{"id":2551,"date":"2016-05-30T12:51:45","date_gmt":"2016-05-30T18:51:45","guid":{"rendered":"https:\/\/www.coloradofloodthreat.com\/?p=2551"},"modified":"2016-05-30T12:52:23","modified_gmt":"2016-05-30T18:52:23","slug":"fto-05-30-2016-elevated-flood-threat-tuesday-followed-by-prolonged-warm-and-dry-period","status":"publish","type":"post","link":"https:\/\/archive-coftb.dewberryanalytics.com\/?p=2551","title":{"rendered":"FTO 05-30-2016: Elevated Flood Threat Tuesday, Followed By Prolonged Warm and Dry Period"},"content":{"rendered":"<p>Issue Date: Monday, May 30th, 2016<br>\nIssue Time: 12:45PM MDT<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2016\/05\/threat_timeline.png\"><img loading=\"lazy\" class=\"aligncenter  wp-image-2553\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2016\/05\/threat_timeline.png\" alt=\"threat_timeline\" width=\"872\" height=\"111\"\/><\/a><\/p>\n<p>May has been a cool month for most of Colorado (see our Storm Total Precipitation discussion for 5\/30\/2016). As the water vapor image shows, below, an amplified pattern with at least two distinct ridge-<span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;trough&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;An elongated area of relatively low atmospheric pressure; the opposite of a ridge.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>trough<\/span> couplets is seen across the vast North Pacific Ocean. At face value, this may seem to suggest that unsettled weather will continue as these features move east in the <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;jet stream&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Relatively strong winds concentrated within a narrow stream in the atmosphere. General weather patterns are related closely to the position, strength and orientation of the jet stream.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>jet stream<\/span>&rsquo;s steering winds. But given that we are about to enter the first week of June, this is never guaranteed! Indeed, it appears that after tomorrow&rsquo;s passage of a large-scale <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;trough&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;An elongated area of relatively low atmospheric pressure; the opposite of a ridge.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>trough<\/span> (Event #1) that will deliver <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;widespread&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;greater than 60% areal coverage&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>widespread<\/span> showers and thunderstorms, the overall pattern will calm down significantly.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2016\/05\/watervapor_20160530.png\"><img loading=\"lazy\" class=\"aligncenter  wp-image-2555\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2016\/05\/watervapor_20160530.png\" alt=\"watervapor_20160530\" width=\"646\" height=\"459\"\/><\/a><\/p>\n<p>The reason for a calmer pattern will be the development of a stout early summer ridge that is currently in its infancy off the southwest US coast. The map below shows the GFS ensembles&rsquo; depiction of the upper atmosphere&rsquo;s pattern for next Sunday 6\/5. Note that by this time, there is essentially unanimous support for a ridge that covers the entire western United States. The implications of this are a prolonged warm and mainly dry period for Colorado starting mid-week last through at least mid-week next week. This does not imply that rainfall will not be found, but simply that it will be generally light and likely favoring high-elevation locations in accordance with Colorado&rsquo;s summer climatology.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2016\/05\/gfs_500mb.png\"><img loading=\"lazy\" class=\"aligncenter  wp-image-2554\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2016\/05\/gfs_500mb.png\" alt=\"gfs_500mb\" width=\"637\" height=\"467\"\/><\/a><\/p>\n<p>Thereafter, guidance is no longer as consistent, with some suggestions of the ridge quickly breaking down and storminess returning east of the <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;Divide&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;!-- wp:paragraph {&amp;quot;textColor&amp;quot;:&amp;quot;white&amp;quot;} --&amp;gt;\n&amp;lt;p class=&amp;quot;has-white-color has-text-color&amp;quot;&amp;gt;the dividing line that separates the watersheds of the western and eastern United States; rivers west of the divide empty into the Pacific Ocean, while rivers east of the divide empty into the Atlantic Ocean or Gulf of Mexico&amp;lt;\/p&amp;gt;\n&amp;lt;!-- \/wp:paragraph --&amp;gt;&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>Divide<\/span>. There is enough loose consensus for us to bring in Event #2 starting late next week. However, there is not enough consensus to be able to estimate rainfall amounts, yet.