Type: | Package |
Title: | Tide Analysis and Prediction of Predominantly Semi-Diurnal Tides |
Version: | 0.0.3 |
Date: | 2020-12-15 |
Description: | Tide analysis and prediction of predominantly semi-diurnal tides with two high waters and two low waters during one lunar day (~24.842 hours, ~1.035 days). The analysis should preferably cover an observation period of at least 19 years. For shorter periods, for example, the nodal cycle can not be taken into account, which particularly affects the height calculation. The main objective of this package is to produce tide tables. |
Imports: | chron (≥ 2.3-54), data.table (≥ 1.13.2) |
Depends: | R (≥ 3.6.0) |
LazyData: | true |
License: | GPL-3 |
RoxygenNote: | 7.1.1 |
Suggests: | testthat (≥ 2.1.0) |
NeedsCompilation: | no |
Packaged: | 2020-12-15 17:30:16 UTC; Moritz |
Author: | Moritz Mueller-Navarra [aut, cre], Sylvin Mueller-Navarra [aut] ((2019) <https://doi.org/10.5194/os-15-1363-2019>), Andreas Boesch [ctb] ((2019) <https://doi.org/10.5194/os-15-1363-2019>) |
Maintainer: | Moritz Mueller-Navarra <muellernavarra@gmail.com> |
Repository: | CRAN |
Date/Publication: | 2020-12-15 19:30:02 UTC |
Builds a TideTable model
Description
Builds a TideTable model of class "tidetable".
Usage
BuildTT(
dataInput,
otz = 1,
asdate,
astime,
aedate,
aetime,
hwi = "99:99",
sharp_hwi = TRUE
)
Arguments
dataInput |
the data frame with observation date, observation time and height. |
otz |
time zone of the observations. Default is 1 (UTC + 1) |
asdate |
The start date.Format: "yyyy/mm/dd" |
astime |
The start time. Format: "hh:mm:ss" |
aedate |
The end date. Format: "yyyy/mm/dd" |
aetime |
The end time. Format: "hh:mm:ss" |
hwi |
The high water interval. Format: "hh::mm" |
sharp_hwi |
should the hwi computation be sharp? Default is TRUE |
Value
Returns a object of class "tidetable" which contains following elements:
fitting.coeff |
Coefficients for the eight fitted linear models used in the synthesis |
diff.analyse |
Time in days spanning the analysis |
omega_t |
Return value of FindOmega() |
tm24 |
Internal constant |
tplus |
Internal constant |
tmhwi |
Mean high water interval |
References
https://doi.org/10.5194/os-15-1363-2019
Examples
BuildTT(dataInput = observation, asdate = "1991/01/01",
astime ="12:00:00", aedate = "1992/01/01", aetime = "12:00:00")
Returns predictor vector for design matrix
Description
Returns predictor vector for design matrix from 39 astronomical angular velocities.
Usage
ComputeAfunc(omega = NULL, xi = NULL)
Arguments
omega |
The return value of FindOmega(). |
xi |
Transit index |
Value
A list with the selected angular velocities, their ranks and the predictor vector (values between -1, 1).
Calculates tmhwi
Description
This functions computes an estimate for the mean high water interval (tmhwi) in UTC
Usage
EstimateTmhwi(input, strict = TRUE)
Arguments
input |
Should be a data.table object with three columns d_days, high_low and height, where d_days is a vector of fraction of days since 1900/01/01 00:00:00, high_low indicating a high water(1) or a low water(0), height is the corresponding height |
strict |
If strict is true (default), the computations are more sharp. |
Value
Returns the mean high water interval in UTC
Returns omegas and their ranks.
Description
Returns omegas and their ranks from 39 astronomical angular velocities.
Usage
FindOmega(tdiff)
Arguments
tdiff |
Length of input time series. |
Value
A list with the selected angular velocities and their ranks.
Returns predictor vector for design matrix
Description
Returns predictor vector for design matrix from 39 astronomical angular velocities.
Usage
Funcs(tdiff, xi)
Arguments
tdiff |
Length of input time series. |
xi |
Transit index |
Value
A list with the selected angular velocities, their ranks and the predictor vector (Values between -1, 1).
