Frank L. Engel

Dr. Frank L. Engel

orcid

Research Focus & Metrics

Academic Career Length

15Years (2012-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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19 November 2012 in Earth Surface Processes and Landforms
Verified
Journal Article
Closed access
PDF file
DPD. R. Parsons
D. R. Parsons
PJP. R. Jackson
P. R. Jackson
JCJonathan A. Czuba
Jonathan A. Czuba
FEFrank L. Engel
Frank L. Engel
BRB. L. Rhoads
B. L. Rhoads
JRJ. D. Riley
J. D. Riley

1 August 2012 in Geomorphology
Verified
Journal Article
Closed access
FEFrank L. Engel
Frank L. Engel
BRBruce L. Rhoads
Bruce L. Rhoads

1 October 2017 in Geomorphology
Verified
Journal Article
Closed access
FEFrank L. Engel
Frank L. Engel
BRBruce L. Rhoads
Bruce L. Rhoads

29 December 2015 in Earth Surface Processes and Landforms
Verified
Journal Article
Closed access
PDF file
FEFrank L. Engel
Frank L. Engel
BRBruce L. Rhoads
Bruce L. Rhoads

3 September 2019 in Water Resources Research
Verified
Journal Article
Open access
PDF file
ADAurélien Despax
Aurélien Despax
JCJérôme Le Coz
Jérôme Le Coz
AHAlexandre Hauet
Alexandre Hauet
DMDavid S Mueller
David S Mueller
FEFrank L. Engel
Frank L. Engel
KOKevin A Oberg
Kevin A Oberg
Repeated measures experiments can be conducted to empirically estimate the uncertainty of a stream gauging method, such as the widespread moving‐boat acoustic Doppler current profilers (ADCPs) approach. Previous ADCP repeated measures experiments, also known as interlaboratory comparisons, provided a credible range of uncertainty estimates reflecting the quality of the site conditions. However, the method, which is a one‐way analysis of variance, only addresses the uncertainty of one lumped factor that combines several distinct factors: instrument, operator, procedure, and cross‐section effects. To decompose the uncertainty of ADCP streamflow measurements due to cross‐section selection and team effects, a large repeated measures experiment has been conducted in the Taurion River (France). The experiment design was crossed and balanced, with two sets of 24 teams circulated over two sets of 12 cross sections. A constant flow rate was released from a dam, located immediately upstream of the experimental site. Prior to the statistical analysis, a data quality review was performed using the U.S. Geological Survey QRev software to clean the data set from avoidable errors and to homogenize the discharge computations. A two‐way analysis of variance was applied to quantify the cross‐section effect, the team effect, and their interaction, which was found to dominate the pure cross‐section effect. It was then possible to predict the average uncertainty of multiple‐transect ADCP discharge measurements, depending on the number of teams, cross sections, and repeated transects included in the discharge average. The method opens interesting avenues for documenting difficult‐to‐estimate uncertainty sources of stream gauging techniques in other measuring conditions, especially the most adverse ones.

14 May 2024 in Earth Surface Processes and Landforms
Verified
Journal Article
Closed access
Carl LegleiterCarl Legleiter
Carl Legleiter
PKPaul Kinzel
Paul Kinzel
FEFrank L. Engel
Frank L. Engel
LHLee R. Harrison
Lee R. Harrison
GHGregory Hewitt
Gregory Hewitt