{"id":12046,"date":"2020-06-25T13:32:56","date_gmt":"2020-06-25T19:32:56","guid":{"rendered":"https:\/\/www.coloradofloodthreat.com\/?p=12046"},"modified":"2020-06-29T11:59:44","modified_gmt":"2020-06-29T17:59:44","slug":"fto-06-25-2020-heavy-rainfall-and-severe-thunderstorms-forecast-for-the-eastern-plains-on-friday","status":"publish","type":"post","link":"https:\/\/archive-coftb.dewberryanalytics.com\/?p=12046","title":{"rendered":"FTO 06-25-2020: Heavy Rainfall and Severe Thunderstorms Forecast for the Eastern Plains on Friday"},"content":{"rendered":"<p>Issue Date: Thursday,&nbsp;June 25th, 2020<br>\nIssue Time: 1:30PM MDT<br>\nValid Dates:&nbsp;6\/26 &ndash; 7\/10<\/p>\n<p><img loading=\"lazy\" class=\"aligncenter wp-image-12049\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/FTO-20200625-1.png\" alt=\"\" width=\"880\" height=\"131\" srcset=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/FTO-20200625-1.png 1152w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/FTO-20200625-1-300x45.png 300w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/FTO-20200625-1-768x115.png 768w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/FTO-20200625-1-1024x153.png 1024w\" sizes=\"(max-width: 880px) 100vw, 880px\"\/><\/p>\n<p>Event #1 continues tomorrow as 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> breaks off the main flow and begins to dig south over California. This will change the flow aloft to more westerly and release some mid-level energy into the state for additional afternoon lift. 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> to our north will also push a cold front south this evening, which will cool temperatures off and allow decent low-level moisture to return for more <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>, organized rainfall over the mountains and adjacent plains on Friday. The moisture rich environment paired with better upper level dynamics will likely produce a few <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;severe thunderstorms&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Thunderstorms that produce a tornado, winds of at least 58 mph (50 kts) and\/or hail at least 1&amp;quot; in diameter.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>severe thunderstorms<\/span> and heavy rainfall over eastern Colorado.<\/p>\n<p>From Saturday into Sunday, the next <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> quickly moves eastward (Event #2). This will help push the California vorticity max (Event #1) through the state, and the vorticity max (Event #2) quickly strengthens into a closed Low system. Event #2 will produce southwest flow aloft, which is expected to pull in drier air over the state from Sunday into Monday. This may cause some <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;critical fire weather&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;weather conditions especially conducive to the formation of wildfires; typically strong winds, low relative humidity, and atmospheric instability&amp;lt;\/p&amp;gt;\n&amp;lt;!-- \/wp:paragraph --&amp;gt;&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>critical fire weather<\/span> for western Colorado as the jet rotates around the base of 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>. Additionally, the drier air mass will reduce afternoon rainfall chances Sunday and likely produce dry conditions on Monday. As Event #2 exits northward (blocking Low to the east), some light rainfall may be possible over the northern mountains and immediate adjacent plains. Expected enhanced fire weather through at least mid-week.<\/p>\n<p><img loading=\"lazy\" class=\"aligncenter wp-image-12048 size-full\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/wv-20200625.png\" alt=\"\" width=\"671\" height=\"398\" srcset=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/wv-20200625.png 671w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/wv-20200625-300x178.png 300w\" sizes=\"(max-width: 671px) 100vw, 671px\"\/><\/p>\n<p>The site for the GEFS plumes is currently down, and with no fix in sight, I had to get a little creative today. Below is the 12Z (or morning) run of the HRRR showing <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;dew points&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;The temperature to which a given air parcel must be cooled (at constant pressure and water vapor content) in order for saturation to occur.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>dew points<\/span> over Colorado at midnight tonight. The first thing you should notice is the very dry air mass over the southwest corner and the very moist air mass over the northern border\/eastern Colorado. The reason for the high moisture over eastern Colorado is the cold front dropping south. <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;dew points&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;The temperature to which a given air parcel must be cooled (at constant pressure and water vapor content) in order for saturation to occur.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>Dew points<\/span> behind the front increase 10-15F! While there may be a little drying at the mid-levels along the Urban Corridor throughout the day on Friday with weak westerly flow aloft, it remains quite moist over the eastern plains. This will translate into very efficient rain rates with moderate steering flows for storms; thus, an Elevated flood threat is issued. Unfortunately, the dry air over southwestern Colorado will remain intact and confine <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>, afternoon storms to the mountains and elevated terrains over the Grand Valley, Northwest Slope, Northern Mountains and Central Mountains.<\/p>\n<p><img loading=\"lazy\" class=\"aligncenter wp-image-12050\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/hrrr_Tds.png\" alt=\"\" width=\"500\" height=\"347\" srcset=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/hrrr_Tds.png 413w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/hrrr_Tds-300x208.png 300w\" sizes=\"(max-width: 500px) 100vw, 500px\"\/><\/p>\n<p>For a look at Event #2, the GEFS 6-8 day (valid Tuesday, Wednesday, and Thursday) chance of precipitation &gt; 0.50 inches was pulled. While there may be some issues with topography due to the coarse resolution of the model, outside of the northeast corner of the state, chances of accumulations greater than 0.50 inches are less than 30% over this period. This just illustrates that there will not be much moisture associated with Event #2, and the main hazard will be <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;critical fire weather&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;weather conditions especially conducive to the formation of wildfires; typically strong winds, low relative humidity, and atmospheric instability&amp;lt;\/p&amp;gt;\n&amp;lt;!