https://gssc.esa.int/navipedia/index.php?action=history&feed=atom&title=Ocean_loading
Ocean loading - Revision history
2026-04-26T00:10:40Z
Revision history for this page on the wiki
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https://gssc.esa.int/navipedia/index.php?title=Ocean_loading&diff=13827&oldid=prev
Raphael.Legouge: link to the ocean loading service modified
2017-01-24T13:46:03Z
<p>link to the ocean loading service modified</p>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The FORTRAN code hardisp.f implementing the full IERS conventions Solid-Tides model is available at ftp://tai.bipm.org/iers/convupdt/chapter7/hardisp/HARDISP.F</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>The FORTRAN code hardisp.f implementing the full IERS conventions Solid-Tides model is available at ftp://tai.bipm.org/iers/convupdt/chapter7/hardisp/HARDISP.F</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>This routine computes time series of tidal displacements from a input file containing the ocean loading coefficients for a given station. These coefficients can be obtained from the ocean loading service under request trough the web site http://<del style="font-weight: bold; text-decoration: none;">www</del>.oso.chalmers.se/<del style="font-weight: bold; text-decoration: none;">~</del>loading</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>This routine computes time series of tidal displacements from a input file containing the ocean loading coefficients for a given station. These coefficients can be obtained from the ocean loading service under request trough the web site http://<ins style="font-weight: bold; text-decoration: none;">holt</ins>.oso.chalmers.se/loading<ins style="font-weight: bold; text-decoration: none;">/</ins></div></td></tr>
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Raphael.Legouge
https://gssc.esa.int/navipedia/index.php?title=Ocean_loading&diff=12216&oldid=prev
Jaume.Sanz at 08:57, 17 February 2013
2013-02-17T08:57:03Z
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Jaume.Sanz
https://gssc.esa.int/navipedia/index.php?title=Ocean_loading&diff=11619&oldid=prev
Carlos.Lopez at 11:34, 23 February 2012
2012-02-23T11:34:26Z
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Carlos.Lopez
https://gssc.esa.int/navipedia/index.php?title=Ocean_loading&diff=11092&oldid=prev
Jaume.Sanz at 10:30, 8 February 2012
2012-02-08T10:30:20Z
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>This is a secondary tidal effect, due to the elastic response of the earth's crust to ocean tides, producing deformation of the sea floor and a surface displacement of an adjacent land.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>This is a secondary tidal effect, due to the elastic response of the earth's crust to ocean tides, producing deformation of the sea floor and a surface displacement of an adjacent land.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>The ocean loading is more localised than the solid earth tides and for convention it does not have permanent part. For kinematic PPP (see [[Code and Carrier Based Positioning (PPP)]]) at the few centimetres accuracy level or few millimetres static PPP over <math>24</math> hours and/or far from the oceans, it can be neglected [Kouba and <del style="font-weight: bold; text-decoration: none;">Heroux</del>, 2000] <ref>[Kouba and <del style="font-weight: bold; text-decoration: none;">Heroux</del>, 2000] Kouba, J. and <del style="font-weight: bold; text-decoration: none;">Heroux</del>, 2000. GPS Precise Point Positioning using IGS Orbit Products. Geodetic Survey Division, Natural Resources Canada.</ref>.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>The ocean loading is more localised than the solid earth tides and for convention it does not have permanent part. For kinematic PPP (see [[Code and Carrier Based Positioning (PPP)]]) at the few centimetres accuracy level or few millimetres static PPP over <math>24</math> hours and/or far from the oceans, it can be neglected [Kouba and <ins style="font-weight: bold; text-decoration: none;">Héroux</ins>, 2000] <ref>[Kouba and <ins style="font-weight: bold; text-decoration: none;">Héroux</ins>, 2000] Kouba, J. and <ins style="font-weight: bold; text-decoration: none;">Héroux</ins>, 2000. GPS Precise Point Positioning using IGS Orbit Products. Geodetic Survey Division, Natural Resources Canada.</ref>.