{"id":2337,"date":"2016-05-12T12:52:09","date_gmt":"2016-05-12T18:52:09","guid":{"rendered":"https:\/\/www.coloradofloodthreat.com\/?p=2337"},"modified":"2016-05-12T12:52:09","modified_gmt":"2016-05-12T18:52:09","slug":"fto-05-12-2016-two-events-one-elevated-flood-threat","status":"publish","type":"post","link":"https:\/\/archive-coftb.dewberryanalytics.com\/?p=2337","title":{"rendered":"FTO 05-12-2016: Two Events, One Elevated Flood Threat"},"content":{"rendered":"<p>Issue Date: 5\/12\/2016<br>\nIssue Time: 12:50 PM<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2016\/05\/Threat_Timeline_20160512.png\"><img loading=\"lazy\" class=\"  wp-image-2338 aligncenter\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2016\/05\/Threat_Timeline_20160512.png\" alt=\"Threat_Timeline_20160512\" width=\"890\" height=\"121\"\/><\/a><\/p>\n<p>Right on cue, the ridging that has dried out Colorado today, and will tomorrow, is forecast to begin breaking down on Saturday and allow for the reintroduction of showers and thunderstorms. Event #1 (denoted by the purple #1 on the water vapor image below) is riding on the heels of this ridge, and will begin to push onshore the West Coast by Saturday afternoon. This movement will bring moist, southwesterly flow across Colorado, helping to fuel afternoon and evening showers\/thunderstorms across the higher terrain and over the adjacent eastern plains. Sunday afternoon\/evening will be when Event #1 really kicks into gear, as the 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> encroaches on Colorado. Overall, this <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> (while being reinforced\/rounded by other disturbances) will influence our weather through Thursday morning before ridging takes over, bringing another short drying trend.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2016\/05\/WV_20160512.png\"><img loading=\"lazy\" class=\"  wp-image-2339 aligncenter\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2016\/05\/WV_20160512.png\" alt=\"WV_20160512\" width=\"565\" height=\"376\"\/><\/a><\/p>\n<p>Event #2 will establish its influence on Colorado next Saturday (5\/21) as moist, southwesterly flow increases as it comes onshore the West Coast. As it comes onshore, it is forecast to stall over the West Coast, and complicate the forecast scenario during the remainder of this FTO period. At times, in response to the more-or-less blocked nature of the 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>\/low, a couple surface lows will develop along the leeside of the Northern Rockies. The placement of these surface lows and their boundaries (cool front\/<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 be important to identify. There are a couple of scenarios that could play out:<\/p>\n<ol><li>The cool front\/<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> placement keeps the best low-level moisture east of Colorado, limiting the amount of thunderstorm activity, especially across the lower elevations of eastern Colorado<\/li>\n<li>Ample low-level moisture is available, helping to increase instability values, and the boundaries are placed well to provide low-level <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;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\"}]'>shear<\/span> that can support strong-to-<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<\/li>\n<li>The most likely scenario is a mixture of the two above scenarios, with days of drying mixed with days of thunderstorms. It will be late May in Colorado, and climatology lends support to this solution.<\/li>\n<\/ol><p>Meanwhile, the southwesterly flow aloft will rotate ribbons of moisture across the region, bringing <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>-to-<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> showers\/thunderstorms to the higher terrain whenever moisture moves overhead. This portion of the forecast period is far from settled, so please check back on Monday for the next FTO edition for an update.<\/p>\n<h3><strong>Event #1: Saturday (05-14-2016) through Thursday Morning (05-19-2016)<\/strong><\/h3>\n<p><em><span style=\"color: #ff6600;\">Elevated Flood Threat<\/span> during Extended Wet Period<\/em><\/p>\n<p>Upper-level ridging will begin to break down on Saturday and allow for the reintroduction of showers and thunderstorms. Concurrently, the upper-level low will push onshore the West Coast by Saturday afternoon. This setup will bring moist, southwesterly flow across Colorado, helping to fuel afternoon and evening showers\/thunderstorms across the higher terrain and over the adjacent eastern plains on Saturday. For Sunday afternoon\/evening, the 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> will start to encroach on Colorado, increasing the number of showers\/thunderstorms. At the same time, easterly flow will develop to the east of the mountains, reinforcing low-level moisture through Tuesday.<\/p>\n<p>Overall, this <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> (while being reinforced\/rounded by other disturbances) will influence our weather through Thursday morning before ridging takes over, bringing another short drying trend. The wettest days, generally speaking, will be Sunday &ndash; Tuesday, thanks to the aforementioned easterly flow and reinforcement of moisture.<\/p>\n<p><iframe loading=\"lazy\" src=\"https:\/\/a.tiles.mapbox.com\/v4\/sgeiger.044dl108\/attribution,zoompan,zoomwheel,geocoder,share.html?access_token=pk.eyJ1Ijoic2dlaWdlciIsImEiOiJmNjc5a3RBIn0.LbLupVkJsS5dbo9fsgrTDg\" width=\"100%\" height=\"500px\" frameborder=\"0\"><\/iframe><\/p>\n<p><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><\/p>\n<h3><strong>Event #2: Saturday (05-21-2016) through Friday (05-27-2016)<\/strong><\/h3>\n<p><span style=\"color: #0000ff;\"><em>No Apparent Flood Threat<\/em><\/span><\/p>\n<p>A couple of scenarios could play out, as mentioned above in the main discussion. The most likely of which is a mixture of days with more sunshine and <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> showers\/thunderstorms (mainly over the higher terrain) and days with more <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> showers\/thunderstorms, some potentially strong-to-severe. Climatologically speaking, that&rsquo;s late May in a nutshell. The stalling\/blocked upper-level low\/<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> complicates the forecast, making this period as clear as mud. Due to this, no precipitation map will be drawn. Stay tuned to the next FTO on Monday for an update on this period.<\/p>","protected":false},"excerpt":{"rendered":"<p>Issue Date: 5\/12\/2016 Issue Time: 12:50 PM Right on cue, the ridging that has dried out Colorado today, and will tomorrow, is forecast to begin breaking down on Saturday and allow for the reintroduction of showers and thunderstorms. Event #1 (denoted by the purple #1 on the water vapor image below) is riding on the [&hellip;]<\/p>","protected":false},"author":1,"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\/2337"}],"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=2337"}],"version-history":[{"count":1,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/2337\/revisions"}],"predecessor-version":[{"id":2340,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/2337\/revisions\/2340"}],"wp:attachment":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=2337"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=2337"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=2337"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}