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Padang, Sumatera Barat

Period
01 Jan 202601 Agu 2026212 days
Datum
Nol sensor stasiun (bukan MSL)
gaps
1333 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

0.0835m

Residual RMS — Admiralty

0.0846m

Condition number κ — Least squares

1.52

Least squares compared with Admiralty
ConstituentH — Least squaresH — AdmiraltyDifference Hg — Least squaresg — AdmiraltyDifference gDetermination
M20.35760.35750.0001337.7338.5-0.8Direct
S20.14870.1505-0.001820.620.8-0.2Direct
K10.12320.1257-0.0025359.51.5-2.1Direct
O10.07640.0781-0.0017348.6347.70.9Direct
N20.07480.07280.0020321.0312.38.6Direct
K20.04150.04060.000914.420.8-6.4Inferred
P10.03060.0416-0.01116.21.54.7Inferred
M40.01680.01630.000436.138.1-2.1Direct
MS40.00660.0067-0.0000151.8145.66.2Direct

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.