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Last modified
1/26/2010 12:33:55 PM
Creation date
10/11/2006 10:49:21 PM
Metadata
Fields
Template:
Water Supply Protection
File Number
8200.766
Description
Gunnison River General
State
CO
Basin
Gunnison
Water Division
4
Date
2/1/1988
Author
BOR
Title
East River Inflows - Upper Gunnison-Uncompahgre Basin - Model Inflow Development
Water Supply Pro - Doc Type
Report/Study
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<br />e <br /> <br />e <br /> <br />e <br /> <br />1) l) ,_ 2 fl4 <br /> <br />Station Name <br />Tomichi Creek <br />at Gunnison <br /> <br />Table 13 <br />Adjusted and unadjusted virgin flow core files <br />(Tomichi Creek above Tomichi Creek at Gunnison) <br />Unadjusted <br />Flow File <br />VG19000 <br /> <br />Adjusted <br />Flow File <br />VJ19000. <br /> <br />Tomichi Creek <br />at Parlin <br /> <br />TOM2C <br /> <br />TOM 2 <br /> <br />Quartz Creek <br />near Ohio <br /> <br />VJ18000 <br /> <br />VGIBOOO <br /> <br />Cochetopa Creek <br />near Parlin <br />* Base station. <br /> <br />VG18500 <br /> <br />VJ18500 <br /> <br />Copies of adjusted virgin flow core station files are given in <br /> <br />Appendix D, <br /> <br />Inflow Development <br />for INFL5 - INFL51 <br /> <br />Two sets of virgin flow estimates for model inflow points in the Upper <br /> <br />Gunnison Basin (INFL5 - INFL51) were derived usiqg unadjusted and adjusted <br /> <br />core station virgin flow estimates, The general methodology for inflow <br /> <br />development used elevation/yield and area proportioniqg techniques. Core <br /> <br />station long-term yields [from 1952-1983] were used to derive elevation/yield <br /> <br />curves, Estimates of 1952-1983 yields for subbasin inflows were taken from <br /> <br />these curves, Annual and monthly flow estimates of subbasin inflows were <br /> <br />developed by distributing the loqg-term yield as taken from the <br /> <br />elevation/yield curve in the same proportions as annual and monthly flows of <br /> <br />the core station, <br /> <br />Where data was available, monthly distribution factors were applied to <br /> <br />core station values to obtain distributions which better represented subbasin <br /> <br />areas. <br /> <br />24 <br />
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