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>A model for the ocean loading is described in the IERS Conventions document [Denis et al., 2004] <ref>[Denis et al., 2004] Denis, D., McCarthy and Petit, G., 2004. IERS Conventions (2003). IERS Technical Note 32.. IERS Convention Center., Frankfurt am Main.</ref>, page 73, whose simplified version can be summarised as <ref group="footnotes"> Additional information describing the model of GIPSY-OASIS II can be found in [Webb and Zumberge, 1993]</ref><ref>[Webb and Zumberge, 1993] Webb, F. and Zumberge, J., 1993. An Introduction to GIPSY/OASIS-II. Jet Propulsion Laboratory, JPL, 4800 Oak Grove Drive, Pasadena, CA 91109</ref>:</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>A model for the ocean loading is described in the IERS Conventions document [Denis et al., 2004] <ref>[Denis et al., 2004] Denis, D., McCarthy and Petit, G., 2004. IERS Conventions (2003). IERS Technical Note 32.. IERS Convention Center., Frankfurt am Main.</ref>, page 73, whose simplified version can be summarised as <ref group="footnotes"> Additional information describing the model of GIPSY-OASIS II can be found in [Webb and Zumberge, 1993]</ref><ref>[Webb and Zumberge, 1993] Webb, F. and Zumberge, J., 1993. An Introduction to GIPSY/OASIS-II. Jet Propulsion Laboratory, JPL, 4800 Oak Grove Drive, Pasadena, CA 91109</ref>:</div></td></tr>
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Jaume.Sanz
https://gssc.esa.int/navipedia/index.php?title=Ocean_loading&diff=11088&oldid=prev
Jaume.Sanz at 08:02, 8 February 2012
2012-02-08T08:02:18Z
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Jaume.Sanz
https://gssc.esa.int/navipedia/index.php?title=Ocean_loading&diff=11042&oldid=prev
Jaume.Sanz at 12:48, 6 February 2012
2012-02-06T12:48:46Z
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>::: <math>\Delta {\mathbf r}</math> is the site displacement vector in (radial, west south) coordinates.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>::: <math>\Delta {\mathbf r}</math> is the site displacement vector in (radial, west south) coordinates.</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>:::<math>j</math> represents 11 tidal waves: <math>M_2</math>, <math>S_2</math>, <math>N_2</math>, <math>K_2</math>, <math>K_1</math>, <math>O_1</math>, <math>P_1</math>, <math>Q_1</math>, <math>M_f</math>, <math>M_m</math>, <math>S_{sa}</math>.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>:::<math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>j</math> represents 11 tidal waves: <math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>M_2</math>, <math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>S_2</math>, <math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>N_2</math>, <math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>K_2</math>, <math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>K_1</math>, <math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>O_1</math>, <math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>P_1</math>, <math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>Q_1</math>, <math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>M_f</math>, <math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>M_m</math>, <math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>S_{sa}</math>.</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>:::<math>f_j</math>, <math>u_j</math> depend on the longitude of lunar node.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>:::<math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>f_j</math>, <math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>u_j</math> depend on the longitude of lunar node.</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>:::<math>\omega_j</math> is the tidal angular velocity at time <math>t= 0^h</math>.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>:::<math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>\omega_j</math> is the tidal angular velocity at time <math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>t= 0^h</math>.</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>:::<math>\chi_j</math> is an astronomical argument at time <math>t= 0^h</math>.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>:::<math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>\chi_j</math> is an astronomical argument at time <math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>t= 0^h</math>.</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>:::<math>A_{cj}</math> is a station specific amplitude.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>:::<math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>A_{cj}</math> is a station specific amplitude.</div></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>:::<math>\varphi_{cj}</math> is a station specific phase.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>:::<math><ins style="font-weight: bold; text-decoration: none;">\displaystyle </ins>\varphi_{cj}</math> is a station specific phase.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
