{"id":10156,"date":"2019-08-04T09:40:13","date_gmt":"2019-08-04T15:40:13","guid":{"rendered":"https:\/\/www.coloradofloodthreat.com\/?p=10156"},"modified":"2019-10-08T11:16:34","modified_gmt":"2019-10-08T17:16:34","slug":"ftb-08-04-2019-more-rain-over-the-high-country-moderate-threat-issued-over-burn-scars","status":"publish","type":"post","link":"https:\/\/archive-coftb.dewberryanalytics.com\/?p=10156","title":{"rendered":"FTB 08-04-2019: More Rain over the High Country, Moderate Threat Issued over Burn Scars"},"content":{"rendered":"<p>Issue Date: Sunday, August 4, 2019<br>\nIssue Time: 10AM MDT<\/p>\n<p><em>-A <strong>MODERATE<\/strong> flood threat has been issued for the 416, Junkins, Spring Creek, Hayden Pass and Lake Christine burn areas<\/em><\/p>\n<p><em>-A <strong>LOW<\/strong> flood threat has been issued for portions of the Southwest Slope, San Juan Mountains, Grand Valley, Northwest Slope, Northern Mountains, Front Range, Central Mountains and Southeast Mountains<\/em><\/p>\n<p>Expect similar weather statewide again today, but with a return of moisture over the northern mountain ranges and areas of the eastern plains. The subtropical high pressure remains overhead, with clockwise flow around the state once again. Embedded within the flow is a <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> (&ldquo;X&rdquo; below) and local vorticity maximum that will move across Colorado today. This feature will provide lift and dynamical forcing for thunderstorms over the high country and eastern plains. Due to extra lift, rain will most likely be heavier than yesterday. Marked below on the visible satellite imagery is a surface high pressure system over the CO\/NM border with a broad region of low pressure over the eastern plains. Wind flow around the two features will combine to produce <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;downsloping&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Refers to the winds that blow from higher elevations down towards lower elevations. As air parcels descend, they warm, which often results in rapid warming of areas near the higher terrains. It also promotes lower relative humidity values and stability, which prevents thunderstorm development.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>downsloping<\/span> flow over the Southeast Plains, creating a localized <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;dryline&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;A low-level, small-scale boundary that separates dry air from moist air. Storms develop along it because the dry air (behind the boundary) is less dense than the moisture-rich air (ahead of the boundary). Typically, it advances eastward during the afternoon and retreats westward at night.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>dryline<\/span> over the area. This <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;dryline&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;A low-level, small-scale boundary that separates dry air from moist air. Storms develop along it because the dry air (behind the boundary) is less dense than the moisture-rich air (ahead of the boundary). Typically, it advances eastward during the afternoon and retreats westward at night.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>dryline<\/span> will <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> most storms over the Southeast Plains but provide a boundary for storms to form to the north. Thunderstorms are forecast over most of the high country as well as the Northeast Plains and Palmer Ridge.<\/p>\n<p>Atmospheric moisture has increased over western Colorado from yesterday, with <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> measuring 1.1 inches over Grand Junction this morning. Surface based moisture is very similar, but dewpoints over the high country have increased to the mid 40&deg;Fs due to yesterday&rsquo;s rain. Over the eastern plains surface moisture is similar to yesterday as well, but sunny skies this morning are likely to mix out low level moisture once again. The <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> will pass over the high country during peak heating, which will create <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> thunderstorms capable of producing heavy rain. The system will arrive past the time of peak instability over the eastern plains, which should keep storms lighter. Steering flows over the mountains will vary between 10 and 20 mph, creating the primary threat of multiple storms over a 2-3 hour period. Recent rainfall over burn areas has increased the threat to Moderate over the 416, Junkins, Hayden Pass, Spring Creek and Lake Christine burn areas<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2019\/08\/FTB_20190804_VIS.jpg\"><img loading=\"lazy\" class=\"aligncenter wp-image-10157\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2019\/08\/FTB_20190804_VIS.jpg\" alt=\"\" width=\"750\" height=\"585\"\/><\/a><\/p>\n<h3><strong>Today&rsquo;s Flood Threat Map<\/strong><\/h3>\n<p>For more information on today&rsquo;s flood threat, see the map below. For Zone-Specific forecasts, scroll below the map.