http://wiki.baw.de/en/index.php?action=history&feed=atom&title=Satellite_altimetry 2026-04-15T00:15:46Z Revision history for this page on the wiki MediaWiki 1.43.5 http://wiki.baw.de/en/index.php?title=Satellite_altimetry&diff=5731&oldid=prev 2017-05-05T13:43:03Z

<p>Edited by Wikibot</p> <table style="background-color: #fff; color: #202122;" data-mw="interface"> <col class="diff-marker" /> <col class="diff-content" /> <col class="diff-marker" /> <col class="diff-content" /> <tr class="diff-title" lang="en"> <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 13:43, 5 May 2017</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l1">Line 1:</td> <td colspan="2" class="diff-lineno">Line 1:</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>{{GlossaryEntry</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>{{GlossaryEntry</div></td></tr> <tr><td colspan="2" class="diff-side-deleted"></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><ins style="font-weight: bold; text-decoration: none;">|definition=A method of satellite remote sensing with the aim of deriving the sea level. Radar pulses are transmitted from a satellite and received again after reflection on the water surface. For the duration of the pulses, the altitude of the satellite is determined above the sea surface. At the same time the satellite's altitude can be calculated from its position via the earth ellipsoid. The difference between the two measures amounts to the height of the sea level above the ellipsoid. This is composed of the so-called geoid height (it represents an average, calm sea) and the so-called marine topography together. For larger areas also inland waters and ice can be observed.</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;"><div>|name_de=Satellitenaltimetrie</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>|name_de=Satellitenaltimetrie</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><del style="font-weight: bold; text-decoration: none;">|definition=A method of satellite remote sensing with the aim of deriving the sea level. Radar pulses are transmitted from a satellite and received again after reflection on the water surface. For the duration of the pulses, the altitude of the satellite is determined above the sea surface. At the same time the satellite's altitude can be calculated from its position via the earth ellipsoid. The difference between the two measures amounts to the height of the sea level above the ellipsoid. This is composed of the so-called geoid height (it represents an average, calm sea) and the so-called marine topography together. For larger areas also inland waters and ice can be observed.</del></div></td><td colspan="2" class="diff-side-added"></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><del style="font-weight: bold; text-decoration: none;">|synonyme=</del></div></td><td colspan="2" class="diff-side-added"></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><del style="font-weight: bold; text-decoration: none;">|abkuerzungen=</del></div></td><td colspan="2" class="diff-side-added"></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><del style="font-weight: bold; text-decoration: none;">|quellen=</del></div></td><td colspan="2" class="diff-side-added"></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><del style="font-weight: bold; text-decoration: none;">|links=</del></div></td><td colspan="2" class="diff-side-added"></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>}}</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>}}</div></td></tr> </table>

imported>BAWiki Glossar http://wiki.baw.de/en/index.php?title=Satellite_altimetry&diff=5730&oldid=prev 2016-03-30T16:22:47Z

<p>GlossaryEntry</p> <p><b>New page</b></p><div>{{GlossaryEntry<br /> |name_de=Satellitenaltimetrie<br /> |definition=A method of satellite remote sensing with the aim of deriving the sea level. Radar pulses are transmitted from a satellite and received again after reflection on the water surface. For the duration of the pulses, the altitude of the satellite is determined above the sea surface. At the same time the satellite&#039;s altitude can be calculated from its position via the earth ellipsoid. The difference between the two measures amounts to the height of the sea level above the ellipsoid. This is composed of the so-called geoid height (it represents an average, calm sea) and the so-called marine topography together. For larger areas also inland waters and ice can be observed.<br /> |synonyme=<br /> |abkuerzungen=<br /> |quellen=<br /> |links=<br /> }}</div>

imported>BAWiki Glossar