{"id":5670,"date":"2017-07-27T14:51:56","date_gmt":"2017-07-27T20:51:56","guid":{"rendered":"https:\/\/www.coloradofloodthreat.com\/?p=5670"},"modified":"2017-07-31T10:32:43","modified_gmt":"2017-07-31T16:32:43","slug":"fto-07-27-2017-streak-of-heavy-rainfall-to-continue-then-substantial-drying","status":"publish","type":"post","link":"https:\/\/archive-coftb.dewberryanalytics.com\/?p=5670","title":{"rendered":"FTO 07-27-2017: Streak Of Heavy Rainfall To Continue, Then Substantial Drying"},"content":{"rendered":"<p>Issue Date: Thursday, July 27, 2017<br>\nIssue Time: 3PM MDT<br>\nValid Dates: 7\/28-8\/11<\/p>\n<h3><strong><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/threat_timeline-7.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-5673\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/threat_timeline-7.png\" alt=\"\" width=\"880\" height=\"123\"\/><\/a><\/strong><\/h3>\n<p>If you have ever read either our Flood Threat Bulletin or Flood Threat Outlook discussions, you can probably quickly recall how much emphasis we place in analyzing moisture content when developing the flood threat forecast. The reason for this is that sometimes, especially in the summertime, moisture is as good or better predictor for heavy rainfall that any other guidance, including model Quantitative Precipitation Forecasts! For you technical readers, <a href=\"http:\/\/journals.ametsoc.org\/doi\/abs\/10.1175\/MWR-D-15-0061.1\">please refer to this paper in the Monthly Weather Review journal<\/a> for more information. In short, it is not so much that moisture is a good predictor of where or when thunderstorms will develop, or even how long they last, but it is a good predictor of the upper limit of their potential rain rates.<\/p>\n<p>So how has moisture fared across Colorado recently? With little shock, the table below shows significantly above normal amounts over (at least) the past 7 days, as measured by column integrated <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;precipitable water&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;The total atmospheric water vapor contained in a vertical column of the atmosphere. It is typically measured in inches, and anomalously (deviation from normal) high values of precipitable water generally correlate to heavy rainfall potential.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>Precipitable Water<\/span> at both the Denver and Grand Junction evening soundings (the asterisk in the measurements at Denver signify that the radiosonde did not sample the entire atmosphere, implying that this reading <em>underestimates<\/em> the actual <span class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;PW&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;(Stands for: Precipitable Water) The total atmospheric water vapor contained in a vertical column of the atmosphere. It is typically measured in inches, and anomalously (deviation from normal) high values of precipitable water generally correlate to heavy rainfall potential.&lt;\/div&gt;\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>PW<\/span>). This was recently punctuated by values over 70% above normal, interestingly coinciding with one of the wettest 48-hour periods observed thus far this summer.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/pw_table.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-5672 size-full\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/pw_table.png\" alt=\"\" width=\"653\" height=\"191\"\/><\/a><\/p>\n<p>As this afternoon&rsquo;s water vapor image shows, below, the same familiar players will once again be in charge of flood potential for the next 5 days or so. The first feature is the upper-level ridge that is currently centered just south of Colorado. As long as the western periphery of this ridge does extend too much west of the Four Corners region, this typically allows for the transport of low and mid-level level <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;monsoon&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;a seasonal wind that brings moisture and rain to the region into which it blows; there is also a dry phase to monsoons, but popular usage refers only to the wet phase; these winds occur in many places around the world, and where they occur they are responsible for a majority of that location&rsquo;s annual precipitation&amp;lt;\/p&amp;gt;\n&amp;lt;!-- \/wp:paragraph --&amp;gt;&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>monsoon<\/span> moisture into Colorado. This is expected to continue over the next 5 days, keeping elevated moisture and above normal heavy rainfall chances in the picture.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/wv_markup-12.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-5674 size-full\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/wv_markup-12.png\" alt=\"\" width=\"590\" height=\"395\"\/><\/a><\/p>\n<p>The second, and often overlooked feature, is the presence of surface high pressure features that act to (i) move southward &ldquo;cool&rdquo; fronts, especially across eastern Colorado and (ii) more importantly, provide enhanced pulses of moist upslope flow that can interact favorably with the climatological circulation to accentuate and expand the lifetime and eastward extent of the elevated <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;convection&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Refers to vertical atmospheric motion driven by buoyancy, i.e., warm air is less dense than cool air, and therefore rises. One of the primary drivers of thunderstorm development, especially during monsoon season.