Description Usage Arguments Value Note Author(s) See Also Examples
Extract the summary table from Asquith–Knight discharge decay analyses returned by akqdecay
for a sequence of USGS streamgages contained within the R environment
that has been previously populated by fill_akqenv
.
1 | akq_summary(akqenv, silent=FALSE, ...)
|
akqenv |
The R |
silent |
Suppress informative calls to |
... |
Additional arguments to pass (see source code to ascertain flexible usage). |
An R data.frame
containing the summary for each streamgage.
site |
The streamgage identification number; |
beg_year |
First year in period of record data retrieval; |
end_year |
Last year in period of record data retrieval; |
yr_range_str |
A neat string representation that might be useful in formal tables for publication; |
total_count |
The total number of daily values; |
count |
The count of daily values processed by the settings of |
kendall_tau |
Kendall's Tau between the days per log-cycle changes and the streamflow from the flow-duration curve; |
spearman_rho |
Spearman's Rho between the days per log-cycle changes and the streamflow from the flow-duration curve; |
median |
The median (Ψ_\mathrm{med}) of the processed daily values; |
L1L2 |
The mean plus square-root pi L-scale: λ_1 + λ_2√{π} (see Note); |
gfactor |
The G_f-factor from a fitted distribution for the probability |
gfactor_emp |
The G_f-factor from the empirical distribution for probability |
As yet, Asquith and Knight have definitive opinion on what the optimal “Gfactor” is in regards to depth into the distribution tail of days per log-cycle change on the recession limb of hydrographs. Please contact the authors for further information.
The L1L2
as a term or concept is expected to have little direct meaning to most users. The first L-moment (arithmetic mean) is λ_1. The second L-moment (L-scale) is λ_2 and is directly interpretable as, but not numerically equal to, the well-known standard deviation (σ). Thus, it has units of days per log-cycle and matches those of the mean. The σ is the second parameter of the normal distribution, and this parameter in terms of L-scale is σ = λ_2√{π}. Thus, this is an estimate of the standard deviation via L-moments. The percentile pnorm(sqrt(pi), sd=sqrt(pi))
is the 84 percentile of the normal for λ_1 = 0—hence, L1L2
can loosely be thought of as a parametric estimate of a G_{\mathrm{nor}}(F=0.84) Gfactor. This would be a Gfactor defined as about “one standard deviation into the right tail of the distribution.”
W.H. Asquith
akqdecay
, akq_lmom
, akq_counts
, akq_summary
1 2 3 4 5 6 7 8 9 10 11 | sites <- c("05403500", "05405000") # Two USGS streamgages in Wisconsin
WisExample <- new.env(); fill_dvenv( sites, envir=WisExample,
sdate="1945-01-01", edate="2016-12-31")
WisAKQ <- new.env(); fill_akqenv(dvenv=WisExample, envir=WisAKQ)
akq_summary(WisAKQ) # These line-wrapped values will change as record increases.
# site beg_year end_year yr_range_str total_count count kendall_tau spearman_rho
# 05403500 1945 2016 1945--2016 18444 9242 -0.20468258 -0.3083903
# 05405000 1945 2016 1945--2016 26297 13724 -0.08380238 -0.1295017
# median L1L2 gfactor gfactor_emp
# 37.98102 125.1716 136.3617 139.3032
# 34.95030 155.0216 161.0996 176.1453 #
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