{"id":16596,"date":"2022-05-05T15:01:10","date_gmt":"2022-05-05T21:01:10","guid":{"rendered":"https:\/\/www.coloradofloodthreat.com\/?p=16596"},"modified":"2022-05-09T12:39:13","modified_gmt":"2022-05-09T18:39:13","slug":"fto-05-05-2022-a-shot-of-moisture-early-then-warmth-in-the-east-and-a-chill-in-the-west-precipitation-uncertain-until-late-next-week","status":"publish","type":"post","link":"https:\/\/archive-coftb.dewberryanalytics.com\/?p=16596","title":{"rendered":"FTO 05-05-2022: A Shot Of Moisture Early, Then Warmth In The East With A Chill In The West; Precipitation Uncertain Until Late Next Week"},"content":{"rendered":"<p>Issue Date: Thursday, May 5th, 2022<br>\nIssue Time: 3PM MDT<br>\nValid Dates: May 6 &ndash; May 20<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/threat_timeline-1.png\"><img loading=\"lazy\" class=\"alignnone size-large wp-image-16598\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/threat_timeline-1-1024x171.png\" alt=\"\" width=\"910\" height=\"152\" srcset=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/threat_timeline-1-1024x171.png 1024w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/threat_timeline-1-300x50.png 300w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/threat_timeline-1-768x128.png 768w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/threat_timeline-1.png 1196w\" sizes=\"(max-width: 910px) 100vw, 910px\"\/><\/a><\/p>\n<p>The change in the longer-range precipitation forecast since Monday&rsquo;s Outlook is one of the more extreme examples of forecast uncertainty. At that time, consensus across many models, &nbsp;in consistency with spring climatology, suggested the likelihood of 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> developing over the western United States. This would promote dynamical support for upward motion across Colorado, as well as southerly 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> from the Gulf of Mexico and\/or eastern subtropical Pacific. In short, precipitation chances looked quite promising.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/wv_markup-1.png\"><img loading=\"lazy\" class=\"alignnone size-full wp-image-16599\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/wv_markup-1.png\" alt=\"\" width=\"1000\" height=\"676\" srcset=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/wv_markup-1.png 1000w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/wv_markup-1-300x203.png 300w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/wv_markup-1-768x519.png 768w\" sizes=\"(max-width: 1000px) 100vw, 1000px\"\/><\/a><\/p>\n<p>Fast forward to today, the water vapor image, below, still shows a very active central Pacific jet. This tends to promote an &ldquo;amplified&rdquo; pattern on the eastern side of the <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;jet stream&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;Relatively strong winds concentrated within a narrow stream in the atmosphere. General weather patterns are related closely to the position, strength and orientation of the jet stream.&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>jet stream<\/span>, and there is still strong indication of 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> developing. The problem is 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> will likely be far enough west to have little affect on Colorado through the end of next week. Instead, after a fairly minor precipitation event over the weekend (Event #1), the state will enter a relatively dry stretch. The formation of the 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> will be close enough to us to promote cooler temperatures 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>. However, to the east, especially in the Northeast and Southeast Plains, warm (perhaps hot?) weather is expected with little to no rainfall.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/gefs_plumes.png\"><img loading=\"lazy\" class=\"alignnone size-large wp-image-16597\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/gefs_plumes-1024x367.png\" alt=\"\" width=\"910\" height=\"326\" srcset=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/gefs_plumes-1024x367.png 1024w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/gefs_plumes-300x107.png 300w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/gefs_plumes-768x275.png 768w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/gefs_plumes.png 1464w\" sizes=\"(max-width: 910px) 100vw, 910px\"\/><\/a><\/p>\n<p>As shown in the forecast <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 GEFS, there is some indication of potential moisture being imported from the southern Great Plains by the end of next week. Note how this only shows up in the Denver sounding, a hint to the moisture&rsquo;s origin. However, the model consensus is rather poor at this time and will depend largely on the ability of the 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> to stay intact for a whole week (a long time in the forecasting world!). Thus, while we do anticipate a return to precipitation by late next week, there is No Apparent Flood threat at this time.