Description Usage Format Details Source
A dataset containing the diverted flow in cfs within watersheds for use with the CVPIA SIT Salmon Population Model.
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dataframe with 985 rows and 32 variables:
CALSIM II date
D104
(C11307 / (C11307 + C11308 + C11309) * D11305)
no modeled diversions
no modeled diversions
no modeled diversions
(C217B + D217)
no modeled diversions
no modeled diversions
no modeled diversions
(C11309 / (C11307 + C11308 + C11309) * D11305)
(C11303 / (C11303 + C11304) * D11301)
(C11308 / (C11307 + C11308 + C11309) * D11305)
no modeled diversions
D17301
(C11304 / (C11303 + C11304) * D11301)
(D109 + D112 + D113A + D113B + D114 + D118 + D122A + D122B + D123 + D124A + D128_WTS + D128)
no modeled diversions
D285
(D201 + D202 + D7A + D7B)
D230
(D129A + D134 + D162 + D165)
no modeled diversions
D302
(D167 + D168 + D168A_WTS)
(D506A + D506B + D506C + D507)
no modeled diversions
(D503A + D503B + D503C + D502A + D502B)*
(D562 + D566)
D528
D545
(D637 + D630B + D630A + D620B)
The proportion diverted was calculated using 'FLOW-CHANNEL' and 'FLOW-DELIVERY' nodes from CALSIM II. The nodes and calculation for each watershed are outlined above.
The diversions of Antelope Creek, Deer Creek and Mill Creek are represented by one diversion node. Diversions for these creeks were estimated in proportion to their flow. Elder Creek and Thomes Creek are also represented with a single node and their diversions were estimated using the same method.
*Mokelumne River flow and diversions are from a separate model provided by EBMUD.
Data Wrangling: Sadie Gill sgill@flowwest.com
Node Selection: Mark Tompkins mtompkins@flowwest.com and Mike Urkov mike.urkov@gmail.com
CALSIM Model Output: Michael Wright mwright@usbr.gov
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