<\/p>\n<div style=\"position: relative;\"><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2019\/08\/FTB_20190804_snap.png\"><img loading=\"lazy\" class=\"aligncenter size-full wp-image-10163\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2019\/08\/FTB_20190804_snap.png\" alt=\"\" width=\"880\" height=\"550\"\/><\/a><\/div>\n<div><img loading=\"lazy\" class=\"alignright wp-image-135\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2015\/04\/floodthreat_legend2.png\" alt=\"Flood Threat Legend\" width=\"275\" height=\"71\"\/><\/div>\n<h3><strong>Zone-Specific Forecasts:<\/strong><\/h3>\n<h4><strong>Southwest Slope, San Juan Mountains, San Luis Valley, Grand Valley, Central Mountains, Northern Mountains, Northwest Slope:<\/strong><\/h4>\n<p>Chances for precipitation are high throughout the area today. Heavier rainfall rates will once again favor the mountains to the south of I-70, however moderate and heavy rainfall is still possible over areas to the north. The primarily threat today is rainfall over a 2-3 hour period. Max 2-3 hour rainfall rates of 1.25 inches are forecast over the area, with rates up to 1.75 inches over the Southwest Slope and San Juan Mountains. <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> areas of 1-hour max rainfall rates up to 1 inch are possible, but most areas will have max 1-hour rainfall rates of 0.5 inches. Rainfall will mostly be confined to higher terrain, with greater threats over steeper terrain and recent burn areas. Threats include <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 flows and flooding of small rivers and streams.<\/p>\n<p>Primetime: 11AM to 11PM<\/p>\n<h4><strong>Front Range, Urban Corridor, Southeast Mountains, Raton Ridge, Southeast Plains, Palmer Ridge, Northeast Plains:<\/strong><\/h4>\n<p>The highest chances of rainfall today will be over the Front Range and Southeast Mountains. Storms may move off of the Front Range this afternoon, but drier air underneath the storm base will limit severe weather potential over the Urban Corridor, Palmer Ridge and Northeast Plains. A few weak storms may move over the Raton Ridge this afternoon, but rainfall will be very limited as well. Max 2-3 hour rainfall rates of 1 inch are forecast over the Southeast Mountains and southern Front Range. Recent rain over the area will increase chances for flooding over these regions, with the highest chance over the recent burn areas. Threats include <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 flows and flooding of small rivers and streams. The northern Front Range, Urban Corridor and eastern plains are expected to be drier once again today, with max 1-hour rainfall rates of 0.4 inches. The chance for measurable rain over these areas is confined to the upper elevations, Palmer Ridge and Northeast Plains.<\/p>\n<p>Primetime: 1PM to 12PM<\/p>","protected":false},"excerpt":{"rendered":"<p>Issue Date: Sunday, August 4, 2019 Issue Time: 10AM MDT -A MODERATE flood threat has been issued for the 416, Junkins, Spring Creek, Hayden Pass and Lake Christine burn areas -A LOW flood threat has been issued for portions of the Southwest Slope, San Juan Mountains, Grand Valley, Northwest Slope, Northern Mountains, Front Range, Central [&hellip;]<\/p>","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":[],"categories":[6],"tags":[],"post_mailing_queue_ids":[],"_links":{"self":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/10156"}],"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\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=10156"}],"version-history":[{"count":3,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/10156\/revisions"}],"predecessor-version":[{"id":11072,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/10156\/revisions\/11072"}],"wp:attachment":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=10156"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=10156"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=10156"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}