<\/p>\n<p>With temperatures running near seasonal normal over the higher terrain, snowmelt is expected to proceed at a slow-to-moderate pace. Friday and Saturday will see a pulse of melt especially over southern and central Colorado, but cooler temperatures thereafter should temper additional melt to its seasonal normal rate. A look at major river basins across the state shows the snowmelt has started in earnest for the Rio Grand, San Juan\/Los Pinos\/Animas and Dolores basins. However, the snowpack is still holding for the Gunnison, Upper Colorado and White\/Yampa basins 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>. To the east, the North Platte, South Platte and Arkansas basins are still yet to see their spring pulse of water. In Monday&rsquo;s Outlook, we will release our first statewide streamflow tracker to provide some actual flow numbers, so stay tuned!<\/p>\n<p>The two identified precipitation events are described in more detail below.<\/p>\n<h4><strong>Event #1: Saturday &ndash; Monday (May 7 &ndash; May 9)<\/strong><\/h4>\n<p><strong>Minor Rain and Snow Event for mainly the Northern Mountains; <span style=\"color: #0000ff;\">No Apparent Flood Threat<\/span><\/strong><\/p>\n<p>A small disturbance will bring a pulse of moisture for mainly northern Colorado resulting in a 36-48 hour period of rain and higher-elevation snow showers for the Northwest Slope, Northern Mountains and parts of the Front Range. Up to 0.5 inches of liquid equivalent is expected for the highest favored peaks, so a precipitation map is not provided.<\/p>\n<h4><strong>Event #2: Thursday &ndash; Sunday (May 12 &ndash; May 15)<\/strong><\/h4>\n<p><strong>Precipitation Chances To Increase, But <span style=\"color: #0000ff;\">No Apparent Flood Threat<\/span> Due To Uncertainty<\/strong><\/p>\n<p>The approach of the 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>, in a strength yet to be determine, is still likely to promote a more active precipitation pattern for Colorado. At this time, it appears that moisture will be generally lacking. The most likely areas to experience precipitation above 0.5 inches are the climatologically favored Front Range and Urban Corridor as well as the Northeast Plains. In terms of heavy rainfall potential, it looks to be confined to the immediate KS border and eastward at this time. Precipitation above 1 inch is not expected with this event as of right now.<\/p>\n<p><img loading=\"lazy\" class=\"aligncenter wp-image-16674\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/FTO_20220505_e2_jpeg.jpg\" alt=\"\" width=\"880\" height=\"594\" srcset=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/FTO_20220505_e2_jpeg.jpg 1776w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/FTO_20220505_e2_jpeg-300x202.jpg 300w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/FTO_20220505_e2_jpeg-1024x691.jpg 1024w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/FTO_20220505_e2_jpeg-768x518.jpg 768w, https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2022\/05\/FTO_20220505_e2_jpeg-1536x1036.jpg 1536w\" sizes=\"(max-width: 880px) 100vw, 880px\"\/><\/p>","protected":false},"excerpt":{"rendered":"<p>Issue Date: Thursday, May 5th, 2022 Issue Time: 3PM MDT Valid Dates: May 6 &ndash; May 20 The change in the longer-range precipitation forecast since Monday&rsquo;s Outlook is one of the more extreme examples of forecast uncertainty. At that time, consensus across many models, &nbsp;in consistency with spring climatology, suggested the likelihood of a large-scale [&hellip;]<\/p>","protected":false},"author":4,"featured_media":0,"comment_status":"closed","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\/16596"}],"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=16596"}],"version-history":[{"count":7,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/16596\/revisions"}],"predecessor-version":[{"id":16675,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/16596\/revisions\/16675"}],"wp:attachment":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=16596"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=16596"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=16596"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}