2006
DOI: 10.3133/sir20055163
|View full text |Cite
|
Sign up to set email alerts
|

Hydrologic requirements of and consumptive ground-water use by riparian vegetation along the San Pedro River, Arizona

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1
1

Citation Types

0
43
0

Year Published

2008
2008
2020
2020

Publication Types

Select...
9

Relationship

3
6

Authors

Journals

citations
Cited by 34 publications
(43 citation statements)
references
References 0 publications
0
43
0
Order By: Relevance
“…As part of the overall planning strategy, the USPP tasked a multidisciplinary team of researchers to better characterize the hydrology of the Upper San Pedro Basin including that of the SPRNCA (Leenhouts et al, 2006). One facet of this work has been to quantify the riparian ET in the Upper San Pedro Basin (Scott et al, 2006b).…”
Section: Background On Determining Riparian Et In the San Pedro Basinmentioning
confidence: 99%
“…As part of the overall planning strategy, the USPP tasked a multidisciplinary team of researchers to better characterize the hydrology of the Upper San Pedro Basin including that of the SPRNCA (Leenhouts et al, 2006). One facet of this work has been to quantify the riparian ET in the Upper San Pedro Basin (Scott et al, 2006b).…”
Section: Background On Determining Riparian Et In the San Pedro Basinmentioning
confidence: 99%
“…As an initial step in determining distinguishable cover types, the 2003 photographs were ground-truthed using field data (Leenhouts et al, 2006 and unpublished data from Gabrielle Katz, Appalachian State University). This process yielded six cover types (Table 2).…”
Section: Riparian Cover Typesmentioning
confidence: 99%
“…These studies include Coes and Pool's [28] assessment of ephemeral-stream channel and basin-floor infiltration and recharge, Gungle's [29] analysis of the timing and duration of ephemeral stream flow in the subwatershed, and Leenhouts and others' [30] analysis of the hydrology, vegetation-hydrologic relationships, and evapotranspiration requirements and plant-water sources in the SPRNCA. Leenhouts and others [30] established additional streamflow and groundwater monitoring in the subwatershed, including streamflow stage and permanence data, near-stream alluvial aquifer groundwater and vertical gradient monitoring, and a continuous meteorological and eddy covariance monitoring station for measurement of evapotranspiration in the SPRNCA.…”
Section: General Hydrologic Processesmentioning
confidence: 99%