{"id":3018,"date":"2019-10-01T17:42:42","date_gmt":"2019-10-01T17:42:42","guid":{"rendered":"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/10\/ContourPlots.png"},"modified":"2019-10-01T17:43:22","modified_gmt":"2019-10-01T17:43:22","slug":"contourplots","status":"inherit","type":"attachment","link":"https:\/\/blogs.oregonstate.edu\/gemmlab\/2019\/10\/01\/surveying-for-marine-mammals-in-the-northern-california-current\/contourplots\/","title":{"rendered":"ContourPlots"},"author":8072,"featured_media":0,"comment_status":"open","ping_status":"closed","template":"","meta":[],"class_list":["post-3018","attachment","type-attachment","status-inherit","hentry"],"jetpack_sharing_enabled":true,"description":{"rendered":"<p class=\"attachment\"><a href='https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/10\/ContourPlots.png'><img loading=\"lazy\" decoding=\"async\" width=\"300\" height=\"70\" src=\"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/10\/ContourPlots-300x70.png\" class=\"attachment-medium size-medium\" alt=\"\" srcset=\"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/10\/ContourPlots-300x70.png 300w, https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/10\/ContourPlots-768x180.png 768w, https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/10\/ContourPlots-1024x239.png 1024w, https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/10\/ContourPlots.png 1608w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><\/p>\n"},"caption":{"rendered":"<p>Figure 4. Temperature contours over the upper 150 m from 1-200 miles off Newport, Oregon from Fall 2014-2019. During Fall 2014, the Warm Blob inundated the Oregon shelf. Surface temperatures during that survey were 17\u00b0- 18\u00b0C along the entire transect. During 2015 and 2016 the warm water (16\u00b0C) layer had deepened and occupied the upper 50 m. During 2018, the temperature was 16\u00b0C in the upper 20 m and cooler on the shelf, indicative of residual upwelling. During this survey in 2019, we again saw very warm (18\u00b0C) temperatures in the upper water column over the entire transect. Image and caption credit: Jennifer Fisher. <\/p>\n"},"alt_text":"","media_type":"image","mime_type":"image\/png","media_details":{"width":1608,"height":376,"file":"2019\/10\/ContourPlots.png","sizes":{"thumbnail":{"file":"ContourPlots-150x150.png","width":150,"height":150,"mime_type":"image\/png","source_url":"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/10\/ContourPlots-150x150.png"},"medium":{"file":"ContourPlots-300x70.png","width":300,"height":70,"mime_type":"image\/png","source_url":"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/10\/ContourPlots-300x70.png"},"medium_large":{"file":"ContourPlots-768x180.png","width":768,"height":180,"mime_type":"image\/png","source_url":"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/10\/ContourPlots-768x180.png"},"large":{"file":"ContourPlots-1024x239.png","width":1024,"height":239,"mime_type":"image\/png","source_url":"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/10\/ContourPlots-1024x239.png"},"post-thumbnail":{"file":"ContourPlots-825x376.png","width":825,"height":376,"mime_type":"image\/png","source_url":"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/10\/ContourPlots-825x376.png"},"full":{"file":"ContourPlots.png","width":1608,"height":376,"mime_type":"image\/png","source_url":"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/10\/ContourPlots.png"}},"image_meta":{"aperture":"0","credit":"","camera":"","caption":"","created_timestamp":"0","copyright":"","focal_length":"0","iso":"0","shutter_speed":"0","title":"","orientation":"0","keywords":[]}},"post":3010,"source_url":"https:\/\/osu-wams-blogs-uploads.s3.amazonaws.com\/blogs.dir\/2115\/files\/2019\/10\/ContourPlots.png","_links":{"self":[{"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/media\/3018","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/media"}],"about":[{"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/types\/attachment"}],"author":[{"embeddable":true,"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/users\/8072"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/comments?post=3018"}],"wp:attached-to":[{"embeddable":true,"post_type":"post","id":3010,"href":"https:\/\/blogs.oregonstate.edu\/gemmlab\/wp-json\/wp\/v2\/posts\/3010"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}