https://wiki.bildungsserver.de/klimawandel/index.php?action=history&feed=atom&title=Datei%3AOcean_currents_N-Atlantic.jpeg 2026-04-25T14:00:49Z Versionsgeschichte dieser Seite in Klimawandel MediaWiki 1.45.3 https://wiki.bildungsserver.de/klimawandel/index.php?title=Datei:Ocean_currents_N-Atlantic.jpeg&diff=32636&oldid=prev 2024-12-22T19:46:59Z

<p></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="de-x-formal"> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">← Nächstältere Version</td> <td colspan="2" style="background-color: #fff; color: #202122; text-align: center;">Version vom 22. Dezember 2024, 19:46 Uhr</td> </tr><tr><td colspan="2" class="diff-lineno" id="mw-diff-left-l4">Zeile 4:</td> <td colspan="2" class="diff-lineno">Zeile 4:</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>{| style=&quot;border:1px solid #8888aa; background-color:#f7f8ff;padding:5px;font-size:95%;&quot;</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>{| style=&quot;border:1px solid #8888aa; background-color:#f7f8ff;padding:5px;font-size:95%;&quot;</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>|</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> <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>Quelle: von Schuckmann, K., et al. (2016): Copernicus Marine Service Ocean State Report, Journal of Operational Oceanography, 11:sup1,S1-S142, DOI: <del style="font-weight: bold; text-decoration: none;">10.1080/1755876X.2018.1489208, https://doi.org/</del>10.1080/1755876X.2018.1489208</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>Quelle: von Schuckmann, K., et al. (2016): <ins style="font-weight: bold; text-decoration: none;">[https://doi.org/10.1080/1755876X.2018.1489208 </ins>Copernicus Marine Service Ocean State Report<ins style="font-weight: bold; text-decoration: none;">]</ins>, Journal of Operational Oceanography, 11:sup1,S1-S142, DOI: 10.1080/1755876X.2018.1489208</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>&lt;br&gt;</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>&lt;br&gt;</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>Lizenz: Licensing: https://www.tandfonline.com/action/showCopyRight?scroll=top&amp;doi=10.1080%2F1755876X.2018.1489208 -&gt; <del style="font-weight: bold; text-decoration: none;">CC BY-NC-ND, </del>https://creativecommons.org/licenses/by-nc-nd/4.0/  </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>Lizenz: Licensing: https://www.tandfonline.com/action/showCopyRight?scroll=top&amp;doi=10.1080%2F1755876X.2018.1489208 -&gt; <ins style="font-weight: bold; text-decoration: none;">[</ins>https://creativecommons.org/licenses/by-nc-nd/4.0/ <ins style="font-weight: bold; text-decoration: none;">CC BY-NC-ND] </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>|}</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>

Dieter Kasang https://wiki.bildungsserver.de/klimawandel/index.php?title=Datei:Ocean_currents_N-Atlantic.jpeg&diff=32635&oldid=prev 2024-12-22T19:44:54Z

<p>== Beschreibung == Meeresströmungen im Nordatlantik: Die nach Norden fließenden Oberflächenströmungen sind in Rot dargestellt (NwASC=Norwegian Atlantic slope current, NwAFC=Norwegian Atlantic front current), die nach Süden fließenden kalten Tiefenströmungen in Schwarz. Grün wird der durch geringen Salzgehalt gekennzeichnete norwegische Küstenstrom (NCC=Norwegian Coastal Current), blau der oberflächennahe kalte Grönland-Strom gekennzeichnet. FS: Fram Strait, BSO: Barents Sea Open, DS: Denmark S…</p> <p><b>Neue Seite</b></p><div>== Beschreibung ==<br /> Meeresströmungen im Nordatlantik: Die nach Norden fließenden Oberflächenströmungen sind in Rot dargestellt (NwASC=Norwegian Atlantic slope current, NwAFC=Norwegian Atlantic front current), die nach Süden fließenden kalten Tiefenströmungen in Schwarz. Grün wird der durch geringen Salzgehalt gekennzeichnete norwegische Küstenstrom (NCC=Norwegian Coastal Current), blau der oberflächennahe kalte Grönland-Strom gekennzeichnet. FS: Fram Strait, BSO: Barents Sea Open, DS: Denmark Strait, FCC: Faroe-Shetland Channel<br /> ==Lizenzhinweis==<br /> {| style=&quot;border:1px solid #8888aa; background-color:#f7f8ff;padding:5px;font-size:95%;&quot;<br /> |<br /> Quelle: von Schuckmann, K., et al. (2016): Copernicus Marine Service Ocean State Report, Journal of Operational Oceanography, 11:sup1,S1-S142, DOI: 10.1080/1755876X.2018.1489208, https://doi.org/10.1080/1755876X.2018.1489208<br /> &lt;br&gt;<br /> Lizenz: Licensing: https://www.tandfonline.com/action/showCopyRight?scroll=top&amp;doi=10.1080%2F1755876X.2018.1489208 -&gt; CC BY-NC-ND, https://creativecommons.org/licenses/by-nc-nd/4.0/ <br /> |}</div>

Dieter Kasang