{"id":1483,"date":"2017-03-03T15:56:13","date_gmt":"2017-03-03T22:56:13","guid":{"rendered":"http:\/\/rammb.cira.colostate.edu\/training\/visit\/blog\/?p=1483"},"modified":"2026-03-06T09:06:28","modified_gmt":"2026-03-06T16:06:28","slug":"comparison-of-goes-16-with-goes-13","status":"publish","type":"post","link":"https:\/\/rammb2.cira.colostate.edu\/visit-blog\/2017\/03\/03\/comparison-of-goes-16-with-goes-13\/","title":{"rendered":"Comparison of GOES-16 with GOES-13"},"content":{"rendered":"<p><strong>The GOES-16 data posted on this page are preliminary, non-operational data and are undergoing testing. \u00a0Users bear all responsibility for inspecting the data prior to use and for the manner in which the data are utilized.<\/strong><\/p>\n<p>One of the 1-minute mesoscale sectors for GOES-16 \u00a0captured a series of polar low-like circulations over northeastern Lake Ontario moving into New York:<\/p>\n<p><a href=\"http:\/\/rammb.cira.colostate.edu\/templates\/loop_directory.asp?data_folder=training\/visit\/loops\/3mar17\/B02&amp;loop_speed_ms=80\" target=\"_blank\" rel=\"noopener\">http:\/\/rammb.cira.colostate.edu\/templates\/loop_directory.asp?data_folder=training\/visit\/loops\/3mar17\/B02&amp;loop_speed_ms=80<\/a><\/p>\n<p>Notice how much more clearly these circulations appear in GOES-16 as compared to current GOES-13:<\/p>\n<p><a href=\"http:\/\/rammb.cira.colostate.edu\/templates\/loop_directory.asp?data_folder=training\/visit\/loops\/3mar17\/GOES13\" target=\"_blank\" rel=\"noopener\">http:\/\/rammb.cira.colostate.edu\/templates\/loop_directory.asp?data_folder=training\/visit\/loops\/3mar17\/GOES13<\/a><\/p>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>The GOES-16 data posted on this page are preliminary, non-operational data and are undergoing testing. \u00a0Users bear all responsibility for inspecting the data prior to use and for the manner in which the data are utilized. One of the 1-minute mesoscale sectors for GOES-16 \u00a0captured a series of polar low-like circulations over northeastern Lake Ontario <a href=\"https:\/\/rammb2.cira.colostate.edu\/visit-blog\/2017\/03\/03\/comparison-of-goes-16-with-goes-13\/\" class=\"more-link\">Continue Reading<\/a><\/p>\n","protected":false},"author":5,"featured_media":0,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[47,48,28],"tags":[],"class_list":["post-1483","post","type-post","status-publish","format-standard","hentry","category-geostationary-satellite-discussion","category-goes-r","category-satellites"],"_links":{"self":[{"href":"https:\/\/rammb2.cira.colostate.edu\/visit-blog\/wp-json\/wp\/v2\/posts\/1483","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/rammb2.cira.colostate.edu\/visit-blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/rammb2.cira.colostate.edu\/visit-blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/rammb2.cira.colostate.edu\/visit-blog\/wp-json\/wp\/v2\/users\/5"}],"replies":[{"embeddable":true,"href":"https:\/\/rammb2.cira.colostate.edu\/visit-blog\/wp-json\/wp\/v2\/comments?post=1483"}],"version-history":[{"count":1,"href":"https:\/\/rammb2.cira.colostate.edu\/visit-blog\/wp-json\/wp\/v2\/posts\/1483\/revisions"}],"predecessor-version":[{"id":6126,"href":"https:\/\/rammb2.cira.colostate.edu\/visit-blog\/wp-json\/wp\/v2\/posts\/1483\/revisions\/6126"}],"wp:attachment":[{"href":"https:\/\/rammb2.cira.colostate.edu\/visit-blog\/wp-json\/wp\/v2\/media?parent=1483"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/rammb2.cira.colostate.edu\/visit-blog\/wp-json\/wp\/v2\/categories?post=1483"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/rammb2.cira.colostate.edu\/visit-blog\/wp-json\/wp\/v2\/tags?post=1483"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}