{"id":5731,"date":"2017-07-31T13:28:26","date_gmt":"2017-07-31T19:28:26","guid":{"rendered":"https:\/\/www.coloradofloodthreat.com\/?p=5731"},"modified":"2017-08-03T12:11:46","modified_gmt":"2017-08-03T18:11:46","slug":"fto-07-31-2017-drying-short-lived-as-moisture-to-find-its-way-back-into-colorado","status":"publish","type":"post","link":"https:\/\/archive-coftb.dewberryanalytics.com\/?p=5731","title":{"rendered":"FTO 07-31-2017: Drying Short-Lived As Moisture To Find Its Way Back Into Colorado"},"content":{"rendered":"<p>Issue Date: Monday, July 31, 2017<br>\nIssue Time: 1:30PM MDT<br>\nValid Dates: 8\/1 &ndash; 8\/15<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/threat_timeline-8.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-5734\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/threat_timeline-8.png\" alt=\"\" width=\"880\" height=\"117\"\/><\/a><\/p>\n<p>After quiet a memorable stretch of active weather, noticeable drying has begun across roughly the western half of our state. Before getting to today&rsquo;s Outlook, we want to reflect on just how impressive the recent rainfall has been. Below are 30-day precipitation estimates from the <a href=\"http:\/\/water.weather.gov\/precip\/\">NOAA River Forecast Centers<\/a>. <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;isolated&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;less than 10% areal coverage&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>Isolated<\/span> parts of southeast Colorado have received over 10 inches (even as high as 15 inches) of rainfall since July 1<sup>st<\/sup>. Even more impressively is that this has occurred through a prolonged stretch of days with very heavy rainfall, as opposed to one or two events. So how does this stack up with climatology? Average July precipitation depends strongly on elevation, but 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>, roughly ranges from 1.5 inches in the lowest elevations to as much as 4 inches in the foothills of the Palmer Ridge and Wet Mountains. Thus, over the last 30 days, <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;isolated&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;less than 10% areal coverage&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>isolated<\/span> locations circled in the left map below, have experienced anywhere from 3 to 5 times their normal rainfall. Looking at NOAA Atlas 14 guidance, this equates to a 1 in 100-500 year event, depending on your exact location. For example, in eastern El Paso County, Atlas 14 estimates that a 30-day rainfall of 10.3 inches is a 1 in a 100 year event, with the 1 in the 1000 year event estimate being 13.7 inches.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/precip_30day.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-5733\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/precip_30day.png\" alt=\"\" width=\"880\" height=\"295\"\/><\/a><\/p>\n<p>Shifting the focus back to the Outlook, this afternoon&rsquo;s water vapor image, below, shows some notable changes in the weather pattern across western North America. The upper-level ridge located south of Colorado, which has been responsible for moisture <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;advection&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;The process of transport of an atmospheric property, typically temperature or moisture in our FTB discussions, by the wind. &amp;quot;Strong&rdquo; or &amp;quot;weak&rdquo; advection refers to the rate of change of the advected property&amp;#039;s value at a given point.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>advection<\/span> into the state, has expanded westward. The upper-level flow is currently switching to a more westerly component, which is now advecting much drier air from the west (see dryness over California). In addition, a strong surface high pressure is expected to move southward out of Canada over the next 72 hours. A cool (or even &ldquo;cold&rdquo;?!) frontal passage is expected across eastern Colorado that will limit high temperatures to as much as 15F below normal by mid-week. Frontal dynamics will likely support light to moderate precipitation that we label Event #1, but with limited instability, we currently do not expect a flood threat. Thereafter, a dynamic pattern will ensue with an upper-level <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> expected to establish across the central United States. Frequent <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;shortwave&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;A disturbance in the mid or upper part of the atmosphere which induces upward motion ahead of it.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>shortwave<\/span> and surface frontal passages are expected across eastern Colorado, which should be accompanied by at least 24 hours of return flow to elevate moisture levels. We expect a multi-day elevated flood threat (Event #2) mainly across northeast Colorado. However, with fast steering winds, only <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;isolated&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;less than 10% areal coverage&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>isolated<\/span> heavy rainfall (though with possible severe weather) is currently expected.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/wv_markup-14.