Description Usage Arguments Details Value Notes References Examples
Compute the Indicators of Hydrologic Alteration for a daily time series.
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ts |
A time series of class |
yearstart |
A character vector specifying the month and day signifying the start of the water year, in the format "mm-dd". Default is "01-01". |
yearend |
A character vector specifying the month and day signifying the end of the water year, in the format "mm-dd". Default is "12-31". |
groups |
The parameter groups to compute. Computes all groups (1-5) by default. |
ut |
The upper flow threshold for identifying high flow pulses. IHA recommends the 75th flow percentile for pre-impact conditions. |
lt |
The lower flow threshold for identifying low flow pulses. IHA recommends the 25th flow percentile for pre-impact conditions. |
parametric |
Logical: perform parametric (mean) or non-parametric (median) analysis. |
The IHA method requires a regular time series with no missing values.
An IHA object containing the the parameter names, the value of the
attribute and the year of record (YoR) for which the attribute was
computed. Use summary()
to report the central tendencies and
measures of dispersion for each parameter and confint()
to compute
parametric or non-parametric confidence intervals for the summary
statistics.
Low- and high-flow pulses occurring at the start of a year of record are ignored when calculating number of pulses and mean duration of pulses.
IHA v7 rounds averages of flow values to the nearest whole number for individual water years, and this rounding propagates through the scorecard. Numerical results may differ slightly from IHAv7.
Richter, B. D., Baumgartner, J. V., Powell, J. and Braun, D. P. (1996), A Method for Assessing Hydrologic Alteration within Ecosystems. Conservation Biology, 10: 1163-1174. doi: 10.1046/j.1523-1739.1996.10041163.x
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