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The following computer codes were kindly made available by their authors over the internet. The internet addresses given are those from which the codes were obtained and may no longer be valid.
CSR Calculates the ocean tide at any location based on
(R. Eanes) satellite altimetry (Schrama & Ray, 1994).
ftp://ftp.csr.utexas.edu/pub/tide/csr_2.0/
ETGTAB Calculates the tidal potential (and hence solid tide) at
(H.-G. Wenzel) any point on the Earth’s surface.
http://www-gik.bau-verm.uni-karlsruhe.de/~iagetc/
HYDROTHRERM Finite difference code to calculate Darcy flow in a
(D. Hayba) porous medium. Uses the full non-linear properties of
water.
http://water.usgs.gov/software/hydrotherm.html
MWPS Implements the multiple window power spectrum
(A. Chave) technique described in Thomson (1982).
ftp://faraday.whoi.edu/pub
SPOTL A suite of programs to calculate the load tide
(D.C. Agnew) (Agnew, 1997).
ftp://bilby.ucsd.edu/pub/spotl
In addition, a selection of codes to predict the ocean tide is currently available from http://podaac-www.jpl.nasa.gov/cdrom/tide/Document/html/models.htm
The following computer codes were written by the author for use in this dissertation.
PREDICT Calculates the time-domain representation of a tidal signal
(T. Jupp) from its Admiralty Method harmonic constants.
HYBRID Extracts the Admiralty Method harmonic constants from
(T. Jupp) a tidally modulated time-series
DIFFUSE Calculates the response of a two dimensional poroelastic
(T. Jupp) subseafloor
convection cell to tidal loading at the seafloor.