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Sabang, Aceh

Period
01 Jan 202601 Agu 2026212 days
Datum
Nol sensor stasiun (bukan MSL)
gaps
6479 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

0.0888m

Residual RMS — Admiralty

0.0905m

Condition number κ — Least squares

1.53

Least squares compared with Admiralty
ConstituentH — Least squaresH — AdmiraltyDifference Hg — Least squaresg — AdmiraltyDifference gDetermination
M20.50910.5118-0.002785.986.6-0.7Direct
S20.23950.2448-0.0053121.6122.7-1.1Direct
K10.10560.1088-0.003238.139.5-1.4Direct
N20.09600.08780.008281.672.09.6Direct
K20.06940.06610.0033115.9122.7-6.8Inferred
O10.04710.0495-0.00243.34.1-0.8Direct
P10.02700.0360-0.009038.339.5-1.2Inferred
M40.01090.00960.0013144.8149.5-4.8Direct
MS40.00970.0101-0.0003176.3176.7-0.4Direct

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.