{"id":42574,"date":"2025-07-10T14:27:09","date_gmt":"2025-07-10T19:27:09","guid":{"rendered":"https:\/\/huewhite.com\/umb\/?p=42574"},"modified":"2025-07-10T14:27:09","modified_gmt":"2025-07-10T19:27:09","slug":"word-of-the-day-1049","status":"publish","type":"post","link":"https:\/\/huewhite.com\/umb\/2025\/07\/10\/word-of-the-day-1049\/","title":{"rendered":"Word Of The Day"},"content":{"rendered":"<p><em>Synoptic scale meteorology<\/em>:<\/p>\n<blockquote><p>In\u00a0<a title=\"Meteorology\" href=\"https:\/\/en.wikipedia.org\/wiki\/Meteorology\">meteorology<\/a>, the\u00a0<b>synoptic scale<\/b>\u00a0(also called the\u00a0<b>large scale<\/b>\u00a0or\u00a0<b>cyclonic scale<\/b>) is a\u00a0<a title=\"Horizontal position representation\" href=\"https:\/\/en.wikipedia.org\/wiki\/Horizontal_position_representation\">horizontal<\/a>\u00a0<a title=\"Length scale\" href=\"https:\/\/en.wikipedia.org\/wiki\/Length_scale\">length scale<\/a>\u00a0of the\u00a0<a title=\"Orders of magnitude (length)\" href=\"https:\/\/en.wikipedia.org\/wiki\/Orders_of_magnitude_(length)\">order<\/a>\u00a0of 1,000\u00a0km (620\u00a0mi) or more.<sup id=\"cite_ref-1\" class=\"reference\"><a href=\"https:\/\/en.wikipedia.org\/wiki\/Synoptic_scale_meteorology#cite_note-1\"><span class=\"cite-bracket\">[<\/span>1<span class=\"cite-bracket\">]<\/span><\/a><\/sup>\u00a0This corresponds to a horizontal scale typical of\u00a0<a title=\"Middle latitudes\" href=\"https:\/\/en.wikipedia.org\/wiki\/Middle_latitudes\">mid-latitude<\/a>\u00a0<a class=\"mw-redirect\" title=\"Depression (meteorology)\" href=\"https:\/\/en.wikipedia.org\/wiki\/Depression_(meteorology)\">depressions<\/a>\u00a0(e.g.\u00a0<a title=\"Extratropical cyclone\" href=\"https:\/\/en.wikipedia.org\/wiki\/Extratropical_cyclone\">extratropical cyclones<\/a>). Most\u00a0<a title=\"High-pressure area\" href=\"https:\/\/en.wikipedia.org\/wiki\/High-pressure_area\">high-<\/a>\u00a0and\u00a0<a title=\"Low-pressure area\" href=\"https:\/\/en.wikipedia.org\/wiki\/Low-pressure_area\">low-pressure areas<\/a>\u00a0seen on\u00a0<a title=\"Weather map\" href=\"https:\/\/en.wikipedia.org\/wiki\/Weather_map\">weather maps<\/a>\u00a0(such as\u00a0<a title=\"Surface weather analysis\" href=\"https:\/\/en.wikipedia.org\/wiki\/Surface_weather_analysis\">surface weather analyses<\/a>) are synoptic-scale systems, driven by the location of\u00a0<a title=\"Rossby wave\" href=\"https:\/\/en.wikipedia.org\/wiki\/Rossby_wave\">Rossby waves<\/a>\u00a0in their respective hemisphere. Low-pressure areas and their related frontal zones occur on the leading edge of a trough within the Rossby wave pattern, while\u00a0<a title=\"High-pressure area\" href=\"https:\/\/en.wikipedia.org\/wiki\/High-pressure_area\">high-pressure areas<\/a>\u00a0form on the back edge of the trough. Most\u00a0<a title=\"Precipitation\" href=\"https:\/\/en.wikipedia.org\/wiki\/Precipitation\">precipitation<\/a>\u00a0areas occur near frontal zones. The word\u00a0<i><a class=\"extiw\" title=\"wikt:synoptic\" href=\"https:\/\/en.wiktionary.org\/wiki\/synoptic\">synoptic<\/a><\/i>\u00a0is derived from the\u00a0<a title=\"Ancient Greek\" href=\"https:\/\/en.wikipedia.org\/wiki\/Ancient_Greek\">Ancient Greek<\/a>\u00a0word\u00a0<span lang=\"grc\"><a class=\"extiw\" title=\"wikt:\u03c3\u03c5\u03bd\u03bf\u03c0\u03c4\u03b9\u03ba\u03cc\u03c2\" href=\"https:\/\/en.wiktionary.org\/wiki\/%CF%83%CF%85%CE%BD%CE%BF%CF%80%CF%84%CE%B9%CE%BA%CF%8C%CF%82#Ancient_Greek\">\u03c3\u03c5\u03bd\u03bf\u03c0\u03c4\u03b9\u03ba\u03cc\u03c2<\/a><\/span>\u00a0(<span lang=\"grc-Latn\" title=\"Ancient Greek transliteration\"><i>sunoptik\u00f3s<\/i><\/span>), meaning &#8220;seen together&#8221;.