My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FLOOD10215
CWCB
>
Floodplain Documents
>
Backfile
>
9001-10000
>
FLOOD10215
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/26/2010 10:12:24 AM
Creation date
10/5/2006 5:00:14 AM
Metadata
Fields
Template:
Floodplain Documents
County
Statewide
Basin
Statewide
Title
1995 Colorado Flood Report
Date
1/1/1995
Prepared For
CWCB
Prepared By
CWCB
Floodplain - Doc Type
Floodplain Report/Masterplan
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
97
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
Show annotations
View images
View plain text
<br /> <br />. <br /> <br />IV. CLIMATIC FACTORS AND HYDROLOGY <br /> <br />Weather Of 1994-1995 <br /> <br />During the "winter" portion (November - March) of the winter of 1994-95, Pacific and <br />Arctic stonn tracks provided the Colorado mountains with generally mild weather. Typical <br />winter stonns from the Pacific area moved infrequently across the southern and central Colorado <br />mountains, causing a less than average snowpack to accumulate. Meanwhile, the central and <br />northern mountains and the eastern high plains received little snow accumulation from Arctic <br />stonns from Canada and Alaska <br /> <br />Then in April, particularly beginning in the middle of the month, it began snowing <br />frequently in the mountains and along the Front Range. A series of persistent stonns (snow <br />and/or rain) began to occur with regularity. These stonns depo~:ited healthy accumulations of <br />snow (and/or rain) every 4-5 days somewhere across the state_ The stonns lasted almost through <br />the second week of June. As the snowpack rose, the moisture content of the snow rose fastel, <br />since spring snowstonns are characteristically "wetter" than winter stonns. <br /> <br />The U.S.D.A. Natural Resources Conservation Service (NRCS) monitors snowpack in <br />Colorado's mountain watershed through a network that includes automated sites and sites that <br />require manual recording. At the beginning of each winter month the manual sites are visited <br />and statewide and basinwide snowpack figures are computed. On April I, 1995 the statewide and <br />basinwide figures (the percent of the 20-year average) were low to slightly above nonnal, as <br />shown below. <br /> <br />Table 1 <br /> <br />Location <br /> <br />Percent of Average <br />April I May 1 June I June 15 <br /> <br />South Platte River Basin 77 122 374 657 <br />Arkansas River Basin 112 183 338 628 <br />Rio Grande Basin 126 167 257 367 <br />Upper Colorado River Basin 106 132 304 413 <br />Gunnison River Basin 125 161 481 991 <br />Southwestern Colorado 125 159 334 405 <br />
The URL can be used to link to this page
Your browser does not support the video tag.