My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
WSPC01844
CWCB
>
Water Supply Protection
>
Backfile
>
14000-14999
>
WSPC01844
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
7/29/2009 8:03:12 AM
Creation date
10/9/2006 3:02:55 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8283.200
Description
Colorado River Basin-Colorado River Computer Models-Colorado River Decision Support System-Ray
State
CO
Water Division
5
Date
7/13/1994
Title
Consumptive Use Modeling-Task 1.14b-Consumptive Use Prototype Development-Phase Iia
Water Supply Pro - Doc Type
Report/Study
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
14
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 />'0 u rJ 3 9 <br />Task 1.14(b) - Consumptive Use Prototype Development <br /> <br />Climate Characteristics i:..... <br />The amount of precipitation is important for determining the amount of irriga~ <br />water plants will consume. Knowing just the amount of precipitation is not enough, <br />the effective precipitation is the actual amount of precipitation used by plants and it <br />may depend on a host of factors not related to precipitation. In practice, effective ...-? <br />precipitation is the amount of water not needed from irrigation sources. <br /> <br />Temperature partly determines the evaporation and transpiration rates of agricultural <br />lands as well as the length of the growing season. Abnormally low temperatures may <br />retard plant growth and unusually high temperatures can produce dormancy. The <br />growing season is usually considered to be the period between killing frosts, though <br />for some plants the beginning of the growing season may come after the frosts and/or <br />the end of the season may be well before the fall frosts. <br /> <br />Latitude differences change the daily amount and seasonal duration of sunlight <br />available for crop growth. Higher northern latitudes experience much longer days in <br />the summer then in the winter. <br /> <br />Other climatic parameters that have an effect on the amount of irrigation water <br />consumed by plants includes relative humidity and wind movement. Hot dry winds <br />can significantly increase the rates of evaporation and transpiration especially in arid <br />and semi-arid climates. <br /> <br />Water Supply <br />Naturally, unless water is available from precipitation, groundwater, or irrigation <br />there can not be consumptive use from crops. In areas of the arid and semi-arid West <br />such as the Western Slope of Colorado the major source of water is irrigation. In these <br />areas the quantity and seasonal distribution of the available water supply will effect the <br />consumptive use characteristics of agricultural lands. Some studies have shown that <br />beside the quantity and seasonal distribution of the water supply, the quality of the <br />water also has an effect of consumptive use. Where soil salinity has begun decreasing <br />yields water supply might be increased to lower the salt concentration to the root zone. <br /> <br />Plant Growth Characteristics <br />The stage of a crop's growth has a very considerable influence on its rate of <br />consumptive use. This is particularly true for annual crops which generally have three <br />distinct stages of growth. These stages are the emergence and development of <br />complete vegetative cover characterized by the consumptive use rapidly increasing <br />from a low value to approaching its maximum value, the period of maximum <br />vegetative cover during which time the consumptive use will be near its maximum as <br />long as the water supply is available, and finally the maturation stage where, for most <br />crops, the consumptive use begins to decrease. <br /> <br />Effective Rainfall l"'l'~ <br />By definition, effective rainfall must,.a portion of a crop's water requirement, since it )0 <br />does not include water lost to surface runoff and/or deep percolation. Effective rainfall <br />is typically estimated from total rainfall for which data is available. The percentage of <br />total rainfall that is effective rainfall depends on soil conditions and climatic factors. In <br />arid areas where the total growing season precipitation is light and the soil profile is <br /> <br />7/13/94 - Draft of Task Memorandum <br /> <br />3 <br /> <br />IDS Group, CSU <br />
The URL can be used to link to this page
Your browser does not support the video tag.