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Moritz Mueller-Navarra [aut, cre], Sylvin Mueller-Navarra [aut]
Tidal analysis of evenly spaced observed time series (time step 1 to 60 min) with or
without shorter gaps.
The analysis should preferably cover an observation period of at least 19 years.
For shorter periods low frequency constituents are not taken into account, in accordance with the Rayleigh-Criterion.
The main objective of this package is to synthesize or predict a tidal time series.

Moritz Mueller-Navarra [aut, cre], Sylvin Mueller-Navarra [aut], Andreas Boesch [aut]

Moritz Mueller-Navarra [aut, cre], Sylvin Mueller-Navarra [aut], Andreas Boesch [ctb]
Tidal analysis of evenly spaced observed time series (time step 1 to 60 min) with or
without shorter gaps using the harmonic representation of inequalities.
The analysis should preferably cover an observation period of at least 19 years.
For shorter periods low frequency constituents are not taken into account, in accordance with the Rayleigh-Criterion.
The main objective of this package is to synthesize or predict a tidal time series.

c(
person("Moritz","Mueller-Navarra", email="muellernavarra@gmail.com",role=c("aut","cre")),
person("Sylvin","Mueller-Navarra", email="4@sylvin.de",role="aut", comment = "(2019) <https://doi.org/10.5194/os-15-1363-2019>"),
person("Andreas", "Boesch", role="ctb", comment = "(2019) <https://doi.org/10.5194/os-15-1363-2019>"))
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>)

Implements harmonic analysis of tidal and sea-level data.
Over 400 harmonic tidal constituents can be estimated, all with
daily nodal corrections. Time-varying mean sea-levels can also
be used.

Tide Analysis and Prediction of Predominantly Semi-Diurnal Tides
c(
person("Moritz","Mueller-Navarra", email="muellernavarra@gmail.com",role=c("aut","cre")),
person("Sylvin","Mueller-Navarra", email="4@sylvin.de",role="aut"))
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.
Moritz Mueller-Navarra [aut, cre],
Sylvin Mueller-Navarra [aut]