Category:Wood - Revision history

Admin: Undo revision 87652 by Admin (talk)

2020-11-12T16:01:52Z

Undo revision 87652 by Admin (talk)

Admin: WTBootstrap: New Category Wood

2020-11-12T15:26:22Z

WTBootstrap: New Category Wood

Admin: /* Datasets based on Wood Archives */

2017-07-21T23:11:21Z

‎Datasets based on Wood Archives

New page

__NOCACHE__

===Category: Wood [http://linked.earth/ontology#Wood]===

Imported from: [[imported from::core:Wood]]

The field of [https://en.wikipedia.org/wiki/Dendroclimatology dendroclimatology] and, to some extent, the field of [[Dendrochronology | dendrochronology]] have played an important role in generating climate reconstructions of the past millennium <ref> Mann, M. E., Bradley, R. S., & Hughes, M. K. (1998). Global-scale temperature patterns and climate forcing over the past six centuries. Nature, 392(6678), 779-787. doi:10.1038/33859 </ref> <ref>Mann, M. E., Bradley, R. S., & Hughes, M. K. (1999). Northern Hemipshere temperatures during the past millennium: Inferences, Uncertainties, and Limitations. Geophysical Research Letters, 26(6), 759. </ref> <ref>Moberg, A., Sonechkin, D. M., Holmgren, K., Datsenko, N. M., & Karlen, W. (2005). Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data. Nature, 433(7026), 613-617. doi:10.1038/nature03265</ref> <ref>Mann, M. E., Zhang, Z., Rutherford, S., Bradley, R., Hughes, M. K., Shindell, D. T., . . . Ni, F. (2009). Global signatures and dynamical origins of the Little Ice Age and Medieval Climate Anomaly. Science, 326, 1256-1260. dos: 10.1126/science.1177303</ref>. In regions with large seasonal variations, trees produce rings of varying color depending on the species. In most cases, the rings shift from a lighter, low density early wood of spring and early summer to a darker, denser band of late wood at the end of the growing season. The growing season generally occurs during the summer month and its length depends on the species, latitude, and altitude. Therefore, trees hold perhaps the greatest potential for reconstructing past terrestrial climates at annual or even sub-annual resolution.
The following observations can be made on the wood archive:

* Tree ring width
* Wood density
* [[Stable Isotopes in trees | Stables isotopes]]

== Datasets based on Wood Archives==

Currently, the LinkedEarth wiki hosts {{#ask:
[[Category:Dataset_(L)]]
[[IncludesPaleoData_(L).FoundInMeasurementTable_(L).IncludesVariable_(L).HasProxySystem_(L).ProxyArchiveType_(L)::Wood]]
| format = count
}} datasets based on wood archives.



{{#ask:
[[Category:Dataset_(L)]]
[[IncludesPaleoData_(L).FoundInMeasurementTable_(L).IncludesVariable_(L).HasProxySystem_(L).ProxyArchiveType_(L)::Wood]] OR [[Category:Location_(L)]] [[CoordinatesFor.ArchiveType::tree]]
| ?CollectedFrom_(L).Coordinates
| ?Name_(L)
| ?IncludesPaleoData_(L).FoundInMeasurementTable_(L).IncludesVariable_(L).ProxyObservationType_(L)
| showtitle=off
| maxzoom=14
| minzoom=1
| limit=500
| template=ByArchiveLocation
| format=leaflet
}}

==References==
<references />


Category Semantics
* Sub-Class of
** [[subcategory of::Category:ProxyArchive (L)]]

[[Category:ProxyArchive (L)]]