Calculates numm and k4
Description
Calculates transit number (numm) and high (1, 3) or low (2, 4) water number (k4).
Usage
NumCulm(t, tmhwi)
Arguments
t |
Time in days after 1900/01/01 00:00:00 UTC. |
tmhwi |
Mean high water interval (Greenwich meridian). |
Value
Returns a list containing numm and k4.
Synthesizes a tide table
Description
Synthesizes a tide table, built with BuildTT().
Usage
SynTT(tmodel = NULL, ssdate, sstime, sedate, setime)
Arguments
tmodel |
The model you built with BuildTT() |
ssdate |
Start date of the synthesis. Format: "yyyy/mm/dd" |
sstime |
Start time of the synthesis Format: "hh:mm:ss". |
sedate |
End date of the synthesis. Format: "yyyy/mm/dd" |
setime |
End time of the synthesis. Format: "hh:mm:ss" |
Value
Returns a tide table as a data.table, which is identical to c.table computed with TideTable().
References
https://doi.org/10.5194/os-15-1363-2019
Examples
## Not run: SynTT(tmodel = tt_model, ssdate = "1991/01/01",
sstime = "12:00:00", sedate = "1992/01/01", setime = "12:00:00")
## End(Not run)
Computes a tide table
Description
Takes a data frame as input with date time, high water and height information and returns a tide table
Usage
TideTable(
dataInput,
otz = 1,
hwi = "99:99",
sharp_hwi = TRUE,
asdate,
astime,
aedate,
aetime,
ssdate,
sstime,
sedate,
setime,
stz = 1
)
Arguments
dataInput |
A data frame with the columns observation_date, observation_time, high_or_low_water and height. See attached data for correct formats. |
otz |
The time zone of the observations |
hwi |
The average of all intervals between the Moon's transit (upper or lower) over the Greenwich meridian and the following high or low waters for all phases of the Moon is known as mean high water lunitidal interval and is abbreviated to high water interval (hwi). Please only supply a value, when you are sure. Otherwise leave the default value "99:99" untouched. hwi is then computed for you. |
sharp_hwi |
Default is TRUE, which results in a sharp hwi computation. Set on FALSE if you analyze shorter time intervals and EstimateTmhwi function returns NA. |
asdate |
A string indication the date you want the analysis to start with. Format: "yyyy/mm/dd". |
astime |
A string indicating the time you want the analysis to start with. Format: "hh:mm:ss" |
aedate |
A string indication the date you want the analysis to end with. Format: "yyyy/mm/dd". |
aetime |
A string indicating the time you want the analysis to end with. Format: "hh:mm:ss" |
ssdate |
Synthesis start date. This indicates the date you want your tide table to start with. Format: See above |
sstime |
Synthesis start time. The starting time for your tide table. Format: See above |
sedate |
Synthesis end date. Format: See above |
setime |
Synthesis end time. Format: See above |
stz |
Dummy for later extension to modify target time zone. |
Value
Returns a list with elements of the analysis, fitting and the tide table for given data
c.table |
The complete synthesis data as a data.table object |
tide.table |
The tide table as a data.table object |
lm.coeff |
Coefficients for the eight fitted linear models used in the synthesis |
diff.analyse |
Time in days spanning the analysis |
i.analyse |
How many different cases where used in the analysis |
References
Horn, W. (1960) Some Recent Approaches to Tidal Problems. Int. Hydrogr. Rev. 37(2), 65-84
Godin, Gabriel (1972) The Analysis of Tides. Toronto, 264pp
https://doi.org/10.5194/os-15-1363-2019
Examples
TideTable(dataInput = observation, asdate = "1991/01/01",
astime = "12:00:00",
aedate = "1992/01/01", aetime = "12:00:00", ssdate = "1991/01/01",
sstime = "00:00:00", sedate = "1991/01/31", setime = "21:00:00")
Sample file of high and low water times and heights
Description
A sample dataset containing observation date, time and height of high and low water
Usage
observation
Format
A data frame with 26819 rows and 4 variables
- observation_date
date of tide, "yyyy/mm/dd" format, character
- observation_time
time of tide, "hh:mm:ss" format, character
- high_or_low_water
indication whether high (1) or low water (0) was present given date and time, integer
- height
height of the tide, numeric