Major Tidal Constituents
Constituent |
Frequency (cpd) |
Description |
|
|---|---|---|---|
sa |
056.554 |
0.00273791 |
Solar annual |
ssa |
057.555 |
0.00547582 |
Solar semiannual |
mm |
065.455 |
0.03629165 |
Lunar monthly |
msf |
073.555 |
0.06772638 |
Lunisolar synodic fortnightly |
mf |
075.555 |
0.07320220 |
Lunar declinational fortnightly |
mt |
085.455 |
0.10949385 |
Termensual |
2q1 |
125.755 |
0.85695241 |
Smaller elliptical diurnal |
σ1 |
127.555 |
0.86180932 |
Lunar variational diurnal |
q1 |
135.655 |
0.89324406 |
Larger lunar elliptical diurnal |
ρ1 |
137.455 |
0.89810097 |
Larger lunar evectional diurnal |
o1 |
145.555 |
0.92953571 |
Lunar diurnal |
τ1 |
147.555 |
0.93501153 |
|
m1 |
155.555 |
0.96613681 |
Smaller lunar elliptical diurnal |
χ1 |
157.455 |
0.97130317 |
Smaller evectional diurnal |
π1 |
162.556 |
0.99452418 |
Solar elliptical diurnal |
p1 |
163.555 |
0.99726209 |
Principal solar diurnal |
s1 |
164.555 |
1.00000000 |
Raditional solar diurnal |
k1 |
165.555 |
1.00273791 |
Principal declinational diurnal |
ᴪ1 |
166.554 |
1.00547582 |
Smaller solar elliptical diurnal |
φ1 |
167.555 |
1.00821373 |
Second-order solar diurnal |
θ1 |
173.655 |
1.03417265 |
Evectional diurnal |
j1 |
175.455 |
1.03902956 |
Smaller lunar elliptical diurnal |
oo1 |
185.555 |
1.07594011 |
Second-order lunar diurnal |
ϵ2 |
227.655 |
1.82825558 |
|
2n2 |
235.755 |
1.85969032 |
Second-order lunar elliptical semidiurnal |
μ2 |
237.555 |
1.86454723 |
Lunar variational |
n2 |
245.655 |
1.89598197 |
Larger lunar elliptical semidiurnal |
ν2 |
247.455 |
1.90083888 |
Larger lunar evectional semidiurnal |
m2 |
255.555 |
1.93227362 |
Principal lunar semidiurnal |
λ2 |
263.655 |
1.96370835 |
Smaller lunar evectional |
l2 |
265.455 |
1.96856526 |
Smaller lunar elliptical semidiurnal |
t2 |
272.556 |
1.99726209 |
Larger solar elliptical semidiurnal |
s2 |
273.555 |
2.00000000 |
Principal solar semidiurnal |
r2 |
274.554 |
2.00273791 |
Smaller solar elliptical semidiurnal |
k2 |
275.555 |
2.00547582 |
Lunisolar declinational semidiurnal |
η2 |
285.455 |
2.04176747 |
|
m3 |
355.555 |
2.89841042 |
Principal lunar terdiurnal |
From Cartwright and Edden [11], Cartwright and Tayler [12], Doodson and Lamb [17]
Compound Constituents
Two or more constituents can interact harmonically in shallow-water to form overtides or compound constituents. The properties of these compound constituents can be derived from the properties of their parent constituents.
Constituent Notations
Every tidal constituent corresponds to a specific combination of astronomical cycles [see Arguments], and several notation systems exist for encoding that combination compactly.
pyTMD supports three (interchangeable) formalisms:
Cartwright numbers: stores the multipliers as signed integers in an ordered list [12].
Doodson numbers: compact decimal representation designed for human-readable identification of constituents [17].
Extended Doodson numbers (XDO): compact and human-readable representation used by the UK Hydrographic Office (UKHO)
Cartwright Numbers
Cartwright numbers are an ordered list of signed integers for the multipliers of the astronomical arguments [see Equation 1.2]:
\(d_1\): multiples of the spherical harmonic dependence (\(\tau\))
\(d_2\): multiples of the mean longitude of the Moon (\(S\))
\(d_3\): multiples of the mean longitude of the Sun (\(H\))
\(d_4\): multiples of the mean longitude of the perigee of the Moon (\(P\))
\(d_5\): multiples of the mean longitude of the node of the Moon (\(N\))
\(d_6\): multiples of the mean longitude of the perigee of the Sun (\(Ps\))
Doodson Numbers
Doodson numbers are an unsigned notion where the second through sixth multipliers (\(d_{2-6}\)) are encoded by adding 5 (the first digit \(d_1\) is not offset). This offset maps the range of multipliers \([-5, +4]\) into \([0, 9]\). This encoding can be extended by mapping \(+5\) to \(\mathrm{X}\), \(+6\) to \(\mathrm{E}\), and \(+7\) to \(\mathrm{T}\) (which would map to \(10\), \(11\) and \(12\) in the standard notation).
Extended Doodson Numbers
The UKHO Extended Doodson Number (XDO) system was designed to address two limitations of the standard Doodson notation:
Range: the +5 digit offset only covers multipliers in \([-5, +4]\). Tidal catalogs larger than the original from Doodson and Lamb [17] can have constituents with multipliers outside that range
Disambiguation: the format carries a seventh character encoding the index \(k\) which resolves ambiguities when constituents share the same Doodson number
The XDO system maps \(0\) to \(\mathrm{Z}\), the range \([1,15]\) to \([\mathrm{A},\mathrm{P}]\), and the range \([-8,-1]\) to \([\mathrm{R},\mathrm{Y}]\).
Tidal Classifications
Classification |
Description |
|---|---|
shared \(d_1\) |
|
Group |
shared \(d_1\) and \(d_2\) |
Subgroup |
shared \(d_1\), \(d_2\) and \(d_3\) |