The Importance of Incorporating Diurnally Fluctuating Stream Discharge in Stream Temperature Energy Balance Models

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Created: Mar 07, 2018 at 5:10 p.m.
Last updated: May 22, 2018 at 10:40 p.m.
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HFLUX input data used to run the diurnally fluctuating streamflow base case model discussed in Baker et al. (2018), "The Importance of Incorporating Diurnally Fluctuating Stream Discharge in Energy Balance Models to Determine Groundwater Inflow Rates". The HFLUX model can be downloaded from, where additional information on the model structure and inputs is located. The 18 excel sheets include the model settings, time steps, distance steps, temperature boundary conditions in space and time, stream channel geometry, discharge data, groundwater temperatures averaged from 5 wells, weather data, average stream bed temperatures and the depth at which they were measured, sediment time, shade and cloud data, site latitude, longitude, and elevation, and the calibrated stream temperatures through space and time over a ~1.2 km reach over a ~5 day period.

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Resource Level Coverage


Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Quilcayhuanca Valley, Peru


Start Date:
End Date:


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Model Output
Includes output files? No

Executed By
Name Unspecified


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Funding Agencies

This resource was created using funding from the following sources:
Agency Name Award Title Award Number
National Science Foundation EAR- 1316429
National Science Foundation DGE-1449617


People or Organizations that contributed technically, materially, financially, or provided general support for the creation of the resource's content but are not considered authors.

Name Organization Address Phone Author Identifiers
Bryan Mark The Ohio State University
Lauren Somers McGill University

How to Cite

Baker, E., L. Lautz, C. Kelleher, J. McKenzie (2018). The Importance of Incorporating Diurnally Fluctuating Stream Discharge in Stream Temperature Energy Balance Models, HydroShare,

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


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