https://wiki.bildungsserver.de/klimawandel/index.php?action=history&feed=atom&title=Datei%3AHolocene_warming_cooling.jpg 2026-04-25T19:47:07Z Versionsgeschichte dieser Seite in Klimawandel MediaWiki 1.45.3 https://wiki.bildungsserver.de/klimawandel/index.php?title=Datei:Holocene_warming_cooling.jpg&diff=32512&oldid=prev 2024-12-15T17:19:49Z

<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 15. Dezember 2024, 17:19 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: <del style="font-weight: bold; text-decoration: none;">Kaufman</del>, <del style="font-weight: bold; text-decoration: none;">D</del>., N. McKay, <del style="font-weight: bold; text-decoration: none;">C</del>. <del style="font-weight: bold; text-decoration: none;">Routson, </del>et al. (<del style="font-weight: bold; text-decoration: none;">2020</del>): [https://doi.org/10.<del style="font-weight: bold; text-decoration: none;">1038</del>/<del style="font-weight: bold; text-decoration: none;">s41597</del>-<del style="font-weight: bold; text-decoration: none;">020</del>-<del style="font-weight: bold; text-decoration: none;">0530</del>-<del style="font-weight: bold; text-decoration: none;">7 </del>Holocene <del style="font-weight: bold; text-decoration: none;">global mean surface temperature</del>, <del style="font-weight: bold; text-decoration: none;">a multi-method reconstruction approach]</del>. <del style="font-weight: bold; text-decoration: none;">Scientific Data 7:201</del>&lt;br&gt;</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: <ins style="font-weight: bold; text-decoration: none;">Erb</ins>, <ins style="font-weight: bold; text-decoration: none;">M.P</ins>., N<ins style="font-weight: bold; text-decoration: none;">.P</ins>. McKay, <ins style="font-weight: bold; text-decoration: none;">N</ins>. <ins style="font-weight: bold; text-decoration: none;">Steiger </ins>et al. (<ins style="font-weight: bold; text-decoration: none;">2022</ins>): [https://doi.org/10.<ins style="font-weight: bold; text-decoration: none;">5194</ins>/<ins style="font-weight: bold; text-decoration: none;">cp</ins>-<ins style="font-weight: bold; text-decoration: none;">18</ins>-<ins style="font-weight: bold; text-decoration: none;">2599</ins>-<ins style="font-weight: bold; text-decoration: none;">2022 Reconstructing </ins>Holocene <ins style="font-weight: bold; text-decoration: none;">temperatures in time and space using paleoclimate data assimilation]</ins>, <ins style="font-weight: bold; text-decoration: none;">Clim</ins>. <ins style="font-weight: bold; text-decoration: none;">Past, 18, 2599–2629</ins>&lt;br&gt;</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>Lizenz: [http://creativecommons.org/licenses/by/4.0/ CC BY 4.0]   </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>Lizenz: [http://creativecommons.org/licenses/by/4.0/ CC BY 4.0]   </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:Holocene_warming_cooling.jpg&diff=32511&oldid=prev 2024-12-15T17:18:35Z

<p>== Beschreibung == Änderung der globalen Mitteltemperatur in der ersten und zweiten Hälfte des Holozäns bzw. vor und nach 6000 vh. Die schwarzen Punkte markieren Fundstellen von Proxydaten. Referenzperiode: 3.000 – 5.000 Jahre vh. Bitte die unterschiedlichen Skalen in beiden Abb. beachten! ==Lizenzhinweis== {| style=&quot;border:1px solid #8888aa; background-color:#f7f8ff;padding:5px;font-size:95%;&quot; | Quelle: Kaufman, D., N. McKay, C. Routson, et al. (2020): [https://doi.org/10.1038/s41597-020-0530-…</p> <p><b>Neue Seite</b></p><div>== Beschreibung ==<br /> Änderung der globalen Mitteltemperatur in der ersten und zweiten Hälfte des Holozäns bzw. vor und nach 6000 vh. Die schwarzen Punkte markieren Fundstellen von Proxydaten. Referenzperiode: 3.000 – 5.000 Jahre vh. Bitte die unterschiedlichen Skalen in beiden Abb. beachten!<br /> ==Lizenzhinweis==<br /> {| style=&quot;border:1px solid #8888aa; background-color:#f7f8ff;padding:5px;font-size:95%;&quot;<br /> |<br /> Quelle: Kaufman, D., N. McKay, C. Routson, et al. (2020): [https://doi.org/10.1038/s41597-020-0530-7 Holocene global mean surface temperature, a multi-method reconstruction approach]. Scientific Data 7:201&lt;br&gt;<br /> Lizenz: [http://creativecommons.org/licenses/by/4.0/ CC BY 4.0] <br /> |}</div>

Dieter Kasang