</table>
Jaume.Sanz
https://gssc.esa.int/navipedia/index.php?title=Ocean_loading&diff=11039&oldid=prev
Jaume.Sanz at 12:43, 6 February 2012
2012-02-06T12:43:38Z
<p></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 12:43, 6 February 2012</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>The FORTRAN code hardisp.f implementing the full IERS conventions Solid-Tides model is available at ftp://tai.bipm.org/iers/convupdt/chapter7/hardisp.<del style="font-weight: bold; text-decoration: none;">f</del></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>The FORTRAN code hardisp.f implementing the full IERS conventions Solid-Tides model is available at ftp://tai.bipm.org/iers/convupdt/chapter7/hardisp<ins style="font-weight: bold; text-decoration: none;">/HARDISP</ins>.<ins style="font-weight: bold; text-decoration: none;">F</ins></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>This routine computes time series of tidal displacements from a input file containing the ocean loading coefficients for a given station. These coefficients can be obtained from the ocean loading service under request trough the web site http://www.oso.chalmers.se/<del style="font-weight: bold; text-decoration: none;">loadings</del></div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>This routine computes time series of tidal displacements from a input file containing the ocean loading coefficients for a given station. These coefficients can be obtained from the ocean loading service under request trough the web site http://www.oso.chalmers.se/<ins style="font-weight: bold; text-decoration: none;">~loading</ins></div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
</table>
Jaume.Sanz
https://gssc.esa.int/navipedia/index.php?title=Ocean_loading&diff=11037&oldid=prev
Jaume.Sanz at 12:38, 6 February 2012
2012-02-06T12:38:11Z
<p></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 12:38, 6 February 2012</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>This is a secondary tidal effect, due to the elastic response of the earth's crust to ocean tides, producing deformation of the sea floor and a surface displacement of an adjacent land.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>This is a secondary tidal effect, due to the elastic response of the earth's crust to ocean tides, producing deformation of the sea floor and a surface displacement of an adjacent land.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>The ocean loading is more localised than the solid earth tides and for convention it does not have permanent part. For kinematic PPP (see [[Code and Carrier Based Positioning (PPP)]]) at the few centimetres accuracy level or few millimetres static PPP over <math>24</math> hours and/or far from the oceans, it can be neglected [Kouba and <del style="font-weight: bold; text-decoration: none;">H\'eroux.</del>, 2000] <ref>[Kouba and <del style="font-weight: bold; text-decoration: none;">H\'eroux.</del>, 2000] Kouba, J. and <del style="font-weight: bold; text-decoration: none;">H\'eroux.</del>, 2000. GPS Precise Point Positioning using IGS Orbit Products. Geodetic Survey Division, Natural Resources Canada.</ref>.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>The ocean loading is more localised than the solid earth tides and for convention it does not have permanent part. For kinematic PPP (see [[Code and Carrier Based Positioning (PPP)]]) at the few centimetres accuracy level or few millimetres static PPP over <math>24</math> hours and/or far from the oceans, it can be neglected [Kouba and <ins style="font-weight: bold; text-decoration: none;">Heroux</ins>, 2000] <ref>[Kouba and <ins style="font-weight: bold; text-decoration: none;">Heroux</ins>, 2000] Kouba, J. and <ins style="font-weight: bold; text-decoration: none;">Heroux</ins>, 2000. GPS Precise Point Positioning using IGS Orbit Products. Geodetic Survey Division, Natural Resources Canada.</ref>.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>A model for the ocean loading is described in the IERS Conventions document [Denis et al., 2004] <ref>[Denis et al., 2004] Denis, D., McCarthy and Petit, G., 2004. IERS Conventions (2003). IERS Technical Note 32.. IERS Convention Center., Frankfurt am Main.