{"id":249,"date":"2015-05-05T11:01:46","date_gmt":"2015-05-05T17:01:46","guid":{"rendered":"https:\/\/www.coloradofloodthreat.com\/?p=249"},"modified":"2015-05-06T10:22:41","modified_gmt":"2015-05-06T16:22:41","slug":"stubborn-upper-level-low-to-continue-producing-showers-and-storms","status":"publish","type":"post","link":"https:\/\/archive-coftb.dewberryanalytics.com\/?p=249","title":{"rendered":"FTB 05-05-2015: Stubborn Upper-level Low To Continue Producing Showers and Storms"},"content":{"rendered":"<p>Issue Date: May 5th, 2015<br>\nIssue Time: 10:55 AM MDT<\/p>\n<p><em>&mdash; Low flood threat for Southeast Plains<br>\n&mdash; Low flood threat for Front Range and Urban Corridor<br>\n&mdash; Low flood threat for Northwest Slope, parts of Northern Mountains and parts of Grand Valley<br><\/em><\/p>\n<p>An impressive subtropical <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> over the eastern Tropical Pacific Ocean and western Mexico continues to send upper-level disturbances north and eastward across Colorado. As the water vapor image shows below, another feature is just entering the state as of this morning. North of this feature, marked by the dashed black line, a plume of moisture, cold upper-level temperatures and dynamical wind forcing will continue to support showers and thunderstorms across our state.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2015\/05\/WV_05052015.png\"><img loading=\"lazy\" class=\"  wp-image-251 aligncenter\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2015\/05\/WV_05052015.png\" alt=\"WV_05052015\" width=\"767\" height=\"432\"\/><\/a><\/p>\n<p>One difference from yesterday&rsquo;s weather setup is that cloud cover will be 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> and many areas may not see any sunshine at all. This is in contrast with yesterday, where areas along and south of the Palmer Ridge broke out of clouds, allowing temperatures to quickly jump into the mid-60s. The implication of today&rsquo;s reduced sunshine will be less instability. Thus, even though <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 remain quite high for this time of year, ranging from 0.7 in Boulder and Grand Junction to 0.8 in Pueblo, the lack of instability will be the main factor that will keep rain rates down. The one exception to this will be in the far eastern portion of the Southeast Plains, where sunshine may bolster temperatures late in the afternoon allowing for rainfall rates to approach 2.0 inches per hour.<\/p>\n<p>However, the combination of yesterday&rsquo;s <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> moderate to heavy rain amounts, elevated stream levels east 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> and today&rsquo;s steady rain rates of 0.4 to 0.7 inches will require a Low flood threat. Additionally, part of the Northern Mountains and Northwest Slope have been added to a Low flood threat because these areas are likely to experience the most sunshine today, raising temperatures and instability.<\/p>\n<p>Please see below for area-specific forecasts (click on &ldquo;About the FTB&rdquo; link above to view Colorado area-specific regions).<br><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2015\/05\/FTB_snapshot_20150505.png\"><img loading=\"lazy\" class=\"alignnone  wp-image-277\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2015\/05\/FTB_snapshot_20150505.png\" alt=\"FTB_snapshot_20150505\" width=\"799\" height=\"454\"\/><\/a><\/p>\n<h3><\/h3>\n<p>&nbsp;<\/p>\n<h3><strong>Zone-Specific Forecasts<\/strong><\/h3>\n<h4><strong>Urban Corridor, Front Range, Northeast Plains, Palmer Ridge, Southeast Plains, Southeast Mountains and Raton Ridge:<\/strong><\/h4>\n<p>Overcast with showers developing by early afternoon. Rain rates of 0.4 to 0.7 inches per hour will be possible across this entire area. In the far southeast portion of the Southeast Plains, more sunshine will cause strong to <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> <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> capable of producing rain rates up to 2 inches per hour. A low flood threat has been issued for parts of this area.<\/p>\n<h4><strong>Central Mountains, San Juan Mountains, San Luis Valley and Southwest Slope:<\/strong><\/h4>\n<p>Morning cloud cover partially break up leading to some sunshine. Rain rates up to 0.5 inches per hour will be possible later in the afternoon as some instability develops. No flood threat is expected.<\/p>\n<h4><strong>Northwest Slope, Grand Valley, and Northern Mountains: <\/strong><\/h4>\n<p>Morning showers 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> thunderstorms will expand in coverage and continue throughout the day. Rain rates will generally be less than 0.5 inches per hour, however later in the afternoon enough instability may allow for stronger thunderstorms with rain rates up to 0.9 inches per hour. A low flood threat has been posted for <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> <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>, debris slides and mud flows.<\/p>","protected":false},"excerpt":{"rendered":"<p>Issue Date: May 5th, 2015 Issue Time: 10:55 AM MDT &mdash; Low flood threat for Southeast Plains &mdash; Low flood threat for Front Range and Urban Corridor &mdash; Low flood threat for Northwest Slope, parts of Northern Mountains and parts of Grand Valley An impressive subtropical <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> over the eastern Tropical Pacific Ocean and [&hellip;]<\/p>","protected":false},"author":4,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":[],"categories":[6],"tags":[],"post_mailing_queue_ids":[],"_links":{"self":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/249"}],"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=249"}],"version-history":[{"count":12,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/249\/revisions"}],"predecessor-version":[{"id":278,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/249\/revisions\/278"}],"wp:attachment":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=249"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=249"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=249"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}