Classical tidal harmonic analysis including error estimates in MATLAB using T_TIDE

By R. Pawlowicz, B. Beardsley, S. Lentz. 2002

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View Paper: https://www.semanticscholar.org/paper/896c654ffd274e313436d202ab0736909a6649aa

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In Oceanography

Citations in the corpus

Gene expression in the intertidal mussel Mytilus californianus: physiological response to environmental factors on a biogeographic scale (2008, positive): “Using the T-Tide toolbox for Matlab (Pawlowicz et al. 2002), we calculated the total amount of time that the still water level at each site was below several tide heights (0.25 or 0.5 m above mean low low water [MLLW]) during the hours from 11:00 to 17:00 during the 30 or 60 d before our samples wer”
Mesoscale to submesoscale wavenumber spectra in Drake Passage (2016, positive): “To assess the fraction of SSH variance due to coherent tides, we remove tidal frequencies using t-tide (Pawlowicz et al. 2002).”
The accuracy of surface elevations in forward global barotropic and baroclinic tide models (2004, methodology): “Frequencies are separated from each other in multi-constituent runs with the harmonic analysis package of Pawlowicz et al. (2002), which is based on that of Foreman (1977).”
A new high-resolution model of non-tidal atmosphere and ocean mass variability for de-aliasing of satellite gravity observations: AOD1B RL06 (2017, methodology): “Tidal signals are estimated and removed by means of the T_TIDE package for classical harmonic analysis (Pawlowicz et al. 2002).”
Observations of Cross-Shelf Flow Driven by Cross-Shelf Winds on the Inner Continental Shelf (2008, background): “This “residual” cross-shelf velocity profile is partly due to tides: it is significantly correlated at the 95% confidence interval with a spring-neap tidal index Isn (defined as the magnitude of the predicted tidal velocity from T_TIDE, low-pass filtered twice with a 33-h cutoff).”
Rectification of the Bias in the Wavelet Power Spectrum (2007, methodology): “After quality control, the sea level record is de-tided by removing the four major tidal constituents: M2, S2, K1, and O1, using the T_Tide Harmonic Analysis Toolbox of Pawlowicz et al. (2002).”
Enhancing tidal harmonic analysis: Robust (hybrid L 1 =L 2 ) solutions (2009, methodology): “Pawlowicz et al. (2002) discusses methods of estimating parameter variance and confidence intervals, including a linearized analysis and nonlinear bootstrap procedures, assuming either white or colored noise.”
Energetics of Barotropic and Baroclinic Tides in the Monterey Bay Area (2012, methodology): “We employ the T-Tide package (Pawlowicz et al. 2002) to estimate the M2 surface amplitudes and phases.”