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-5735 size-full\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/wv_markup-14.png\" alt=\"\" width=\"672\" height=\"404\"\/><\/a><\/p>\n<p>The forecasted <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> plumes from the GFS Ensembles, below, show that Denver will continue to experience average to above average moisture levels. Meanwhile, Grand Junction will remain mainly below normal. Overall, we expect a pause in the <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>, and an increase in &ldquo;action&rdquo; for northeast Colorado.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/gefs_pw-2.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-5732\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/gefs_pw-2.png\" alt=\"\" width=\"800\" height=\"281\"\/><\/a><\/p>\n<p>We have identified two precipitation events for this Outlook, which are described in more detail below.<\/p>\n<h3><strong>Event #1: Tuesday (8\/1) through Thursday (8\/3)<\/strong><\/h3>\n<p><span style=\"color: #3366ff;\"><strong>No Apparent Flood Threat <\/strong><\/span>though light to moderate precipitation will be possible<\/p>\n<p>Elevated moisture levels will continue to be scoured out of Colorado as upper-level westerly flow advects in drier air. On Tuesday and Wednesday, <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> thunderstorms will be possible mainly across southern Colorado. However, with faster steering winds, total precipitation is expected to stay on the lighter side, in the 0.5 &ndash; 0.75 inch range (hence, no precipitation map). On Thursday, a strong, fall-like cool front will move southward across eastern Colorado, stabilizing the air mass and putting a <span class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;cap&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;The area where a parcel of air has negative buoyancy or sinks. The intensity of the cap is measured by its convective inhibition. If the cap is sufficiently large, it may prevent thunderstorms from forming at all.&lt;\/div&gt;\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>cap<\/span> on heavy rainfall coverage and intensity. Some upslope rain showers and perhaps a weak thunderstorm are expected, but flooding is not expected at this time.<\/p>\n<h3><strong>Event #2: Friday (8\/4) through Monday (8\/7)<\/strong><\/h3>\n<p><span style=\"color: #ff6600;\"><strong>Elevated Flood Threat <\/strong><\/span>for <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;isolated&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;less than 10% areal coverage&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>isolated<\/span> heavy rainfall with current guidance suggesting northeast Colorado as target<\/p>\n<p>Summer-time cool fronts are fleeting and return southeasterly flow will quickly set up by Friday. <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 return back into the 0.9 &ndash; 1.1 inch range (which is above normal). <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;isolated&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;less than 10% areal coverage&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>Isolated<\/span> thunderstorms will return to our forecast then, and increase in coverage and intensity into the weekend as one or more additional weak frontal passages is possible. These fronts will act more of focal points for storms, with little temperature changes. The northeast quadrant of the state is expected to see the highest coverage of thunderstorm activity. At this time, we foresee max 1-hour rain rates up to 1.2 inches (west) and 1.6 inches (east). In addition, severe weather chances, are expected to increase as bulk <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;wind shear&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Local variation of the wind, either in the horizontal or vertical direction.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>wind shear<\/span> ramps up to above 30 kts. We have labeled this event with an elevated flood threat mainly for <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;isolated&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;less than 10% areal coverage&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>isolated<\/span> <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>. Stay tuned to the next Outlook for a better assessment of this event.<\/p>\n<div style=\"position: relative;\"><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/FTO_20170731_e1.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-5776\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/FTO_20170731_e1.png\" alt=\"\" width=\"880\" height=\"500\"\/><\/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: Monday, July 31, 2017 Issue Time: 1:30PM MDT Valid Dates: 8\/1 &ndash; 8\/15 After quiet a memorable stretch of active weather, noticeable drying has begun across roughly the western half of our state. Before getting to today&rsquo;s Outlook, we want to reflect on just how impressive the recent rainfall has been. Below are [&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\/5731"}],"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=5731"}],"version-history":[{"count":3,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/5731\/revisions"}],"predecessor-version":[{"id":5778,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/5731\/revisions\/5778"}],"wp:attachment":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=5731"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=5731"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=5731"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}