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30 minute streamflow data measured and computed for the irregular weir located at the Marshall Gultch catchment outlet (Santa Catalina Mountains,Arizona). Streamflow are derived using pressure measurements to infer water levels and hence discharge in the weir. Pressure is measured using Onset Hobo pressure transducers model U20.
15 minute discharge data measured and computed for the Seep located at the Marshall Gultch schist catchment (Santa Catalina Mountains,Arizona). Discharge is measured by directing the flow from a spring into a large custom made tipping bucket measuring 1 liter per tip. Data is logged using an Onset hobo pendant event datalogger.
|The following acknowledgment should accompany any publication or citation of these data - Logistical support and/or data were provided by the NSF-supported Jemez River Basin and Santa Catalina Mountains Critical Zone Observatory EAR-0724958 and EAR-1331408.
|Data for 2007-2012 were collected and computed by Ingo Heidbuechel, Graduate assistant, University of Arizona, firstname.lastname@example.org. From 2011, instrumentation is maintained and data are collected and computed by Nate Abramson, University of Arizona, email@example.com. Seep discharge measured in a 1L/tip tipping bucket, installed 7/1/2011 replacing the old v-notch weir. Data are provisional and may be subject to revision.
|Hydrology, Streamflow, Discharge, Seep, Marshall Gulch, Santa Catalina Mountains, Arizona
|Marshall Gulch Streamflow / Discharge Data
|This resource is referenced by
|Heidbüchel I., Troch P.A., Lyon S.W., and Weiler M. (2012). The master transit time distribution of variable flow systems. Water Resources Research 48(6): W06520 http://dx.doi.org/10.1029/2011WR011293
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This resource is shared under the Creative Commons Attribution CC BY.http://creativecommons.org/licenses/by/4.0/