{"id":590,"date":"2013-11-16T18:59:48","date_gmt":"2013-11-16T18:59:48","guid":{"rendered":"http:\/\/www.atmos.washington.edu\/~thornton"},"modified":"2014-01-08T16:57:17","modified_gmt":"2014-01-08T16:57:17","slug":"soas-centerville-2013","status":"publish","type":"page","link":"https:\/\/www.atmos.washington.edu\/~thornton\/field-campaigns\/soas-centerville-2013","title":{"rendered":"SOAS Centerville 2013"},"content":{"rendered":"<p>While part of our group and our instrumentation was flying aboard the NOAA WP-3D aircraft in the Southeastern U.S. during <a href=\"http:\/\/www.atmos.washington.edu\/~thornton\/field-campaigns\/senex-2013\"> SENEX<\/a>, we simultaneously deployed a HR-ToF-CIMS at the ground site in Centerville, Alabama, as part of the Southern Oxidant and Aerosol Study <a href=\"http:\/\/soas2013.rutgers.edu\/\"> (SOAS<\/a>). Similar and complementary to the aircraft measurements, the six-week ground-based field campaign during the summer of 2013 focused on the study of biosphere-atmosphere and biogenic\u2010anthropogenic interactions to address the question of the cooling trend in this region.<\/p>\n<figure id=\"attachment_726\" aria-describedby=\"caption-attachment-726\" style=\"width: 276px\" class=\"wp-caption alignleft\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-726\" title=\"2013-06-25 14.50.18\" src=\"http:\/\/www.atmos.washington.edu\/~thornton\/wordpress\/wp-content\/uploads\/2013-06-25-14.50.184-300x225.jpg\" alt=\"\" width=\"276\" height=\"205\" \/><figcaption id=\"caption-attachment-726\" class=\"wp-caption-text\">SOAS ground site in Centerville, Alabama<\/figcaption><\/figure>\n<figure id=\"attachment_727\" aria-describedby=\"caption-attachment-727\" style=\"width: 277px\" class=\"wp-caption alignleft\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-727\" title=\"1012196_10151767335067491_5431097_n\" src=\"http:\/\/www.atmos.washington.edu\/~thornton\/wordpress\/wp-content\/uploads\/1012196_10151767335067491_5431097_n1-300x225.jpg\" alt=\"\" width=\"277\" height=\"206\" \/><figcaption id=\"caption-attachment-727\" class=\"wp-caption-text\">A thunderstorm is bulding up<\/figcaption><\/figure>\n<figure id=\"attachment_728\" aria-describedby=\"caption-attachment-728\" style=\"width: 274px\" class=\"wp-caption alignleft\"><img loading=\"lazy\" decoding=\"async\" class=\"size-medium wp-image-728 \" title=\"2013-06-29 17.35.04\" src=\"http:\/\/www.atmos.washington.edu\/~thornton\/wordpress\/wp-content\/uploads\/2013-06-29-17.35.04-300x225.jpg\" alt=\"\" width=\"274\" height=\"207\" srcset=\"https:\/\/www.atmos.washington.edu\/~thornton\/wordpress\/wp-content\/uploads\/2013-06-29-17.35.04-300x225.jpg 300w, https:\/\/www.atmos.washington.edu\/~thornton\/wordpress\/wp-content\/uploads\/2013-06-29-17.35.04-1024x768.jpg 1024w\" sizes=\"auto, (max-width: 274px) 100vw, 274px\" \/><figcaption id=\"caption-attachment-728\" class=\"wp-caption-text\">The FIGAERO-HRToF-CIMS during SOAS<\/figcaption><\/figure>\n<p>We investigated chemical compounds in both the gas and particle phases with our newly developed FIGAERO (Filter Inlet for Gases and Aerosols, <a href=\"http:\/\/www.atmos-meas-tech-discuss.net\/6\/9347\/2013\/amtd-6-9347-2013.html\"> <em>Lopez-Hilfiker et al.<\/em><\/a>).  Close to six weeks of continuous data with a time resolution of ~2 hrs  of both gas and particle phase components will give us new insights into  oxidation processes of biogenic and anthropogenic volatile organic  compounds and subsequent particle formation.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>While part of our group and our instrumentation was flying aboard the NOAA WP-3D aircraft in the Southeastern U.S. during SENEX, we simultaneously deployed a HR-ToF-CIMS at the ground site in Centerville, Alabama, as part of the Southern Oxidant and Aerosol Study (SOAS). Similar and complementary to the aircraft measurements, the six-week ground-based field campaign during the summer of 2013 focused on the study of biosphere-atmosphere and biogenic\u2010anthropogenic interactions to address the question of the cooling trend in this region. We investigated chemical compounds in both the gas and particle <\/p>\n","protected":false},"author":1,"featured_media":0,"parent":37,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-590","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/pages\/590","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/comments?post=590"}],"version-history":[{"count":8,"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/pages\/590\/revisions"}],"predecessor-version":[{"id":755,"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/pages\/590\/revisions\/755"}],"up":[{"embeddable":true,"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/pages\/37"}],"wp:attachment":[{"href":"https:\/\/www.atmos.washington.edu\/~thornton\/wp-json\/wp\/v2\/media?parent=590"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}