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Bitung, Sulawesi Utara

Period
01 Jan 202601 Agu 2026212 days
Datum
Nol sensor stasiun (bukan MSL)
gaps
27707 jam
Source
IOC Sea Level Station Monitoring Facility (UNESCO/IOC & VLIZ)
Source, licence and datum notes

Licence: Akses terbuka dengan kewajiban sitasi (VLIZ/IOC, DOI 10.14284/482)

Flanders Marine Institute (VLIZ); Intergovernmental Oceanographic Commission (IOC) (2026): Sea level station monitoring facility. https://www.ioc-sealevelmonitoring.org — DOI 10.14284/482

Not for navigationThe official Indonesian tide tables are published by Pushidrosal.

Methods

Method comparison

The same record, two classical methods. Least squares solves every constituent jointly; Admiralty projects them one at a time and infers the rest from fixed ratios.

Residual RMS — Least squares

0.0786m

Residual RMS — Admiralty

0.0828m

Condition number κ — Least squares

1.65

Least squares compared with Admiralty
ConstituentH — Least squaresH — AdmiraltyDifference Hg — Least squaresg — AdmiraltyDifference gDetermination
M20.34140.3456-0.0042277.0278.0-1.0Direct
S20.22540.21730.0081314.5316.6-2.1Direct
K10.20820.2239-0.0158310.1312.6-2.5Direct
O10.11950.1264-0.0069291.6289.81.8Direct
K20.06770.05870.0091307.3316.6-9.3Inferred
P10.06290.0741-0.0112309.7312.6-3.0Inferred
N20.05080.04490.0060269.5254.515.0Direct
M40.00720.0078-0.0006169.8167.02.7Direct
MS40.00610.0061-0.0000258.5266.4-7.9Direct

Admiralty infers K2, P1 from its neighbours through fixed ratios rather than solving for them. Least squares solves every constituent jointly and so accounts for the correlation between neighbours; that is the only fundamental difference between the two here.

The Admiralty implementation here is its projection-and-inference scheme, not a reproduction of the printed NP 159 tabulation and its filtering multipliers.