</ref>, page 73, whose simplified version can be summarised as <ref group="footnotes"> Additional information describing the model of GIPSY-OASIS II can be found in [Webb and Zumberge, 1993]</ref><ref>[Webb and Zumberge, 1993] Webb, F. and Zumberge, J., 1993. An Introduction to GIPSY/OASIS-II. Jet Propulsion Laboratory, JPL, 4800 Oak Grove Drive, Pasadena, CA 91109</ref>:</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>A model for the ocean loading is described in the IERS Conventions document [Denis et al., 2004] <ref>[Denis et al., 2004] Denis, D., McCarthy and Petit, G., 2004. IERS Conventions (2003). IERS Technical Note 32.. IERS Convention Center., Frankfurt am Main.</ref>, page 73, whose simplified version can be summarised as <ref group="footnotes"> Additional information describing the model of GIPSY-OASIS II can be found in [Webb and Zumberge, 1993]</ref><ref>[Webb and Zumberge, 1993] Webb, F. and Zumberge, J., 1993. An Introduction to GIPSY/OASIS-II. Jet Propulsion Laboratory, JPL, 4800 Oak Grove Drive, Pasadena, CA 91109</ref>:</div></td></tr>
</table>
Jaume.Sanz
https://gssc.esa.int/navipedia/index.php?title=Ocean_loading&diff=11032&oldid=prev
Jaume.Sanz at 12:27, 6 February 2012
2012-02-06T12:27:45Z
<p></p>
<table style="background-color: #fff; color: #202122;" data-mw="interface">
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<col class="diff-content" />
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<col class="diff-content" />
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 12:27, 6 February 2012</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>This is a secondary tidal effect, due to the elastic response of the earth's crust to ocean tides, producing deformation of the sea floor and a surface displacement of an adjacent land.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>This is a secondary tidal effect, due to the elastic response of the earth's crust to ocean tides, producing deformation of the sea floor and a surface displacement of an adjacent land.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>The ocean loading is more localised than the solid earth tides and for convention it does not have permanent part. For kinematic PPP (see [[Code and Carrier Based Positioning (PPP)]]) at the few centimetres accuracy level or few millimetres static PPP over <math>24</math> hours and/or far from the oceans, it can be neglected [Kouba and <del style="font-weight: bold; text-decoration: none;">H_eroux</del>., 2000] <ref>[Kouba and H\'eroux., 2000] Kouba, J. and <del style="font-weight: bold; text-decoration: none;">H_eroux</del>., 2000. GPS Precise Point Positioning using IGS Orbit Products. Geodetic Survey Division, Natural Resources Canada.</ref>.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>The ocean loading is more localised than the solid earth tides and for convention it does not have permanent part. For kinematic PPP (see [[Code and Carrier Based Positioning (PPP)]]) at the few centimetres accuracy level or few millimetres static PPP over <math>24</math> hours and/or far from the oceans, it can be neglected [Kouba and <ins style="font-weight: bold; text-decoration: none;">H\'eroux</ins>., 2000] <ref>[Kouba and H\'eroux., 2000] Kouba, J. and <ins style="font-weight: bold; text-decoration: none;">H\'eroux</ins>., 2000. GPS Precise Point Positioning using IGS Orbit Products. Geodetic Survey Division, Natural Resources Canada.</ref>.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>A model for the ocean loading is described in the IERS Conventions document [Denis et al., 2004] <ref>[Denis et al., 2004] Denis, D., McCarthy and Petit, G., 2004. IERS Conventions (2003). IERS Technical Note 32.. IERS Convention Center., Frankfurt am Main.</ref>, page 73, whose simplified version can be summarised as <ref group="footnotes"> Additional information describing the model of GIPSY-OASIS II can be found in [Webb and Zumberge, 1993]</ref><ref>[Webb and Zumberge, 1993] Webb, F. and Zumberge, J., 1993. An Introduction to GIPSY/OASIS-II. Jet Propulsion Laboratory, JPL, 4800 Oak Grove Drive, Pasadena, CA 91109</ref>:</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>A model for the ocean loading is described in the IERS Conventions document [Denis et al., 2004] <ref>[Denis et al., 2004] Denis, D., McCarthy and Petit, G., 2004. IERS Conventions (2003). IERS Technical Note 32.. IERS Convention Center., Frankfurt am Main.</ref>, page 73, whose simplified version can be summarised as <ref group="footnotes"> Additional information describing the model of GIPSY-OASIS II can be found in [Webb and Zumberge, 1993]</ref><ref>[Webb and Zumberge, 1993] Webb, F. and Zumberge, J., 1993. An Introduction to GIPSY/OASIS-II. Jet Propulsion Laboratory, JPL, 4800 Oak Grove Drive, Pasadena, CA 91109</ref>:</div></td></tr>
