Analysis of hydrologic data collected by the U.S. Bureau of Land Management 1987-1995 and recommendations for future monitoring programs
| dc.contributor.author | Sharma, Vandana | |
| dc.contributor.author | Mac Nish, Robert D. | |
| dc.contributor.author | Maddock, Thomas, III | |
| dc.date.accessioned | 2016-07-08T00:03:07Z | |
| dc.date.available | 2016-07-08T00:03:07Z | |
| dc.date.issued | 1997 | |
| dc.identifier.uri | http://hdl.handle.net/10150/615797 | |
| dc.description.abstract | The purpose of this study was to establish a more efficient monitoring program for the San Pedro Riparian National Conservation Area (SPRNCA). This report analyzes data on stream flow measurements taken at nine locations on the San Pedro river and one location on the Babocomari river and ground water levels in eighteen wells collected by the BLM over the period from 1987 to 1995 and discusses possible causes for trends and anomalies in the data. The report also recommends future data collection and analytical efforts. All of the stream discharge data and some of the groundwater levels were collected at discrete and unsystematic intervals, and further, the streamflow measurements may not have been collected at the same location at each site. Surface water flow was measured by a Marsh- McBirney flow meter. | |
| dc.description.sponsorship | The investigation described in this report was performed with the financial support of the U. S. Bureau of Land Management (BLM). The findings and conclusions presented in this report are those of the authors, and do not necessarily reflect the positions of the BLM. The authors are indebted to the staff at the Bureau of Land Management office in Sierra Vista, and in particular to Ben Lomeli who spent a considerable amount of time in assembling the data that had been collected in the San Pedro Riparian National Conservation Area. Thanks are also due to Christopher Smith of the Arizona District Office of the U. S. Geological Survey for assistance with retrieving the USGS flow data for the Charleston stream gage. We also greatly appreciate the review comments provided by Howard F. McCormack of the U. S. Geological Survey. | en |
| dc.language.iso | en_US | en |
| dc.publisher | Department of Hydrology and Water Resources, University of Arizona (Tucson, AZ) | en |
| dc.relation.ispartofseries | Technical Reports on Hydrology and Water Resources, No. 97-060 | en |
| dc.rights | Copyright © Arizona Board of Regents | en |
| dc.source | Provided by the Department of Hydrology and Water Resources. | en |
| dc.title | Analysis of hydrologic data collected by the U.S. Bureau of Land Management 1987-1995 and recommendations for future monitoring programs | en_US |
| dc.type | text | en |
| dc.type | Technical Report | en |
| dc.contributor.department | Department of Hydrology & Water Resources, The University of Arizona | en |
| dc.contributor.department | Arizona Research Laboratory for Riparian Studies | en |
| dc.description.collectioninformation | This title from the Hydrology & Water Resources Technical Reports collection is made available by the Department of Hydrology & Atmospheric Sciences and the University Libraries, University of Arizona. If you have questions about titles in this collection, please contact repository@u.library.arizona.edu. | en |
| refterms.dateFOA | 2018-06-11T14:12:41Z | |
| html.description.abstract | The purpose of this study was to establish a more efficient monitoring program for the San Pedro Riparian National Conservation Area (SPRNCA). This report analyzes data on stream flow measurements taken at nine locations on the San Pedro river and one location on the Babocomari river and ground water levels in eighteen wells collected by the BLM over the period from 1987 to 1995 and discusses possible causes for trends and anomalies in the data. The report also recommends future data collection and analytical efforts. All of the stream discharge data and some of the groundwater levels were collected at discrete and unsystematic intervals, and further, the streamflow measurements may not have been collected at the same location at each site. Surface water flow was measured by a Marsh- McBirney flow meter. |
