{"id":46337,"date":"2022-05-11T23:55:00","date_gmt":"2022-05-11T23:55:00","guid":{"rendered":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/?p=46337"},"modified":"2022-05-13T21:01:30","modified_gmt":"2022-05-13T21:01:30","slug":"stereoscopic-views-of-convection-using-goes-16-and-goes-18-visible-data","status":"publish","type":"post","link":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/archives\/46337","title":{"rendered":"Stereoscopic views of convection using GOES-16 and GOES-18 visible data"},"content":{"rendered":"\n<figure class=\"wp-block-video\"><video height=\"960\" style=\"aspect-ratio: 2880 \/ 960;\" width=\"2880\" controls loop src=\"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-content\/uploads\/sites\/5\/2022\/05\/GOES-18R_GOES-16L_ABI_RadM1_C02_2022131_1920_to_2349anim.mp4\"><\/video><figcaption>GOES-16 and GOES-18 imagery, 1920 &#8211; 2350 UTC on 11 May 2022<\/figcaption><\/figure>\n\n\n\n<p>GOES-18 data in this post are preliminary and non-operational and beautiful.  Because GOES-18 and GOES-16 nadir positions are separated by almost 15<sup>o<\/sup> of longitude (89.5<sup>o<\/sup> and 75.2<sup>o<\/sup>, respectively), they can be used (when remapped to the same projection, in this case using a beta version of <a href=\"http:\/\/cimss.ssec.wisc.edu\/csppgeo\/geo2grid_v1.0.0.html\">geo2grid<\/a> that supports GOES-18 imagery) to create pseudo-stereoscopic imagery.  That is, if you cross your eyes when looking at the imagery, and focus on the image that appears in the middle of the two other images, a three-dimensional image can be viewed (Note:  Not all human brains can do this).  The image above shows convection on 11 May 2022 over Nebraska between 1920 and 2350 UTC.  <\/p>\n\n\n\n<p>Thanks to Tim Schmit, NOAA\/ASPB, for supplying me with these images!<\/p>\n","protected":false},"excerpt":{"rendered":"<p>GOES-18 data in this post are preliminary and non-operational and beautiful. Because GOES-18 and GOES-16 nadir positions are separated by almost 15o of longitude (89.5o and 75.2o, respectively), they can be used (when remapped to the same projection, in this case using a beta version of geo2grid that supports GOES-18 imagery) to create pseudo-stereoscopic imagery. [&hellip;]<\/p>\n","protected":false},"author":19,"featured_media":46340,"comment_status":"closed","ping_status":"","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[74,114,3],"tags":[],"class_list":["post-46337","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-goes-16","category-goes-18","category-severe-convection"],"acf":[],"_links":{"self":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/46337","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/users\/19"}],"replies":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/comments?post=46337"}],"version-history":[{"count":5,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/46337\/revisions"}],"predecessor-version":[{"id":46345,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/posts\/46337\/revisions\/46345"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media\/46340"}],"wp:attachment":[{"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/media?parent=46337"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/categories?post=46337"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/cimss.ssec.wisc.edu\/satellite-blog\/wp-json\/wp\/v2\/tags?post=46337"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}