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Upper Los Angeles River Area Annual Report  10/01/2015 - 09/30/2016

Watermaster Information

Upper Los Angeles River Area 4-12 SAN FERNANDO VALLEY
City of Los Angeles vs. City of San Fernando, et. al. 650079 01/26/1979
Upper Los Angeles River Area (ULARA) Watermaster, c/o Richard C. Slade & Associates LLC 14051 Burbank Blvd, Ste 300 Sherman Oaks CA
info@ularawatermaster.com (818) 506-0418 91401
Richard Slade
slade@ularawatermaster.com
City of LA vs. City of San Fernando et al. JUDGEMENT.pdf (1.5MB)
ULARA Adjudicated Bounadries.zip (113.3kB)
http://ularawatermaster.com/
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A

Groundwater Level

Is water level data submitted to the CASGEM Program?
Yes
Does this watermaster collect or receive additional groundwater levels?
No
Does this watermaster measure groundwater levels?
No
Comment(s)
Groundwater elevation data is submitted pursuant to Water Code section 10932, therefore no additional groundwater level data is required. Water Code § 10720.8(f)(3)(A). 
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B

Groundwater Use

Reporting Period
From 10/01/2015 To 09/30/2016 
Total Annual Groundwater Extraction (AF)
Method used to determine extraction (if available):
  Volume (AF) Explanation Uncertainty
Groundwater Extraction by water use sector (if available):
Sector Volume (AF) Explanation Uncertainty
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C

Surface Water Use

Reporting Period
From 10/01/2015 To 09/30/2016 
Surface Water Supply (AF)
Method used to determine
 
Uncertainty
Medium 
Water available for recharge or in-lieu use by source type (if available):
  Volume (AF) Explanation Uncertainty
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D

Total Water Use

Reporting Period
From 10/01/2015 To 09/30/2016 
Total Water Use (AF)
Method used to determine
Summation of Metered Flows 
Uncertainty
Low 
Total water Use by water use sector (if available)
  Volume (AF)
Water use met by source type
Type Volume (AF)
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E

Change in GW Storage

Reporting Period
From 10/01/2015 To 09/30/2016 
Change in storage (AF)
Method used to determine
Reported change in storage is a summation of the change in storage calculated for each of the four ULARA groundwater basins. In the San Fernando Basin, the change in the storage is estimated by calculation using the measured change in groundwater elevations from multiple monitoring wells distributed throughout each basin using methodology similar to the methodology described in the Report of Referee. Then, the existing groundwater flow model developed for the San Fernando Basin is qualitatively used to corroborate the magnitude of the calculated change in storage. In the Verdugo, Sylmar, and Eagle Rock basins, the change in storage value is determined by calculation using the measured change in water levels in the basin (depending on the availability of sufficient water level data from monitoring wells), or by calculation using the annual native safe yield published in the Report of Referee compared to the groundwater extracted during the Water Year. 
Uncertainty
Medium 
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F

Required Documents

Reporting Period
From 10/01/2015 To 09/30/2016 
Please submit an electronic (PDF preferred) copy of your annual report.
WY2015-16-ULARA-WM-Rpt-12-2017.pdf (19.4MB) Uploaded on 07/27/2018 at 09:14AM
 
Please submit additional reports or documents.