{"id":5189,"date":"2017-07-02T16:07:42","date_gmt":"2017-07-02T22:07:42","guid":{"rendered":"https:\/\/www.coloradofloodthreat.com\/?p=5189"},"modified":"2017-07-06T13:28:58","modified_gmt":"2017-07-06T19:28:58","slug":"fto-07-02-2017-relief-on-the-way-for-dry-western-slope-heat-persists-elsewhere","status":"publish","type":"post","link":"https:\/\/archive-coftb.dewberryanalytics.com\/?p=5189","title":{"rendered":"FTO 07-02-2017: Relief On The Way For Dry Western Slope; Heat Persists Elsewhere"},"content":{"rendered":"<p>Issue Date: Sunday, July 2nd, 2017<br>\nIssue Time: 4PM MDT<br>\nValid Dates: 7\/3-7\/17<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/threat_timeline.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-5192\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/threat_timeline.png\" alt=\"\" width=\"880\" height=\"100\"\/><\/a><\/p>\n<p>For almost all Flood Threat Outlooks, it is usually necessary to look far westward across the Pacific Ocean to get a heads up on Colorado&rsquo;s precipitation chances over the coming weeks. Interestingly, this is not the case during this 15-day Outlook. As can be seen in the water vapor image, below, the domain includes only a bit of the eastern Pacific. After the passage of a weak disturbance, identified as Event #1 that will bring light to moderate precipitation mainly for eastern areas, the atmospheric pattern becomes remarkably persistent. This is due to the development and migration of a blocking ridge to become situated along the Montana\/Saskatchewan border.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/wv_markup.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-5193\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/wv_markup.png\" alt=\"\" width=\"660\" height=\"410\"\/><\/a><\/p>\n<p>As can be seen in the long-range 500-mb height anomaly forecast, below, once this ridge sets up across southern Canada by later this week, it will move little over the next 7 or so days. In fact, there is a high degree of consistency across ensemble guidance (both GFS and ECMWF) that this will occur. With such a ridge position, significantly above average temperatures can be expected immediately under the anomalous ridge. However, Colorado will lie on its southern periphery meaning the temperature signal is weaker (although generally above average temperatures are expected throughout this entire Outlook period). The more notable impact of this ridge position is that it is far enough north to allow for the <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> of relatively moist easterly flow into southern Colorado, including 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>. This will certainly be welcome news for western slope residents who have been in a notable dry streak throughout most of June. This pattern resembles that of the desert southwest <span class=\"glossaryLink\" aria-describedby=\"tt\" data-cmtooltip=\"&lt;div class=glossaryItemTitle&gt;monsoon&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;a seasonal wind that brings moisture and rain to the region into which it blows; there is also a dry phase to monsoons, but popular usage refers only to the wet phase; these winds occur in many places around the world, and where they occur they are responsible for a majority of that location&rsquo;s annual precipitation&amp;lt;\/p&amp;gt;\n&amp;lt;!-- \/wp:paragraph --&amp;gt;&lt;\/div&gt;\" data-gt-translate-attributes='[{\"attribute\":\"data-cmtooltip\", \"format\":\"html\"}]'>monsoon<\/span>; but without distinct moisture surges, we avoid calling it as such for the time being.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/gfs_500hgt_anom.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-5190\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/gfs_500hgt_anom.png\" alt=\"\" width=\"660\" height=\"411\"\/><\/a><\/p>\n<p>Looking at the ensemble <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> forecast plumes, below, note the persistent increase in moisture at Grand Junction. By July 7<sup>th<\/sup>, the <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> is forecasted to finally get above average across western Colorado, for the first time in weeks. That is the good news. The bad news is that while <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> is a good predictor of precipitation <em>chances<\/em>, it is a rather poor predictor of precipitation amount. Thus, we have stayed conservative for this Outlook and have not posted an elevated flood threat for western Colorado yet, because at this time rainfall rates are expected to stay below flood intensity levels. However, given the persistence of the pattern, this may certainly change as the finer details become clearer during the next 3-5 days.<\/p>\n<p><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/pw_gefs.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-5191\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/pw_gefs.png\" alt=\"\" width=\"760\" height=\"263\"\/><\/a><\/p>\n<p>Below we describe each of the two identified precipitation events in more detail.<\/p>\n<h3><strong>Event #1: Monday (7\/3)<\/strong><\/h3>\n<p><span style=\"color: #0000ff;\"><strong>No Apparent Flood Threat<\/strong><\/span> as disturbance bring light rainfall across Colorado<\/p>\n<p>A weak disturbance will quickly move across Colorado on Monday morning, and will likely support some <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> shower and thunderstorm activity mainly across eastern areas. Storm motion will be relatively high, and moisture content will be marginal. Thus, flooding is not currently anticipated as rainfall is expected to stay below 0.75 inches.<\/p>\n<h3><strong>Event #2: Friday (7\/7) through Wednesday (7\/12)<\/strong><\/h3>\n<p><span style=\"color: #0000ff;\"><strong>No Apparent Flood Threat<\/strong><\/span> as moisture and precipitation chances finally increase for western slope<\/p>\n<p>A persistent pattern will bring easterly flow into southern Colorado, allowing for the return of moisture to the area. With plenty of morning sunshine expected daily, generating instability will not be an issue and <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> to <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> shower and storm activity is expected across southwest and southern Colorado. However, low level moisture supply currently looks to be marginal. Without organized disturbances, only popcorn thunderstorms are currently expected, generally yielding up to 0.5 inches of quick rainfall, but not much of a flood threat. Nonetheless, with such a prolonged event, total rainfall will add up over time, and over 1.5 inches is looking more likely for southwest Colorado. Wet soils could become an issue later in the event, which may necessitate an elevated flood threat. However, without knowledge of exact location, this is currently too speculative to act upon. Stay tuned!<\/p>\n<div style=\"position: relative;\"><a href=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/FTO_20170702_e2.png\"><img loading=\"lazy\" class=\"aligncenter wp-image-5253\" src=\"https:\/\/archive-coftb.dewberryanalytics.com\/wp-content\/uploads\/2017\/07\/FTO_20170702_e2.png\" alt=\"\" width=\"880\" height=\"497\"\/><\/a><\/div>\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: Sunday, July 2nd, 2017 Issue Time: 4PM MDT Valid Dates: 7\/3-7\/17 For almost all Flood Threat Outlooks, it is usually necessary to look far westward across the Pacific Ocean to get a heads up on Colorado&rsquo;s precipitation chances over the coming weeks. Interestingly, this is not the case during this 15-day Outlook. As [&hellip;]<\/p>","protected":false},"author":4,"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\/5189"}],"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=5189"}],"version-history":[{"count":3,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/5189\/revisions"}],"predecessor-version":[{"id":5254,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=\/wp\/v2\/posts\/5189\/revisions\/5254"}],"wp:attachment":[{"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=5189"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=5189"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/archive-coftb.dewberryanalytics.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=5189"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}