{"id":3805,"date":"2016-09-12T14:56:53","date_gmt":"2016-09-12T20:56:53","guid":{"rendered":"https:\/\/www.coloradofloodthreat.com\/?p=3805"},"modified":"2016-09-12T14:58:06","modified_gmt":"2016-09-12T20:58:06","slug":"fto-09-12-2016-active-pattern-ahead-as-dynamics-and-moisture-return-to-colorado","status":"publish","type":"post","link":"https:\/\/archive-coftb.dewberryanalytics.com\/?p=3805","title":{"rendered":"FTO 09-12-2016: Active Pattern Ahead as Dynamics And Moisture Return To Colorado"},"content":{"rendered":"<p>Issue Date: Monday, September 12th, 2016<br>\nIssue Time: 3:00PM MDT<br>\nValid Dates: September 13th through September 27th<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2016\/09\/threat_timeline2.png\"><img loading=\"lazy\" class=\"aligncenter  wp-image-3806\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2016\/09\/threat_timeline2.png\" alt=\"threat_timeline\" width=\"874\" height=\"115\"\/><\/a><\/p>\n<p>As alluded to in last Thurday&rsquo;s Flood Threat Outlook and shown in the water vapor image, below, a low-pressure system and associated 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> is located over northern California. Despite the seemingly favorable dynamics of this kind of setup, initially (today) rain drops will be few and far between over Colorado. However, as the <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;boundary layer&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;&amp;lt;\/p&amp;gt;\n&amp;lt;!-- \/wp:paragraph --&amp;gt;&amp;lt;br \/&amp;gt;&amp;lt;p&amp;gt;&amp;lt;span style=&amp;quot;color: #ffffff;&amp;quot;&amp;gt;The lower portion of the atmosphere that is directly influenced by the earth&amp;#039;s surface. Primarily, the boundary layer is driven by solar heating during the day and radiational cooling at night.&amp;lt;\/span&amp;gt;&amp;lt;\/p&amp;gt;&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>boundary layer<\/span> flow turns southeasterly in association with a surface low-pressure expected to form north of CO, higher moisture will slowly stream into Colorado. This will setup Event #1 on Wednesday and Thursday. Thereafter, a ridge off the west coast of North American will establish dominance over western Canada. This will promote seasonably mild and drier conditions statewide for a period of 3-5 days. By the week of Monday, 9\/19, another 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> currently found off the southwest side of the far western Aleutian islands will propagate across the eastern North Pacific and will likely impact Colorado. However, despite the once-again generally favorable dynamics from the proximity to the <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>, the heavy rainfall threat is not certain. One uncertainty is the degree of moisture return, which will tend to limit the flood threat to southern and eastern areas. Another somewhat related uncertainty is the potential for a deep subtropical connection, which would promote a chance of heavy rain across relatively large portions of the western slope. Currently, the moisture return for Event #2 looks marginal; hence, we identify this as No Apparent Flood Threat. However, stay tuned to the next FTO for updates. After Event #2, guidance rapidly diverges with some scenarios showing a wet Colorado with prolonged subtropical moisture return from the south\/southwest. Others paint a much drier scenario with seasonable temperatures. This disparity in guidance is likely due to the expected development of 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> across the southwest, which is notorious for erratic movements. Again, check the next FTO for an updated assessment of this feature.<\/p>\n<h3><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2016\/09\/wv_markup5.png\"><img loading=\"lazy\" class=\"aligncenter  wp-image-3807\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2016\/09\/wv_markup5.png\" alt=\"wv_markup\" width=\"746\" height=\"407\"\/><\/a><\/h3>\n<p>Below we describe the details of the two Events.<\/p>\n<p><strong>Event #1: Wednesday (9\/14) and Thursday (9\/15)<\/strong><\/p>\n<p>An <span style=\"color: #ff6600;\"><strong>Elevated Flood Threat<\/strong><\/span> for eastern areas<\/p>\n<p>This is Event #2 from last Thursday&rsquo;s FTO and certainly a rapidly evolving one. The latest guidance suggests the possibility of a cool front to stall out across eastern Colorado. At a minimum, daily rounds of <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;scattered&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;25-40% areal coverage&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>scattered<\/span> showers and thunderstorms will be found across and south of the front, mainly closer to the Kansas border. On the other hand, a focused stalled out front could cause multiple rounds of storm activity on Wednesday and Thursday. At this point, up to 2.25 inches of rainfall will be possible over a 48-hour period across eastern Colorado with up to 0.75 inches farther south and west in the foothills. There is a chance that this event may need to be upgraded to a High flood threat status, depending on whether there is enough consensus that thunderstorm <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;training&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Continuous or repeated rainfall over the same region&nbsp;in a relatively short time span. Training thunderstorms can produce very high rainfall totals and cause flash flooding.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>training<\/span> (or redevelopment over the areas). Stay tuned to upcoming FTBs for the latest updates.<\/p>\n<p><iframe loading=\"lazy\" src=\"https:\/\/a.tiles.mapbox.com\/v4\/sgeiger.1cffam84\/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: Monday (9\/19) and Tuesday (9\/20)<\/strong><\/h3>\n<p><span style=\"color: #0000ff;\"><strong>No Apparent Flood Threat<\/strong><\/span> but this event could be upgraded<\/p>\n<p>The active weather conditions will pause briefly as drier air follows the passage of Event #1. By Sunday 9\/18, height falls associated with the next 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> will being across the southwest United States. While some rainfall may occur Sunday, it is likely that the atmosphere will be too dry at that point (in fact, similar to today&rsquo;s weather situation, 9\/12). However, by Monday, southerly flow will usher in higher low-level moisture and adequate instability will develop to promote <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;scattered&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;25-40% areal coverage&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>scattered<\/span> to <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> thunderstorms. The most favored areas for heavy rain will likely be across southern areas. A few rounds of thunderstorm activity could produce up to 1.5 inches of rain over a 48-hour period. At this point, we are leaving this without a flood threat as rainfall amounts should remain below flood guidance. However, it is certainly possible that this event may need to be upgraded. This could occur if deep tropical moisture becomes involved in the return flow. Another potential scenario is the recurving of a tropical cyclone, as we recently witnessed with Newton. Due to the low confidence in such long-lead forecasts in the tropics, No Apparent Flood Threat is seen at this time.<br><iframe loading=\"lazy\" src=\"https:\/\/a.tiles.mapbox.com\/v4\/sgeiger.1cffn0c8\/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>","protected":false},"excerpt":{"rendered":"<p>Issue Date: Monday, September 12th, 2016 Issue Time: 3:00PM MDT Valid Dates: September 13th through September 27th As alluded to in last Thurday&rsquo;s Flood Threat Outlook and shown in the water vapor image, below, a low-pressure system and associated 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> is located over northern California. Despite the seemingly favorable dynamics of this kind of [&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\/3805"}],"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=3805"}],"version-history":[{"count":5,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/3805\/revisions"}],"predecessor-version":[{"id":3812,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/3805\/revisions\/3812"}],"wp:attachment":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=3805"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=3805"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=3805"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}