-- \/wp:paragraph --&amp;gt;&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>critical fire weather<\/span> for Colorado &ndash; especially western Colorado.<\/p>\n<p><img loading=\"lazy\" class=\"aligncenter wp-image-12051 size-full\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/GEFS_prcp.gt_.0.5.png\" alt=\"\" width=\"719\" height=\"433\" srcset=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/GEFS_prcp.gt_.0.5.png 719w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/GEFS_prcp.gt_.0.5-300x181.png 300w\" sizes=\"(max-width: 719px) 100vw, 719px\"\/><\/p>\n<h3><strong>Event #1:<\/strong> <strong>Friday<\/strong><strong> (6\/2<\/strong><strong>6<\/strong><strong>) &ndash; <\/strong><strong>Sunday<\/strong><strong> (6\/2<\/strong><strong>8<\/strong><strong>)<\/strong><\/h3>\n<p><span style=\"color: #ff6600;\"><strong>Elevated Threat<\/strong><\/span><strong>\/<span style=\"color: #0000ff;\">No Apparent Threat<\/span>&nbsp;<\/strong>as a cutoff vorticity max brings extra mid-level energy to a moist air mass over eastern Colorado.<\/p>\n<p>Friday should have more organized thunderstorms when compared to the last couple of days. A couple of these could become severe over the eastern plains with heavy rainfall, large hail (&gt;1.25 in), and wind gusts (60 mph) possible. The wind threat will increase as storms become more of a <span class=\"glossaryLink\"  aria-describedby=\"tt\"  data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;MCS&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;(Stands for: Mesoscale Convective System) A complex of thunderstorms that produces a large, contiguous area of precipitation on the order of 100 km or more in the horizontal scale and normally persist for several hours or more.&lt;\/div&gt;\"  data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>MCS<\/span>\/bow echo over the plains. <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;outflow boundaries&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;A surface boundary formed by the horizontal spreading of thunderstorm-cooled air. Outflow boundaries may intersect with each other or with other features (fronts, dry line, low-level jet) and initiate new convection. Brief strong winds are possible with outflow boundaries, and they can also persist for more than 24 hours.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>Outflow boundaries<\/span> will help trigger additional <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> for more <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> coverage as they move off the mountains by early afternoon. Storms are expected to cross into Kansas and Nebraska around midnight.<\/p>\n<p>On Saturday, residual moisture may cause some storms to form over the Central, Northern and Front Range Mountains. With storm motion from the southwest to northeast, storms should spread into the Urban Corridor, Palmer Ridge, and Northeast Plains. With drier low levels the main threat will be gusty <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;outflow&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;A cool pool of air that results when a thunderstorm downdraft reaches the surface and spreads horizontally.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>outflow<\/span> winds and moderate rainfall. Even fewer storms are anticipated to form over the mountains on Sunday.<\/p>\n<p><img loading=\"lazy\" class=\"alignnone wp-image-12092\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/FTO_20200625_e1.png\" alt=\"\" width=\"880\" height=\"595\" srcset=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/FTO_20200625_e1.png 891w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/FTO_20200625_e1-300x203.png 300w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/FTO_20200625_e1-768x519.png 768w\" sizes=\"(max-width: 880px) 100vw, 880px\"\/><\/p>\n<h3><strong>Event #2: <\/strong><strong>Tuesday<\/strong><strong> &ndash; <\/strong><strong>Wednesday<\/strong><strong> (6\/<\/strong><strong>30<\/strong> <strong>&ndash;<\/strong> <strong>7\/1<\/strong><strong>)<\/strong><\/h3>\n<p><strong><span style=\"color: #0000ff;\">No Apparent Threat<\/span>&nbsp;<\/strong>as the closed Low lifts northwards out of the state.<\/p>\n<p>As mentioned above, the main threat will be fire danger for Event #2 over Colorado. Rain will likely return to the northern portion of the state for one of these days, but little to no accumulation is forecast. The image below just shows the area that will likely receive a little precipitation, but I&nbsp;have very low confidence&nbsp;that totals will reach 0.50 inches with the dry and abnormally strong system. Storms will also be moving quickly with the jet overhead, which will help to reduce totals. Expecting temperatures to reach near the triple digits on Sunday afternoon over the far eastern plains. So be sure to get in your afternoon activities on Saturday.<\/p>\n<p><img loading=\"lazy\" class=\"alignnone wp-image-12093\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/FTO_20200625_e2.png\" alt=\"\" width=\"880\" height=\"590\" srcset=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/FTO_20200625_e2.png 890w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/FTO_20200625_e2-300x201.png 300w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2020\/06\/FTO_20200625_e2-768x515.png 768w\" sizes=\"(max-width: 880px) 100vw, 880px\"\/><\/p>","protected":false},"excerpt":{"rendered":"<p>Issue Date: Thursday,&nbsp;June 25th, 2020 Issue Time: 1:30PM MDT Valid Dates:&nbsp;6\/26 &ndash; 7\/10 Event #1 continues tomorrow as 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> breaks off the main flow and begins to dig south over California. This will change the flow aloft to more westerly and release some mid-level energy into the state for additional afternoon lift. 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> [&hellip;]<\/p>","protected":false},"author":8,"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\/12046"}],"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\/8"}],"replies":[{"embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=12046"}],"version-history":[{"count":3,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/12046\/revisions"}],"predecessor-version":[{"id":12094,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/12046\/revisions\/12094"}],"wp:attachment":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=12046"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=12046"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=12046"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}