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>convection<\/span> over our higher terrain. As shown below in an interesting analysis of surface pressure anomalies available on the <a href=\"http:\/\/www.tropicaltidbits.com\/\">Tropical Tidbits<\/a> model site, another surface high pressure is expected to move southward out of Canada. By Sunday and Monday, a stronger than normal fetch of moist, upslope easterly flow is expected across southeast Colorado. The result will be a pattern conducive for slow moving storms capable of producing very heavy rain rates, much like on Wednesday.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/gfs-ens_mslpaNorm_us_15.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-5671\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/gfs-ens_mslpaNorm_us_15.png\" alt=\"\" width=\"680\" height=\"462\"\/><\/a><\/p>\n<p>After the passage of this surface high pressure, guidance has now come into good agreement that the upper-level ridge will shift westward, which will drastically reduce moisture levels across most of Colorado. Heavy rainfall and precipitation chances are expected to lessen to below their climatological average accordingly.<\/p>\n<p>For this edition of the 15-day Flood Threat Outlook, we have identified one prolonged Elevated\/High flood threat event that is discussed in more detail below.<\/p>\n<h3><strong>Event #1: Friday (7\/28) through Tuesday (8\/1)<\/strong><\/h3>\n<p><span style=\"color: #ff6600;\"><strong>Elevated\/<span style=\"color: #800000;\">High<\/span> Flood Threat<\/strong><\/span> for <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;flash flooding&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;flash flooding can refer to usually dry areas becoming rapidly inundated with water, or rapid water level rises on streams, creeks, or rivers beyond flood stage; typically caused by heavy rainfall, but can also be caused by meltwater&amp;lt;\/p&amp;gt;\n&amp;lt;!-- \/wp:paragraph --&amp;gt;&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>flash flooding<\/span>, debris slides and mud flows, especially over higher terrain<\/p>\n<p>Above normal moisture will persist statewide through early next week. <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;precipitable water&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;The total atmospheric water vapor contained in a vertical column of the atmosphere. It is typically measured in inches, and anomalously (deviation from normal) high values of precipitable water generally correlate to heavy rainfall potential.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>Precipitable water<\/span> is expected to remain in the 0.9 &ndash; 1.6 inch range, which will support daily bouts 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> to <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;numerous&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;40-60% areal coverage&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>numerous<\/span> shower and thunderstorm activity from Friday through Tuesday. Rain rates up to 1.4 inches per hour (west) and 2.9 inches per hour (far east) will be possible, which will support an elevated flood threat. Highest coverage will be over the higher terrain, especially 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> as well as southeast Colorado. On Sunday\/Monday, a cool front is expected to enhance rainfall coverage over southeast Colorado and amplify the intensity further, sustaining longer duration heavy rainfall. Current guidance suggests 3-hour rainfall up to 4 inches will be possible in the foothills of the Sangre de Cristo and Wet Mountains. Max 3-hour rainfall up to 2.4 inches will be possible in the San Juan Mountains.<\/p>\n<p>As with the recent heavy rainfall event on Wednesday, this event will not have significant upper-level support implying that sustained heavy rainfall, beyond 3 hours, will not be likely. Thus, currently the main impacts of this event will be mud flows and debris slides in higher elevation locations, as well as small stream flooding associated with the stronger cells. Major riverine flooding is not expected at this time. Please stay tuned to daily Flood Threat Bulletins for more detailed information, especially if you plan on camping and hiking over the weekend.<\/p>\n<div style=\"position: relative;\"><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/FTO_20170727_e1.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-5729\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/FTO_20170727_e1.png\" alt=\"\" width=\"880\" height=\"499\"\/><\/a><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><\/div>","protected":false},"excerpt":{"rendered":"<p>Issue Date: Thursday, July 27, 2017 Issue Time: 3PM MDT Valid Dates: 7\/28-8\/11 If you have ever read either our Flood Threat Bulletin or Flood Threat Outlook discussions, you can probably quickly recall how much emphasis we place in analyzing moisture content when developing the flood threat forecast. The reason for this is that sometimes, [&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\/5670"}],"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=5670"}],"version-history":[{"count":4,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/5670\/revisions"}],"predecessor-version":[{"id":5730,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/5670\/revisions\/5730"}],"wp:attachment":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=5670"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=5670"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=5670"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}