<em> [<a href=\"https:\/\/en.wikipedia.org\/wiki\/Synoptic_scale_meteorology\" target=\"_blank\" rel=\"noopener\"><strong>Wikipedia<\/strong><\/a>]<\/em><\/p><\/blockquote>\n<p><a href=\"https:\/\/www.youtube.com\/c\/RyanHallYall\" target=\"_blank\" rel=\"noopener\">Ryan Hall<\/a>, an Internet weather analyst and owner of a lovely voice, uses <em>synoptic<\/em> frequently in his discussions of weather forecasts, such as this one here.<\/p>\n<p><iframe loading=\"lazy\" title=\"These Storms Will Cause Days Of Problems...\" width=\"800\" height=\"450\" src=\"https:\/\/www.youtube.com\/embed\/xVDUnIjcPRU?feature=oembed\" frameborder=\"0\" allow=\"accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture; web-share\" referrerpolicy=\"strict-origin-when-cross-origin\" allowfullscreen><\/iframe><\/p>\n<p>I&#8217;ll leave it to the reader to actually find it. Yes, I do assume his <em>synoptic <\/em>is <em>Synoptic scale meteorology<\/em>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Synoptic scale meteorology: In\u00a0meteorology, the\u00a0synoptic scale\u00a0(also called the\u00a0large scale\u00a0or\u00a0cyclonic scale) is a\u00a0horizontal\u00a0length scale\u00a0of the\u00a0order\u00a0of 1,000\u00a0km (620\u00a0mi) or more.[1]\u00a0This corresponds to a horizontal scale typical of\u00a0mid-latitude\u00a0depressions\u00a0(e.g.\u00a0extratropical cyclones). Most\u00a0high-\u00a0and\u00a0low-pressure areas\u00a0seen on\u00a0weather maps\u00a0(such as\u00a0surface weather analyses) are synoptic-scale systems, driven by the location of\u00a0Rossby waves\u00a0in their respective hemisphere. Low-pressure areas and their related \u2026 <a class=\"continue-reading-link\" href=\"https:\/\/huewhite.com\/umb\/2025\/07\/10\/word-of-the-day-1049\/\"> Continue reading <span class=\"meta-nav\">&rarr; <\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"nf_dc_page":"","_jetpack_memberships_contains_paid_content":false,"footnotes":""},"categories":[1],"tags":[],"class_list":["post-42574","post","type-post","status-publish","format-standard","hentry","category-uncategorized"],"jetpack_featured_media_url":"","jetpack_sharing_enabled":true,"_links":{"self":[{"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/posts\/42574","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/comments?post=42574"}],"version-history":[{"count":1,"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/posts\/42574\/revisions"}],"predecessor-version":[{"id":42575,"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/posts\/42574\/revisions\/42575"}],"wp:attachment":[{"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/media?parent=42574"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/categories?post=42574"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/huewhite.com\/umb\/wp-json\/wp\/v2\/tags?post=42574"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}