@@ Line 1: / Line 1: @@
 ===Category: Wood [http://linked.earth/ontology#Wood]===
 Imported from: [[imported from::core:Wood]]
-<p>The field of [https://en.wikipedia.org/wiki/Dendroclimatology dendroclimatology] and, to some extent, the field of [#cite_note-1 [1]]</sup> <sup id="cite_ref-2" class="reference">[#cite_note-3 [3]]</sup> <sup id="cite_ref-4" class="reference"><a href="#cite_note-4">[4]</a></sup>. In regions with large seasonal variations, trees produce rings of varying color depending on the species. In most cases, the rings shift from a lighter, low density early wood of spring and early summer to a darker, denser band of late wood at the end of the growing season. The growing season generally occurs during the summer month and its length depends on the species, latitude, and altitude. Therefore, trees  hold perhaps the greatest potential for reconstructing past terrestrial climates at annual or even sub-annual resolution.
+The field of [https://en.wikipedia.org/wiki/Dendroclimatology dendroclimatology] and, to some extent, the field of [[Dendrochronology | dendrochronology]] have played an important role in generating climate reconstructions of the past millennium <ref> Mann, M. E., Bradley, R. S., & Hughes, M. K. (1998). Global-scale temperature patterns and climate forcing over the past six centuries. Nature, 392(6678), 779-787. doi:10.1038/33859 </ref> <ref>Mann, M. E., Bradley, R. S., & Hughes, M. K. (1999). Northern Hemipshere temperatures during the past millennium: Inferences, Uncertainties, and Limitations. Geophysical Research Letters, 26(6), 759. </ref> <ref>Moberg, A., Sonechkin, D. M., Holmgren, K., Datsenko, N. M., & Karlen, W. (2005). Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data. Nature, 433(7026), 613-617. doi:10.1038/nature03265</ref> <ref>Mann, M. E., Zhang, Z., Rutherford, S., Bradley, R., Hughes, M. K., Shindell, D. T., . . . Ni, F. (2009). Global signatures and dynamical origins of the Little Ice Age and Medieval Climate Anomaly. Science, 326, 1256-1260. dos: 10.1126/science.1177303</ref>. In regions with large seasonal variations, trees produce rings of varying color depending on the species. In most cases, the rings shift from a lighter, low density early wood of spring and early summer to a darker, denser band of late wood at the end of the growing season. The growing season generally occurs during the summer month and its length depends on the species, latitude, and altitude. Therefore, trees  hold perhaps the greatest potential for reconstructing past terrestrial climates at annual or even sub-annual resolution.
-</p><p>The following observations can be made on the wood archive:
+The following observations can be made on the wood archive:
-</p>
-<ul><li> Tree ring width</li>
+* Tree ring width
-<li> Wood density</li>
+* Wood density
-<li> Stables isotopes<ol class="references"></li></ul><ol>
+* [[Stable Isotopes in trees | Stables isotopes]]
-<li id="cite_note-1"><span class="mw-cite-backlink"><a href="#cite_ref-1">?</a></span> <span class="reference-text"> Mann, M. E., Bradley, R. S., &amp; Hughes, M. K. (1998). Global-scale temperature patterns and climate forcing over the past six centuries. Nature, 392(6678), 779-787. doi:10.1038/33859 </span>
-</li>
+== Datasets based on Wood Archives==
-<li id="cite_note-2"><span class="mw-cite-backlink"><a href="#cite_ref-2">?</a></span> <span class="reference-text">Mann, M. E., Bradley, R. S., &amp; Hughes, M. K. (1999). Northern Hemipshere temperatures during the past millennium: Inferences, Uncertainties, and Limitations. Geophysical Research Letters, 26(6), 759. </span>
-</li>
+Currently, the LinkedEarth wiki hosts {{#ask:
-<li id="cite_note-3"><span class="mw-cite-backlink"><a href="#cite_ref-3">?</a></span> <span class="reference-text">Moberg, A., Sonechkin, D. M., Holmgren, K., Datsenko, N. M., &amp; Karlen, W. (2005). Highly variable Northern Hemisphere temperatures reconstructed from low- and high-resolution proxy data. Nature, 433(7026), 613-617. doi:10.1038/nature03265</span>
+[[Category:Dataset_(L)]]
-</li>
+[[IncludesPaleoData_(L).FoundInMeasurementTable_(L).IncludesVariable_(L).HasProxySystem_(L).ProxyArchiveType_(L)::Wood]]
-<li id="cite_note-4"><span class="mw-cite-backlink"><a href="#cite_ref-4">?</a></span> <span class="reference-text">Mann, M. E., Zhang, Z., Rutherford, S., Bradley, R., Hughes, M. K., Shindell, D. T., . . . Ni, F. (2009). Global signatures and dynamical origins of the Little Ice Age and Medieval Climate Anomaly. Science, 326, 1256-1260. dos: 10.1126/science.1177303</span>
+| format = count
-</li>
+}} datasets based on wood archives.
-</ol>
 <!-- Do not edit below this unless you know what you are doing -->