Data and code for: Modeling Seasonal Effects of River Flow on Water Temperatures in an Agriculturally Dominated California River


Authors:
Owners: J. Eli Asarian
Type: Resource
Storage: The size of this resource is 1.0 GB
Created: Mar 08, 2021 at 6:35 p.m.
Last updated: Feb 05, 2024 at 2:01 p.m. (Metadata update)
Published date: Feb 14, 2023 at 9:32 p.m.
DOI: 10.4211/hs.a6653e2919964f9b840ec0340d86e11c
Citation: See how to cite this resource
Sharing Status: Published
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Abstract

This resource contains the data and scripts used for: Asarian, J.E., Robinson, C., Genzoli, L. 2023. Modeling Seasonal Effects of River Flow on Water Temperatures in an Agriculturally Dominated California River. Water Resources Research, e2022WR032915. https://doi.org/10.1029/2022WR032915.

Abstract from the article:
Low streamflows can increase vulnerability to warming, impacting coldwater fish. Water managers need tools to quantify these impacts and predict future water temperatures. Contrary to most statistical models’ assumptions, many seasonally changing factors (e.g., water sources and solar radiation) cause relationships between flow and water temperature to vary throughout the year. Using 21 years of air temperature and flow data, we modeled daily water temperatures in California’s snowmelt-driven Scott River where agricultural diversions consume most summer surface flows. We used generalized additive models to test time-varying and nonlinear effects of flow on water temperatures. Models that represented seasonally varying flow effects with intermediate complexity outperformed simpler models assuming constant relationships between water temperature and flow. Cross-validation error of the selected model was ≤1.2 °C. Flow variation had stronger effects on water temperatures in April–July than in other months. We applied the model to predict effects of instream flow scenarios proposed by regulatory agencies. Relative to historic conditions, the higher instream flow scenario would reduce annual maximum temperature from 25.2 °C to 24.1 °C, reduce annual exceedances of 22 °C (a cumulative thermal stress metric) from 106 to 51 degree-days, and delay onset of water temperatures >22 °C during some drought years. Testing the same modeling approach at nine additional sites showed similar accuracy and flow effects. These methods can be applied to streams with long-term flow and water temperature records to fill data gaps, identify periods of flow influence, and predict temperatures under flow management scenarios.

The files are organized into 6 folders: R_Scripts, SourceDataFiles, CompiledData, WorkingFiles, Outputs, and OtherStudies. Details of file are provided in the README.txt file.

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Klamath Basin, California, USA
North Latitude
41.8541°
East Longitude
-122.5939°
South Latitude
40.6565°
West Longitude
-123.9784°

Temporal

Start Date: 01/01/1998
End Date: 12/31/2020
Leaflet Map data © OpenStreetMap contributors

Content

    No files to display.

Related Geospatial Features

This HydroShare resource is linked to the following geospatial features

Related Resources

This resource is referenced by Asarian, J.E., and Robinson, C., Genzoli, L. 2023. Modeling Seasonal Effects of River Flow on Water Temperatures in an Agriculturally Dominated California River. Water Resources Research, e2022WR032915. https://doi.org/10.1029/2022WR032915

Credits

Funding Agencies

This resource was created using funding from the following sources:
Agency Name Award Title Award Number
Klamath Tribal Water Quality Consortium
U.S. Environmental Protecion Agency, Region IX

How to Cite

Asarian, J. E., C. Robinson, L. Genzoli (2023). Data and code for: Modeling Seasonal Effects of River Flow on Water Temperatures in an Agriculturally Dominated California River, HydroShare, https://doi.org/10.4211/hs.a6653e2919964f9b840ec0340d86e11c

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/
CC-BY

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