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  1. Deutsche Hydrografische Zeitschrift
  2. Deutsche Hydrografische Zeitschrift : Volume 64
  3. Deutsche Hydrografische Zeitschrift : Volume 64, Issue 2, February 2014
  4. Seasonal variation of the M 2 tide
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Deutsche Hydrografische Zeitschrift : Volume 67
Deutsche Hydrografische Zeitschrift : Volume 66
Deutsche Hydrografische Zeitschrift : Volume 65
Deutsche Hydrografische Zeitschrift : Volume 64
Deutsche Hydrografische Zeitschrift : Volume 64, Issue 12, December 2014
Deutsche Hydrografische Zeitschrift : Volume 64, Issue 11, November 2014
Deutsche Hydrografische Zeitschrift : Volume 64, Issue 10, October 2014
Deutsche Hydrografische Zeitschrift : Volume 64, Issue 9, September 2014
Deutsche Hydrografische Zeitschrift : Volume 64, Issue 8, August 2014
Deutsche Hydrografische Zeitschrift : Volume 64, Issue 7, July 2014
Deutsche Hydrografische Zeitschrift : Volume 64, Issue 6, June 2014
Deutsche Hydrografische Zeitschrift : Volume 64, Issue 5, May 2014
Deutsche Hydrografische Zeitschrift : Volume 64, Issue 4, April 2014
Deutsche Hydrografische Zeitschrift : Volume 64, Issue 3, March 2014
Deutsche Hydrografische Zeitschrift : Volume 64, Issue 2, February 2014
Seasonal variation of the M 2 tide
Seasonal dynamics and stoichiometry of the planktonic community in the NW Mediterranean Sea: a 3D modeling approach
Wind-forced circulation model and water exchanges through the channel in the Bay of Toulon
Observations of bedforms on a dissipative macrotidal beach
A model study of the Copper River plume and its effects on the northern Gulf of Alaska
Analysis of STCC eddies using the Okubo–Weiss parameter on model and satellite data
Model studies of dense water overflows in the Faroese Channels
Numerical study on wave propagation over a fluid-mud layer with different bottom conditions
Modeling flocculation in a hypertidal estuary
Deutsche Hydrografische Zeitschrift : Volume 64, Issue 1, January 2014
Deutsche Hydrografische Zeitschrift : Volume 63
Deutsche Hydrografische Zeitschrift : Volume 62
Deutsche Hydrografische Zeitschrift : Volume 61
Deutsche Hydrografische Zeitschrift : Volume 60
Deutsche Hydrografische Zeitschrift : Volume 59
Deutsche Hydrografische Zeitschrift : Volume 58
Deutsche Hydrografische Zeitschrift : Volume 57
Deutsche Hydrografische Zeitschrift : Volume 56
Deutsche Hydrografische Zeitschrift : Volume 55
Deutsche Hydrografische Zeitschrift : Volume 54
Deutsche Hydrografische Zeitschrift : Volume 53
Deutsche Hydrografische Zeitschrift : Volume 52
Deutsche Hydrografische Zeitschrift : Volume 51
Deutsche Hydrografische Zeitschrift : Volume 50
Deutsche Hydrografische Zeitschrift : Volume 49

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Seasonal variation of the M 2 tide

Content Provider Springer Nature Link
Author Müller, Malte Cherniawsky, Josef Y. Foreman, Michael G. G. Storch, Jin Song
Copyright Year 2014
Abstract The seasonal cycle of the main lunar tidal constituent M 2 is studied globally by an analysis of a high-resolution ocean circulation and tide model (STORMTIDE) simulation, of 19 years of satellite altimeter data, and of multiyear tide-gauge records. The barotropic seasonal tidal variability is dominant in coastal and polar regions with relative changes of the tidal amplitude of 5–10 %. A comparison with the observations shows that the ocean circulation and tide model captures the seasonal pattern of the M 2 tide reasonably well. There are two main processes leading to the seasonal variability in the barotropic tide: First, seasonal changes in stratification on the continental shelf affect the vertical profile of eddy viscosity and, in turn, the vertical current profile. Second, the frictional effect between sea-ice and the surface ocean layer leads to seasonally varying tidal transport. We estimate from the model simulation that the M 2 tidal energy dissipation at the sea surface varies seasonally in the Arctic (ocean regions north of 60°N) between 2 and 34 GW, whereas in the Southern Ocean, it varies between 0.5 and 2 GW. The M 2 internal tide is mainly affected by stratification, and the induced modified phase speed of the internal waves leads to amplitude differences in the surface tide signal of 0.005–0.0150 m. The seasonal signals of the M 2 surface tide are large compared to the accuracy demands of satellite altimetry and gravity observations and emphasize the importance to consider seasonal tidal variability in the correction processes of satellite data.
Starting Page 159
Ending Page 177
Page Count 19
File Format PDF
ISSN 16167341
Journal Deutsche Hydrografische Zeitschrift
Volume Number 64
Issue Number 2
e-ISSN 16167228
Language English
Publisher Springer Berlin Heidelberg
Publisher Date 2014-01-09
Publisher Place Berlin, Heidelberg
Access Restriction One Nation One Subscription (ONOS)
Subject Keyword Ocean tides Seasonal variations Arctic tides Coastal tides Nonstationary tides Satellite altimetry Tide-gauge records Oceanography Geophysics/Geodesy Atmospheric Sciences Fluid- and Aerodynamics Environmental Monitoring/Analysis
Content Type Text
Resource Type Article
Subject Oceanography
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