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Benoa, Bali

Period
01 Jan 202601 Agu 2026212 days
Datum
Nol sensor stasiun (bukan MSL)
gaps
6988 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

0.1890m

Residual RMS — Admiralty

0.1913m

Condition number κ — Least squares

1.53

Least squares compared with Admiralty
ConstituentH — Least squaresH — AdmiraltyDifference Hg — Least squaresg — AdmiraltyDifference gDetermination
M20.64320.6440-0.000751.652.6-1.0Direct
S20.36540.36410.0013107.8108.5-0.7Direct
K10.25320.2606-0.0074357.5358.5-1.0Direct
O10.16400.1684-0.0044344.7343.90.8Direct
N20.11900.1200-0.000926.515.011.5Direct
K20.09940.09830.0011101.9108.5-6.6Inferred
P10.06380.0863-0.0225348.3358.5-10.2Inferred
M40.00920.0118-0.0026210.2220.7-10.5Direct
MS40.00640.0065-0.0001270.3277.0-6.7Direct

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.