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Differences between mean tide level and mean sea level

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Abstract

This paper discusses the differences between mean tide level (MTL) and mean sea level (MSL) as demonstrated using information from a global tide gauge data set. The roles of the two main contributors to differences between MTL and MSL (the M4 harmonic of the M2 semidiurnal tide, and the combination of the diurnal tides K1 and O1) are described, with a particular focus on the spatial scales of variation in MTL–MSL due to each contributor. Findings from the tide gauge data set are contrasted with those from a state-of-the-art global tide model. The study is of interest within tidal science, but also has practical importance regarding the type of mean level used to define land survey datums. In addition, an appreciation of MTL–MSL difference is important in the use of the historical sea level data used in climate change research, with implications for some of the data stored in international databanks. Particular studies are made of how MTL and MSL might differ through the year, and if MTL is measured in daylight hours only, as has been the practice of some national geodetic agencies on occasions in the past.

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Acknowledgments

This work was undertaken when the author was an Honorary Research Fellow at the National Oceanography Centre in Liverpool. I would like to thank Mark Tamisiea and David Pugh (NOC) and Peter Hogarth (Kongsberg Maritime) for discussions on the need to understand possible MTL/MSL biases when both quantities are included in sea level time series. Richard Ray (Goddard Space Flight Center) and Thomas Wahl (University of Southampton) provided valuable comments and information. The International Hydrographic Organization tidal constants were made available via David Blackman (NOC). Many thanks are due to the providers of data to the GESLA-2 set. Some of the figures in this paper were generated using the Generic Mapping Tools (Wessel and Smith 1998).

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Correspondence to P. L. Woodworth.

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Appendix

Appendix

Names and speeds (deg/solar hour times 10\(^{7}\)) of the tidal constituents in the standard set used in this study

Name

Speed

ZO

0

SA

0410686

SSA

0821373

MM

5443747

MSF

10158958

MF

10980331

2Q1

128542862

SIG1

129271398

Q1

133986609

RO1

134715145

O1

139430356

MP1

140251729

M1

144920521

CHI1

145695476

PI1

149178647

P1

149589314

S1

150000000

K1

150410686

PSI1

150821353

PHI1

151232059

TH1

155125897

J1

155854433

SO1

160569644

OO1

161391017

OQ2

273416965

MNS2

274238337

2N2

278953548

MU2

279682084

N2

284397295

NU2

285125831

OP2

289019669

M2

289841042

MKS2

290662415

LAM2

294556253

L2

295284789

T2

299589333

S2

300000000

R2

300410667

K2

300821373

MSN2

305443747

KJ2

306265120

2SM2

310158958

MO3

429271398

M3

434761563

SO3

439430356

MK3

440251729

SK3

450410686

MN4

574238337

M4

579682084

SN4

584397295

MS4

589841042

MK4

590662415

S4

600000000

SK4

600821373

2MN6

864079380

M6

869523127

MSN6

874238337

2MS6

879682084

2MK6

880503457

2SM6

889841042

MSK6

890662415

MA2

289430356

MB2

290251728

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Woodworth, P.L. Differences between mean tide level and mean sea level. J Geod 91, 69–90 (2017). https://doi.org/10.1007/s00190-016-0938-1

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