.html\"><span style=\"font-weight: 400\">Schilt et al., 2014<\/span><\/a><span style=\"font-weight: 400\">) during the last deglaciation. \u00a0We are now during our attention to older time periods in this record. \u00a0<\/span><\/p>\n<p><b>Greenhouse gas dynamics during the last ice age from the\u00a0<\/b><a href=\"http:\/\/www.waisdivide.unh.edu\/\"><b>WAIS Divide Ice Core<\/b><\/a><b>.<\/b><span style=\"font-weight: 400\">\u00a0\u00a0We are using the very high resolution WAIS Divide ice core to investigate the fine details of abrupt changes in atmospheric CO<\/span><span style=\"font-weight: 400\">2<\/span><span style=\"font-weight: 400\">\u00a0(<\/span><a href=\"http:\/\/www.nature.com\/nature\/journal\/v514\/n7524\/full\/nature13799.html\"><span style=\"font-weight: 400\">Marcott et al., 2014<\/span><\/a><span style=\"font-weight: 400\">) and CH<\/span><span style=\"font-weight: 400\">4<\/span><span style=\"font-weight: 400\"> (<\/span><a href=\"http:\/\/science.sciencemag.org\/content\/348\/6238\/1016\"><span style=\"font-weight: 400\">Rhodes et al., 2015<\/span><\/a><span style=\"font-weight: 400\">).\u00a0\u00a0New work using stable isotopes in CH4 and CO2, and the interpolar gradient in CH<\/span><span style=\"font-weight: 400\">4<\/span><span style=\"font-weight: 400\">, will take this work further. <\/span><\/p>\n<p><b>Ice core chronology and the bi-polar see saw.\u00a0<\/b><span style=\"font-weight: 400\">\u00a0Gas records, particularly methane concentration records, provide a way to synchronize ice core records and precisely compare climate data from different locations.\u00a0\u00a0Applications include detailed constraints on the timing of the bipolar see saw (<\/span><a href=\"http:\/\/www.nature.com\/nature\/journal\/v520\/n7549\/abs\/nature14401.html\"><span style=\"font-weight: 400\">WAIS Community, 2015<\/span><\/a><span style=\"font-weight: 400\">) and dating the new\u00a0<\/span><a href=\"http:\/\/www.rice.aq\/\"><span style=\"font-weight: 400\">RICE<\/span><\/a><span style=\"font-weight: 400\">\u00a0ice core from Roosevelt Island in Antarctica.<\/span><\/p>\n<p><b>Continuous gas measurements in ice cores.<\/b><span style=\"font-weight: 400\">\u00a0\u00a0We are using laser spectroscopy and continuous melter systems to measure gases continuously (<\/span><a href=\"http:\/\/www.sciencedirect.com\/science\/article\/pii\/S0012821X13001088\"><span style=\"font-weight: 400\">Rhodes et al., 2013<\/span><\/a><span style=\"font-weight: 400\">; 2015), with applications in the above work and in detailed studies of trace gas anomalies in ice cores (Rhodes et al., 2016; 2017).\u00a0\u00a0We now deploy these systems in the field for rapid analysis and stratigraphic mapping on ablation zones. \u00a0Future work could develop isotopic analysis and other aspects of gas records. \u00a0<\/span><\/p>\n<p><b>Studies of 1 Ma old ice from Alan Hills, Antarctica.\u00a0\u00a0<\/b><span style=\"font-weight: 400\">In a project led by colleagues from Princeton and University of Maine we are making the oldest direct greenhouse gas measurements known, in isolated pockets of 1 Ma ice in Antarctica (<\/span><a href=\"http:\/\/www.pnas.org\/content\/112\/22\/6887.full\"><span style=\"font-weight: 400\">Higgins et al, 2015<\/span><\/a><span style=\"font-weight: 400\">).\u00a0\u00a0New ice samples will provide more, and older material for this work.<\/span><\/p>\n<p><b>Stable isotope research. \u00a0<\/b><span style=\"font-weight: 400\">We developed high precision carbon isotope measurements for atmospheric CO2 in ice (<\/span><a href=\"http:\/\/www.atmos-meas-tech.net\/7\/3825\/2014\/\"><span style=\"font-weight: 400\">Bauska et al., 2014<\/span><\/a><span style=\"font-weight: 400\">), isotopic measurements of N<\/span><span style=\"font-weight: 400\">2<\/span><span style=\"font-weight: 400\">O (<\/span><a href=\"http:\/\/www.nature.com\/nature\/journal\/v516\/n7530\/abs\/nature13971.html\"><span style=\"font-weight: 400\">Schilt et al., 2014<\/span><\/a><span style=\"font-weight: 400\">) and are now starting to develop methane isotopic measurements and site specific isotope measurements in N<\/span><span style=\"font-weight: 400\">2<\/span><span style=\"font-weight: 400\">O. \u00a0Expanding the scope of these measurements to the penultimate interglacial and older time periods is a major goal. <\/span><\/p>\n<p><b>Other work:<\/b><span style=\"font-weight: 400\"> We continue exploring the mysteries of total air content in ice cores, and occasionally work on extraterrestrial dust in ice (<\/span><a href=\"http:\/\/www.sciencedirect.com\/science\/article\/pii\/S0012821X09004397\"><span style=\"font-weight: 400\">Brook et al., 2009<\/span><\/a><span style=\"font-weight: 400\">) and cosmogenic isotopes in rocks.<\/span><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Most of our research investigates the interlinked history of greenhouse gases and climate, and related topics like ice core dating, method development, and various other things. Current projects include: Holocene carbon dioxide and nitrous oxide dynamics from the South Pole Ice Core (SPICE).\u00a0\u00a0We are using carbon, nitrogen, and oxygen isotopes to try to understand why &hellip; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/dev.blogs.oregonstate.edu\/icecores\/researchprojects\/\" class=\"more-link\">Continue reading<span class=\"screen-reader-text\"> &#8220;Research Projects&#8221;<\/span><\/a><\/p>\n","protected":false},"author":8676,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"open","template":"","meta":{"footnotes":""},"class_list":["post-2","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/dev.blogs.oregonstate.edu\/icecores\/wp-json\/wp\/v2\/pages\/2","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/dev.blogs.oregonstate.edu\/icecores\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/dev.blogs.oregonstate.edu\/icecores\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/dev.blogs.oregonstate.edu\/icecores\/wp-json\/wp\/v2\/users\/8676"}],"replies":[{"embeddable":true,"href":"https:\/\/dev.blogs.oregonstate.edu\/icecores\/wp-json\/wp\/v2\/comments?post=2"}],"version-history":[{"count":5,"href":"https:\/\/dev.blogs.oregonstate.edu\/icecores\/wp-json\/wp\/v2\/pages\/2\/revisions"}],"predecessor-version":[{"id":119,"href":"https:\/\/dev.blogs.oregonstate.edu\/icecores\/wp-json\/wp\/v2\/pages\/2\/revisions\/119"}],"wp:attachment":[{"href":"https:\/\/dev.blogs.oregonstate.edu\/icecores\/wp-json\/wp\/v2\/media?parent=2"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}