{"id":278,"date":"2024-04-05T17:31:52","date_gmt":"2024-04-05T17:31:52","guid":{"rendered":"https:\/\/fs.wp.odu.edu\/gcutter\/?page_id=278"},"modified":"2024-04-10T17:14:19","modified_gmt":"2024-04-10T17:14:19","slug":"ioc-2002","status":"publish","type":"page","link":"https:\/\/fs.wp.odu.edu\/gcutter\/ioc-2002\/","title":{"rendered":"IOC 2002"},"content":{"rendered":"\n<p><\/p>\n\n\n\n<figure class=\"wp-block-image size-large\"><a href=\"https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/IOC-2002_1-scaled.gif\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"579\" src=\"https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/IOC-2002_1-1024x579.gif\" alt=\"\" class=\"wp-image-333\" srcset=\"https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/IOC-2002_1-1024x579.gif 1024w, https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/IOC-2002_1-300x170.gif 300w, https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/IOC-2002_1-768x435.gif 768w, https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/IOC-2002_1-1536x869.gif 1536w, https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/IOC-2002_1-2048x1159.gif 2048w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><\/a><\/figure>\n\n\n\n<p>Departed: Osaka, Japan<\/p>\n\n\n\n<p>Date: 1 May 2002<\/p>\n\n\n\n<p>Arrived: Honolulu, Hawaii,<\/p>\n\n\n\n<p>Date: 5 June 2002<\/p>\n\n\n\n<p>The IOC 2002 Contaminant Baseline Survey in the western Pacific Ocean was the fourth in a series of cruises intended to establish the current concentrations of trace elements and other materials in the major water masses of the ocean and to reveal the pathways of the materials delivered to the surface ocean and how they are incorporated in the subsurface waters. The expedition included nine vertical profile stations in the subtropical and subarctic gyre of the western North Pacific. In addition, underway surface water samples were collected during transits between the stations.<\/p>\n\n\n\n<p>The cruise utilized the United States Research Vessel Melville<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><a href=\"https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/image-8.png\"><img loading=\"lazy\" decoding=\"async\" width=\"950\" height=\"662\" src=\"https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/image-8.png\" alt=\"\" class=\"wp-image-451\" srcset=\"https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/image-8.png 950w, https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/image-8-300x209.png 300w, https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/image-8-768x535.png 768w\" sizes=\"(max-width: 950px) 100vw, 950px\" \/><\/a><\/figure>\n\n\n\n<p><em>Figure 1<\/em> Distribution of temperature and Salinity from underway sensors along the ship&#8217;s track. Discrete salinity samples are shown to indicate agreement with sensor value. Vertical station positions along the cruise trach are shown S1-S9<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><a href=\"https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/image-9.png\"><img loading=\"lazy\" decoding=\"async\" width=\"963\" height=\"557\" src=\"https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/image-9.png\" alt=\"\" class=\"wp-image-453\" srcset=\"https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/image-9.png 963w, https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/image-9-300x174.png 300w, https:\/\/fs.wp.odu.edu\/gcutter\/wp-content\/uploads\/sites\/1996\/2024\/04\/image-9-768x444.png 768w\" sizes=\"(max-width: 963px) 100vw, 963px\" \/><\/a><\/figure>\n\n\n\n<p><em>Figure 2<\/em> Nitrite+Nitrate from the continuous underway sampling system. Data were contoured using Generic Mapping Tools. Contours were computed after fitting a minimum curvature surface with tension to the gridded data<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Departed: Osaka, Japan Date: 1 May 2002 Arrived: Honolulu, Hawaii, Date: 5 June 2002 The&#8230;<\/p>\n<div class=\"more-link-wrapper\"><a class=\"more-link\" href=\"https:\/\/fs.wp.odu.edu\/gcutter\/ioc-2002\/\">Read the post<span class=\"screen-reader-text\">IOC 2002<\/span><\/a><\/div>\n","protected":false},"author":26740,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"_links":{"self":[{"href":"https:\/\/fs.wp.odu.edu\/gcutter\/wp-json\/wp\/v2\/pages\/278"}],"collection":[{"href":"https:\/\/fs.wp.odu.edu\/gcutter\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/fs.wp.odu.edu\/gcutter\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/fs.wp.odu.edu\/gcutter\/wp-json\/wp\/v2\/users\/26740"}],"replies":[{"embeddable":true,"href":"https:\/\/fs.wp.odu.edu\/gcutter\/wp-json\/wp\/v2\/comments?post=278"}],"version-history":[{"count":4,"href":"https:\/\/fs.wp.odu.edu\/gcutter\/wp-json\/wp\/v2\/pages\/278\/revisions"}],"predecessor-version":[{"id":454,"href":"https:\/\/fs.wp.odu.edu\/gcutter\/wp-json\/wp\/v2\/pages\/278\/revisions\/454"}],"wp:attachment":[{"href":"https:\/\/fs.wp.odu.edu\/gcutter\/wp-json\/wp\/v2\/media?parent=278"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}