{"id":12135,"date":"2020-07-02T14:27:18","date_gmt":"2020-07-02T20:27:18","guid":{"rendered":"https:\/\/www.coloradofloodthreat.com\/?p=12135"},"modified":"2020-07-06T07:53:03","modified_gmt":"2020-07-06T13:53:03","slug":"fto-07-02-2020-rainfall-returns-for-july-4th-weekend-intense-heat-to-follow","status":"publish","type":"post","link":"https:\/\/archive-coftb.dewberryanalytics.com\/?p=12135","title":{"rendered":"FTO 07-02-2020: Rainfall Returns for July 4th Weekend; Intense Heat To Follow"},"content":{"rendered":"<p>Issue Date: Thursday, July 2<sup>nd<\/sup>, 2020<br>\nIssue Time: 2:25PM MDT<br>\nValid Dates: 7\/03 &ndash; 7\/17<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/threat_timeline.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-12138\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/threat_timeline-1024x151.png\" alt=\"\" width=\"880\" height=\"130\" srcset=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/threat_timeline-1024x151.png 1024w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/threat_timeline-300x44.png 300w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/threat_timeline-768x113.png 768w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/threat_timeline.png 1195w\" sizes=\"(max-width: 880px) 100vw, 880px\"\/><\/a><\/p>\n<p>The afternoon&rsquo;s water vapor imagery, below, shows an amplified pattern over the eastern Pacific Ocean and stretching into the central United States. Amplified patterns sometimes result in active weather, but such is absolutely not the case in this situation. A large ridge, currently centered just east of Colorado, will be almost stationary over the next 7-10 days, resulting in little to no movement of water vapor in or out of the state. Meanwhile, 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> over southwest Canada will attempt to usher in <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> ripples in the flow. Ultimately, the ridge will remain in control, but not before a 72-96 hour event of increased precipitation chances mainly across central and eastern Colorado. This is the only precipitation event identified during this Independence Day Weekend-edition of the Outlook.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/WV_markup.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-12139\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/WV_markup-1024x619.png\" alt=\"\" width=\"811\" height=\"490\" srcset=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/WV_markup-1024x619.png 1024w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/WV_markup-300x181.png 300w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/WV_markup-768x464.png 768w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/WV_markup.png 1213w\" sizes=\"(max-width: 811px) 100vw, 811px\"\/><\/a><\/p>\n<p>Looking at the <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> plumes from the GFS ensemble shows a marked difference across 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>. While Denver will see a prolonged stretch of above normal moisture, Grand Junction will stay generally below normal. Thus, expect to see little to no precipitation below about 8,000 feet west 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>, with precipitation limited to about 0.5 inches for the higher elevations of the San Juan Mountains and Central Mountains. The area likely to see the highest rainfall amounts will be across the far eastern and southeastern Colorado border. There, plenty of residual moisture will be trapped 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> up to 1.3 inches along the southern border with Kansas. Although synoptic scale support will be rather weak, there will be sufficient instability for a 48 hour stretch of <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, warranted an Elevated flood threat for the Saturday-Sunday timeframe. This is certainly good news given the recent upgrade to extreme drought status for parts of southeast Colorado.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/GEFS_pw_plumes.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-12137\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/GEFS_pw_plumes-1024x360.png\" alt=\"\" width=\"907\" height=\"319\" srcset=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/GEFS_pw_plumes-1024x360.png 1024w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/GEFS_pw_plumes-300x105.png 300w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/GEFS_pw_plumes-768x270.png 768w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/GEFS_pw_plumes.png 1289w\" sizes=\"(max-width: 907px) 100vw, 907px\"\/><\/a><\/p>\n<p>The aforementioned ridge is expected to take firm control of Colorado&rsquo;s weather beginning Tuesday of next week (July 7th), as is clearly seen in the GFS ensemble forecast of 850 mb temperatures for Denver. Expect a 3+ day stretch of much above normal temperatures, reaching 100F even for elevations up to 5,500 feet. The prospects for <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> rainfall look very slim from Tuesday July 7th, onward. However, residual moisture could still produce higher terrain showers and storms depending on how much moisture is available in 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>. However, at this time, precipitation amounts above 0.5 inches do not appear likely.<\/p>\n<p>Event #1 is outlined in more detail.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/GEFS_Denver_850mb.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-12136\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/GEFS_Denver_850mb.png\" alt=\"\" width=\"480\" height=\"317\" srcset=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/GEFS_Denver_850mb.png 806w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/GEFS_Denver_850mb-300x198.png 300w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/GEFS_Denver_850mb-768x507.png 768w\" sizes=\"(max-width: 480px) 100vw, 480px\"\/><\/a><\/p>\n<h3>Event #1: Friday (6\/26) &ndash; Monday (6\/29)<\/h3>\n<p><strong><span style=\"color: #ff6600;\">Elevated Threat<\/span> on Saturday and Sunday with heavy rainfall possible along the Kansas border<\/strong><\/p>\n<p>Rainfall coverage will increase on Friday, with the highest coverage over the higher terrain as well as northeast Colorado where <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> severe storms will be possible. On Saturday and Sunday, the southeast quadrant of the state is expected to see the most activity, with one or two rounds of afternoon and evening showers and thunderstorms possible. Rainfall rates in the higher terrain are expected to stay at or below 0.5 inches so no flooding is anticipated, though the Decker and Spring Creek burn scars will need to be watched. Farther southeast, rainfall rates up to 2.4 inches per hour look to be possible across far southeast Colorado, as <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> approaches 1.3 inches. Exact placement of storms will depend on mesoscale boundaries and the <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> position. Check back to daily Flood Threat Bulletins for updates.<\/p>\n<p><img loading=\"lazy\" class=\"alignnone wp-image-12179\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/FTO_20200702_e1.png\" alt=\"\" width=\"880\" height=\"594\" srcset=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/FTO_20200702_e1.png 888w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/FTO_20200702_e1-300x202.png 300w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/07\/FTO_20200702_e1-768x518.png 768w\" sizes=\"(max-width: 880px) 100vw, 880px\"\/><\/p>","protected":false},"excerpt":{"rendered":"<p>Issue Date: Thursday, July 2nd, 2020 Issue Time: 2:25PM MDT Valid Dates: 7\/03 &ndash; 7\/17 The afternoon&rsquo;s water vapor imagery, below, shows an amplified pattern over the eastern Pacific Ocean and stretching into the central United States. Amplified patterns sometimes result in active weather, but such is absolutely not the case in this situation. A [&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\/12135"}],"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=12135"}],"version-history":[{"count":3,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/12135\/revisions"}],"predecessor-version":[{"id":12180,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/12135\/revisions\/12180"}],"wp:attachment":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=12135"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=12135"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=12135"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}