</table>
Jaume.Sanz
https://gssc.esa.int/navipedia/index.php?title=Ocean_loading&diff=11030&oldid=prev
Jaume.Sanz at 12:27, 6 February 2012
2012-02-06T12:27:16Z
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<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Older revision</td>
<td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Revision as of 12:27, 6 February 2012</td>
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<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>This is a secondary tidal effect, due to the elastic response of the earth's crust to ocean tides, producing deformation of the sea floor and a surface displacement of an adjacent land.</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>This is a secondary tidal effect, due to the elastic response of the earth's crust to ocean tides, producing deformation of the sea floor and a surface displacement of an adjacent land.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker" data-marker="−"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #ffe49c; vertical-align: top; white-space: pre-wrap;"><div>The ocean loading is more localised than the solid earth tides and for convention it does not have permanent part. For kinematic PPP (see [[Code and Carrier Based Positioning (PPP)]]) at the few centimetres accuracy level or few millimetres static PPP over <math>24</math> hours and/or far from the oceans, it can be neglected [Kouba and H_eroux., 2000] <ref>[Kouba and <del style="font-weight: bold; text-decoration: none;">H_eroux</del>., 2000] Kouba, J. and H_eroux., 2000. GPS Precise Point Positioning using IGS Orbit Products. Geodetic Survey Division, Natural Resources Canada.</ref>.</div></td><td class="diff-marker" data-marker="+"></td><td style="color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #a3d3ff; vertical-align: top; white-space: pre-wrap;"><div>The ocean loading is more localised than the solid earth tides and for convention it does not have permanent part. For kinematic PPP (see [[Code and Carrier Based Positioning (PPP)]]) at the few centimetres accuracy level or few millimetres static PPP over <math>24</math> hours and/or far from the oceans, it can be neglected [Kouba and H_eroux., 2000] <ref>[Kouba and <ins style="font-weight: bold; text-decoration: none;">H\'eroux</ins>., 2000] Kouba, J. and H_eroux., 2000. GPS Precise Point Positioning using IGS Orbit Products. Geodetic Survey Division, Natural Resources Canada.</ref>.</div></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><br></td></tr>
<tr><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>A model for the ocean loading is described in the IERS Conventions document [Denis et al., 2004] <ref>[Denis et al., 2004] Denis, D., McCarthy and Petit, G., 2004. IERS Conventions (2003). IERS Technical Note 32.. IERS Convention Center., Frankfurt am Main.</ref>, page 73, whose simplified version can be summarised as <ref group="footnotes"> Additional information describing the model of GIPSY-OASIS II can be found in [Webb and Zumberge, 1993]</ref><ref>[Webb and Zumberge, 1993] Webb, F. and Zumberge, J., 1993. An Introduction to GIPSY/OASIS-II. Jet Propulsion Laboratory, JPL, 4800 Oak Grove Drive, Pasadena, CA 91109</ref>:</div></td><td class="diff-marker"></td><td style="background-color: #f8f9fa; color: #202122; font-size: 88%; border-style: solid; border-width: 1px 1px 1px 4px; border-radius: 0.33em; border-color: #eaecf0; vertical-align: top; white-space: pre-wrap;"><div>A model for the ocean loading is described in the IERS Conventions document [Denis et al., 2004] <ref>[Denis et al., 2004] Denis, D., McCarthy and Petit, G., 2004. IERS Conventions (2003). IERS Technical Note 32.. IERS Convention Center., Frankfurt am Main.</ref>, page 73, whose simplified version can be summarised as <ref group="footnotes"> Additional information describing the model of GIPSY-OASIS II can be found in [Webb and Zumberge, 1993]</ref><ref>[Webb and Zumberge, 1993] Webb, F. and Zumberge, J., 1993. An Introduction to GIPSY/OASIS-II. Jet Propulsion Laboratory, JPL, 4800 Oak Grove Drive, Pasadena, CA 91109</ref>:</div></td></tr>
</table>
Jaume.Sanz