<\/p>\n<h3><strong>Event #1: Tuesday, May 31<sup>st<\/sup><\/strong><\/h3>\n<p><em><strong><span style=\"color: #ff6600;\">Elevated<\/span><\/strong> Flood Threat for Southeast Colorado<br><\/em><\/p>\n<p>A <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;cut-off low&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;!-- wp:paragraph {&amp;quot;textColor&amp;quot;:&amp;quot;white&amp;quot;} --&amp;gt;\n&amp;lt;p class=&amp;quot;has-white-color has-text-color&amp;quot;&amp;gt;an upper-level low pressure system that has been &amp;quot;cut off&rdquo; from the prevailing winds that steer weather systems; cut-off lows typically become stationary or move very slowly, bringing prolonged periods of unsettled weather&amp;lt;\/p&amp;gt;\n&amp;lt;!-- \/wp:paragraph --&amp;gt;&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>cut-off low<\/span> will propagate eastward, providing favorable dynamics for a <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;widespread&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;greater than 60% areal coverage&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>widespread<\/span> rain event for the Palmer Ridge, Southeast Mountains, Raton Ridge, Southeast Plains and parts of the Urban Corridor. A cool front passage will limit instability the farther north one goes, thus lighter rainfall rates will result north of Colorado Springs. In areas to the south, rainfall amounts up to 2 inches will be possible as at least one round of thunderstorms moves through the area during the afternoon and evening hours. An elevated flood threat is warranted for this region. Check out tomorrow&rsquo;s Flood Threat Bulletin for the most up-to-date discussion and rainfall estimates.<\/p>\n<p><iframe loading=\"lazy\" src=\"https:\/\/a.tiles.mapbox.com\/v4\/sgeiger.0959edoj\/attribution,zoompan,zoomwheel,geocoder,share.html?access_token=pk.eyJ1Ijoic2dlaWdlciIsImEiOiJmNjc5a3RBIn0.LbLupVkJsS5dbo9fsgrTDg\" width=\"100%\" height=\"500px\" frameborder=\"0\"><\/iframe><br><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2015\/05\/Legend.png\"><img loading=\"lazy\" class=\"alignnone size-full wp-image-230\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2015\/05\/Legend.png\" alt=\"Legend\" width=\"94\" height=\"158\"\/><\/a><\/p>\n<h3><strong>Event #2: Saturday, June 11<sup>th<\/sup> through Monday, June 13<sup>th<\/sup><\/strong><\/h3>\n<p><em><strong><span style=\"color: #0000ff;\">No Apparent<\/span><\/strong> <span style=\"color: #0000ff;\">Flood Threat<\/span> as timing of ridge weakening is uncertain<\/em><\/p>\n<p>After a prolonged warm and mainly dry period, there are indications that the upper-level ridge will break down. This will open up the door for northwest flow and disturbances that could generate heavy rainfall mainly east of the <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;Continental Divide&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;&amp;lt;!-- wp:paragraph {&amp;quot;textColor&amp;quot;:&amp;quot;white&amp;quot;} --&amp;gt;\n&amp;lt;p class=&amp;quot;has-white-color has-text-color&amp;quot;&amp;gt;the dividing line that separates the watersheds of the western and eastern United States; rivers west of the divide empty into the Pacific Ocean, while rivers east of the divide empty into the Atlantic Ocean or Gulf of Mexico&amp;lt;\/p&amp;gt;\n&amp;lt;!-- \/wp:paragraph --&amp;gt;&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>Continental Divide<\/span>. At this time, there is not enough guidance to pinpoint rainfall amounts. However, climatologically speaking, the northeast part of the state, including the Front Range and Urban Corridor, is the most likely target for the threat.<\/p>","protected":false},"excerpt":{"rendered":"<p>Issue Date: Monday, May 30th, 2016 Issue Time: 12:45PM MDT May has been a cool month for most of Colorado (see our Storm Total Precipitation discussion for 5\/30\/2016). As the water vapor image shows, below, an amplified pattern with at least two distinct ridge-<span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;trough&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;An elongated area of relatively low atmospheric pressure; the opposite of a ridge.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>trough<\/span> couplets is seen across the vast North Pacific Ocean. At face [&hellip;]<\/p>","protected":false},"author":4,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":[],"categories":[3],"tags":[],"post_mailing_queue_ids":[],"_links":{"self":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/2551"}],"collection":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/users\/4"}],"replies":[{"embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=2551"}],"version-history":[{"count":2,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/2551\/revisions"}],"predecessor-version":[{"id":2557,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/2551\/revisions\/2557"}],"wp:attachment":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=2551"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=2551"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=2551"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}