Description Usage Arguments Value References See Also
View source: R/tq_regime_signatures.R
This function computes signatures based on the air temperature (T) and streamflow (Q) regime cycle: the slopes of 4 periods (T+Q+, T+Q-, T-Q-1, T-Q-2 periods) of the T-Q cycle and timing of the Q maximum.
1 2 3 4 5 6 7 8 | tq_signatures(
hdays,
T,
Q,
n = 30,
remove_last = TRUE,
periods = c(183, 336, 62)
)
|
hdays |
numeric vector. vector of 'julian' date of length m which
should be computed according to hydrological year (see function
|
T |
numeric vector. air temperature regime (365 or 366 values) |
Q |
numeric vector. streamflow regime (365 or 366 values) |
n |
integer. smoothing window |
remove_last |
logical. should the last day of the year (366) be |
peridos |
numeric vector. a vector of length 3 defining (1) the start of the T+Q+ period, (2) the start (resp. end) of the T-Q-2 (resp. T-Q-1) period and (3) the end of the T-Q-2 period. Note: the other period boundaries are computed using the air temperature and streamflow regime maxima timings. |
A vector of length 5 with the following named components: "TQslp_TpQp", "TQslp_TpQm", "TQslp_TmQm1", "TQslp_TmQm2", "tQmax"
I. Horner, F. Branger, H. McMillan, O. Vannier, and I. Braud, “Information content of snow hydrological signatures based on streamflow, precipitation and air temperature,” Hydrological Processes, vol. 34, no. 12, Art. no. 12, 2020, doi: 10.1002/hyp.13762.
[tq_periods][regime_curve][q_timing][tq_slopes]
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