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WSP11333
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Last modified
1/26/2010 3:17:00 PM
Creation date
10/12/2006 4:54:38 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8273.100
Description
Colorado River Basin Salinity Control - Federal Agency Reports - BOR
Basin
Colorado Mainstem
Water Division
5
Date
5/1/1975
Title
Application of Stochastic Hydrology to Simulate Streamflow and Salinity in the Colorado River
Water Supply Pro - Doc Type
Report/Study
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<br /> <br />N <br />~ <br />-.J <br />~, <br /> <br />In the case of one variable depending on several others, stepwise <br />multiple regression is a valuable tool. This analysis proceeds <br />stepwise finding the least-squares relationship between the dependent <br />variable and the others in order of their contribution or effect. <br />This analysis indicates which variables are most important and should <br />be included in an equation. This is needed in the model to preserve <br />the relationships between stream gaging stations. <br /> <br />The spatial variation of the residual components controls the relation- <br />ship between high and low periods across basins, as well as among <br />stations within a single basin. Thus, a basin may be above average <br />on the whole, yet contain individual gaging stations with below- <br />normal flows. Also, one basin may be above normal while adjacent <br />basins are below normal. It should be clear that this type of spatial <br />variation in the randomness of streamflow can have a substantial <br />impact on the development, use, and management of the water resource <br />system. <br /> <br />To preserve the pattern of above- and below-normal relationships <br />between stations and basins, extensive analysis of correlations <br />between the random components was made. The residual series for <br />several stations were first inspected by a simple correlation matrix. <br />This matrix indicated the association between two stations by the <br />correlation coefficient of each pair. For example, two stations <br />which are concurrently above or below their normal flows might show <br />a high degree of dependence as seen by a correlation coefficient on <br />the order of 0.70 to perhaps 0.90. If two stations do not bekave <br />similarly, their residuals will not tend to follow high and low <br />values jointly. The correlation coefficient will be low (perhaps <br />0.00 to 0,30) and indicate the lack of dependence between them. <br /> <br />It should be emphasized that this correlation study was performed on <br />the residual values at each station after the mean, standard deviation, <br />and serial dependence properties have been removed. A large portion <br />of the correlation between total flow (the actual monthly value) is <br />due to the fact that the flow series are periodic. The periodic <br />structure of the time series representation used in the model preserves <br />this dependence between flow stations before any correlation is <br />explicitly investigated. By analyzing ;the relationship among the <br />residual series we are able to quantify the degree of association <br />between the abnormalities at neighboring stations. <br /> <br />Stepwise multiple regression was used to quantify the dependence <br />among stations. This analysis selects the most significant variables <br />in a relationship between a dependent variable and several possible <br />independent variables. It was decided to include a maximum of four <br />independent variables for the equation used in estimating the residual <br />values at each station. This equation is in the form of: <br /> <br />10 <br />
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