{"id":660,"date":"2015-06-01T13:46:50","date_gmt":"2015-06-01T19:46:50","guid":{"rendered":"https:\/\/www.coloradofloodthreat.com\/?p=660"},"modified":"2015-06-01T13:48:04","modified_gmt":"2015-06-01T19:48:04","slug":"fto-06-01-2015-the-transition-to-summer-is-underway","status":"publish","type":"post","link":"https:\/\/archive-coftb.dewberryanalytics.com\/?p=660","title":{"rendered":"FTO 06-01-2015: The Transition to Summer is Underway"},"content":{"rendered":"<p>Issue Date: 6\/1\/2015<br>\nIssue Time: 1:38 PM<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2015\/06\/06012015_ThreatTimeline.png\"><img loading=\"lazy\" class=\"  wp-image-658 aligncenter\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2015\/06\/06012015_ThreatTimeline.png\" alt=\"06012015_ThreatTimeline\" width=\"827\" height=\"113\"\/><\/a><\/p>\n<p>The transition to the summer season here in Colorado marks a particularly challenging time for forecasters. As low-pressure systems become fewer and further in between as compared to winter and spring, much of the forecasting reduces to a smaller, more individualized scale. The hot southwest United States ridge becomes a semi-permanent feature, with smaller disturbances attempting to break into that ridge. Only those disturbances, on average, will bring about an organized flood threat. During this 15 day period, there is only one such organized threat in which this FTO will be focused upon.<\/p>\n<ul><li>Event #1: Thursday (06-04-2015) through Tuesday (06-09-2015)\n<ul><li>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> (marked by the purple line) will deepen across the West Coast, increasing southwesterly flow across the state. While there is a lot of dry air out over the SW United States and nearby Pacific Ocean, one feature will attempt to allow deeper moisture to flow over Colorado. This feature is known as Hurricane Andres, and is circled in red. If, and only if, 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> can deepen and tap into the tropical moisture associated with Hurricane Andres, then an organized flood threat will develop. If not, dry, mid-level air will be driven over Colorado, reducing the flood threat to an individualized storm basis.<\/li>\n<\/ul><\/li>\n<\/ul><p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2015\/06\/06012015_WV.png\"><img loading=\"lazy\" class=\"  wp-image-659 aligncenter\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2015\/06\/06012015_WV.png\" alt=\"06012015_WV\" width=\"614\" height=\"410\"\/><\/a><\/p>\n<p>After the aforementioned 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> washes out, upper-level ridging is forecast to again build back in over Colorado, tapping into the dry air from the southwest. This will bring summer warmth right on schedule. How long this ridging and will last is the million dollar question. Current thinking is that the most likely outcome is the ridging will persist through the end of the period, since there aren&rsquo;t any notable disturbances coming down the storm track pipe. Be sure check daily on the Flood Threat Bulletin to stay up-to-date with the forecast.<\/p>\n<h3><strong>Event #1: Thursday (06-04-2015) through Tuesday (06-09-2015)<\/strong><\/h3>\n<p><em><span style=\"color: #ff6600;\">Elevated Flood Threat<\/span> on the Horizon, IF the Tropical Moisture can be Tapped<\/em><\/p>\n<p>The big question in this forecast is if the upper-level low can tap into the tropical moisture from Hurricane Andes. If it can, <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;precipitable water&lt;\/div&gt;&lt;div class=glossaryItemBody&gt;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\"}]'>precipitable water<\/span> values will climb to near an inch statewide, which will be in the 90th percentile for this time of year. That depth of moisture will make showers and thunderstorms efficient rainfall producers, bringing a heavy rain and <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> threat.<\/p>\n<p>At the same time, a surface low\/lee-side <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 develop across eastern Colorado early in the event period, helping to bring in low-level moisture from the Gulf of Mexico and upslope flow. It will be important to monitor the locations of fronts and drylines to determine where the strongest storms and heaviest rain will develop. These features\/associated fronts will exit Colorado over the weekend as the whole event winds down on Sunday-Monday-Tuesday.<\/p>\n<p>The precipitation map below depicts the outcome IF THE UPPER-LEVEL LOW CAN TAP INTO THE TROPICAL MOISTURE. If it cannot, then totals will be measurably less.<\/p>\n<p><iframe loading=\"lazy\" src=\"https:\/\/a.tiles.mapbox.com\/v4\/sgeiger.mbahm42g\/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>","protected":false},"excerpt":{"rendered":"<p>Issue Date: 6\/1\/2015 Issue Time: 1:38 PM The transition to the summer season here in Colorado marks a particularly challenging time for forecasters. As low-pressure systems become fewer and further in between as compared to winter and spring, much of the forecasting reduces to a smaller, more individualized scale. The hot southwest United States ridge [&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\/660"}],"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=660"}],"version-history":[{"count":4,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/660\/revisions"}],"predecessor-version":[{"id":664,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/660\/revisions\/664"}],"wp:attachment":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=660"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=660"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=660"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}