Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...
This resource contains some files/folders that have non-preferred characters in their name. Show non-conforming files/folders.
This resource contains content types with files that need to be updated to match with metadata changes. Show content type files that need updating.
Authors: |
|
|
---|---|---|
Owners: |
|
This resource does not have an owner who is an active HydroShare user. Contact CUAHSI (help@cuahsi.org) for information on this resource. |
Type: | Resource | |
Storage: | The size of this resource is 1.6 KB | |
Created: | Feb 07, 2023 at 7:05 p.m. | |
Last updated: | Feb 07, 2023 at 7:05 p.m. | |
Citation: | See how to cite this resource |
Sharing Status: | Public |
---|---|
Views: | 595 |
Downloads: | 212 |
+1 Votes: | Be the first one to this. |
Comments: | No comments (yet) |
Abstract
Water managers in the Santa Rosa Plain face the challenge of meeting increasing water demand with a combination of Russian River water, which has uncertainties in its future availability; local groundwater resources; and ongoing and expanding recycled water and water from other conservation programs. To address this challenge, the U.S. Geological Survey, in cooperation with the Sonoma County Water Agency, the cities of Cotati, Rohnert Park, Santa Rosa, and Sebastopol, the town of Windsor, the California American Water Company, and the County of Sonoma, undertook development of a fully coupled groundwater and surface-water model to better understand and to help manage the hydrologic resources in the Santa Rosa Plain watershed. The purpose of this report is to (1) describe the construction and calibration of the fully coupled groundwater and surface-water flow model for the Santa Rosa Plain watershed, referred to as the Santa Rosa Plain hydrologic model; (2) present results from simulation of the Santa Rosa Plain hydrologic model, including water budgets, recharge distributions, streamflow, and the effect of pumping on water-budget components; and (3) present the results from using the model to evaluate the potential hydrologic effects of climate change and variability without pumpage for water years 2011-99 and with projected pumpage for water years 2011-40.
Subject Keywords
Coverage
Spatial
Content
Additional Metadata
Name | Value |
---|---|
DOI | 10.3133/sir20145052 |
Depth | 625 |
Scale | 101 - 1 000 km² |
Layers | 6-10 layers |
Purpose | Groundwater resources |
GroMoPo_ID | 90 |
IsVerified | True |
Model Code | MODFLOW |
Model Link | https://doi.org/10.3133/sir20145052 |
Model Time | 2011–2099 |
Model Year | 2014 |
Model Authors | L.R. Woolfenden, T. Nishikawa |
Model Country | United States |
Data Available | Report/paper only |
Developer Email | lrwoolfe@usgs.gov |
Dominant Geology | Model focuses on multiple geologic materials |
Developer Country | USA |
Publication Title | Simulation of groundwater and surface-water resources of the Santa Rosa Plain watershed, Sonoma County, California |
Original Developer | No |
Additional Information | |
Integration or Coupling | Surface water |
Evaluation or Calibration | Static water levels;Dynamic water levels |
Geologic Data Availability |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
Comments
There are currently no comments
New Comment