跳至內容

File:Five Myr Climate Change.png

頁面內容不支援其他語言。
這個檔案來自維基共享資源
維基百科,自由的百科全書

Five_Myr_Climate_Change.png (745 × 224 像素,檔案大小:18 KB,MIME 類型:image/png


摘要

描述

reconstruction of the past 5 million years of climate history, based on oxygen isotope fractionation (serving as a proxy for the total global mass of glacial ice sheets). See the discussion below for a summary of the methods and models used.

Note that in 2010, User:SeL media switched the orientation of the time axis and the vertical axes, apparently without discussion, and some descriptions of the image may refer to the older version, resulting in confusion of 'right' and 'left' in the image.
日期
來源 original image by User:Dragons flight, based on data (figure 4?) from Lisiecki and Raymo (2005)
作者 Dragons flight (Robert A. Rohde)
授權許可
(重用此檔案)
This figure was prepared by Robert A. Rohde based on published data and is incorporated into the Global Warming Art project.
其他版本 vector versions (note the loss in graph resolution, do not use!): Five Myr Climate Change.svg, File:Five Myr Climate Change-ml.svg, Five Myr Climate Change (de) File:Vijf miljoen jaar zuurstofisotopen.svg

Discussion

Expansion of changes during the recent sequence of glacials and interglacials
Climate change during the last 65 million years

This figure shows the climate record of Lisiecki and Raymo (2005) [1] constructed by combining measurements from 57 globally distributed deep sea sediment cores. The measured quantity is oxygen isotope fractionation (δ18O) in benthic foraminifera, which serves as a proxy for the total global mass of glacial ice sheets.

Lisiecki and Raymo constructed this record by first applying a computer aided process of adjusting individual "wiggles" in each sediment core to have the same alignment (i.e. wiggle matching). Then the resulting stacked record is orbitally tuned by adjusting the positions of peaks and valleys to fall at times consistent with an orbitally driven ice model (see Milankovitch cycles). Both sets of these adjustments are constrained to be within known uncertainties on sedimentation rates and consistent with independently dated tie points (if any). Constructions of this kind are common. However, they assume that ice volume is driven by changes in insolation, and such data therefore cannot be used to establish the existence of such a relationship.

Many studies have produced evidence that the two strongest orbital cycles (obliquity, 41 kyr and precession, 26 kyr) probably do drive changes in ice volume. The data in the figure have been fitted to these periods and also to the longer, much weaker 100 kyr eccentricity cycle. Over the past ~1 million years there have been a number of very strong glacial maxima and minima, spaced by 80,000 - 120,000 years, but the evidence for orbital forcing of these events is less secure. It is likely that this ~100 kyr cycle is controlled by some other as yet unknown mechanism. For further discussion of orbital periodicities see Milankovitch cycles.

The observed isotope variations are very similar in shape to the temperature variations recorded at Vostok, Antarctica during the 420 kyr for which that record exists. Hence the right hand scale of the figure was established by fitting the reported temperature variations at Vostok (Petit et al. 1999) to the observed isotope variations. This temperature scale should be regarded as approximate and its magnitude only representative of the changes observed in the Vostok core. In particular, temperature changes at polar sites such as Vostok frequently exceed the changes observed in the tropics or in the global average. A horizontal line at 0 °C indicates modern temperatures (circa 1950).


References

  • Supplement: Lisiecki, L. E.; Raymo, M. E. (2005). "Pliocene-Pleistocene stack of globally distributed benthic stable oxygen isotope records". Pangaea. DOI:10.1594/PANGAEA.704257.
  • Lisiecki, L. E.; Raymo, M. E. (May 2005). "Correction to “A Pliocene-Pleistocene stack of 57 globally distributed benthic d18O records”". Paleoceanography: PA2007. DOI:10.1029/2005PA001164.
  • Petit, J. R.; Jouzel, J.; Raynaud, D.; Barkov, N. I.; Barnola, J. M.; Basile, I.; Bender, M.; Chappellaz, J.; Davis, J.; Delaygue, G.; Delmotte, M.; Kotlyakov, V. M.; Legrand, M.; Lipenkov, V.; Lorius, C.; Pépin, L.; Ritz, C.; Saltzman, E.; Stievenard, M. (1999). "Climate and Atmospheric History of the Past 420,000 years from the Vostok Ice Core, Antarctica". Nature 399: 429-436. DOI:10.1038/20859.


Image from Global Warming Art
This image is an original work created for Global Warming Art. Please refer to the image description page for more information.
GNU head 已授權您依據自由軟體基金會發行的無固定段落、封面文字和封底文字GNU自由文件授權條款1.2版或任意後續版本,對本檔進行複製、傳播和/或修改。該協議的副本列在GNU自由文件授權條款中。
w:zh:共享創意
姓名標示 相同方式分享
此檔案採用共享創意 姓名標示-相同方式分享 3.0 未在地化版本授權條款。
您可以自由:
  • 分享 – 複製、發佈和傳播本作品
  • 重新修改 – 創作演繹作品
惟需遵照下列條件:
  • 姓名標示 – 您必須指名出正確的製作者,和提供授權條款的連結,以及表示是否有對內容上做出變更。您可以用任何合理的方式來行動,但不得以任何方式表明授權條款是對您許可或是由您所使用。
  • 相同方式分享 – 如果您利用本素材進行再混合、轉換或創作,您必須基於如同原先的相同或兼容的條款,來分布您的貢獻成品。
已新增授權條款標題至此檔案,作為GFDL授權更新的一部份。



Dragons flight's Temperature Record Series
This figure is part of a series of plots created by Dragons flight to illustrate
changes in Earth's temperature and climate across many different time scales.
Time Period: 25 yrs | 150 yrs | 1 kyr | 2 kyr | 12 kyr | 450 kyr | 5 Myr | 65 Myr | 500 Myr
For articles related to this topic see: Temperature record

說明

添加單行說明來描述出檔案所代表的內容

在此檔案描寫的項目

描繪內容

著作權狀態 繁體中文 (已轉換拼寫)

有著作權 繁體中文 (已轉換拼寫)

多媒體型式 繁體中文 (已轉換拼寫)

image/png

檔案歷史

點選日期/時間以檢視該時間的檔案版本。

日期/時間縮⁠圖尺寸用戶備⁠註
目前2010年7月18日 (日) 13:25於 2010年7月18日 (日) 13:25 版本的縮圖745 × 224(18 KB)SeL mediatime axis reversed
2009年7月4日 (六) 22:40於 2009年7月4日 (六) 22:40 版本的縮圖745 × 224(17 KB)FalcorianLossless compression with pngout.
2005年12月7日 (三) 10:27於 2005年12月7日 (三) 10:27 版本的縮圖745 × 224(22 KB)JoonaslClimate changes over the last 5 million years. Diagram by [http://fi.wikipedia.org/wiki/K%C3%A4ytt%C3%A4j%C3%A4:Merikanto Merikanto] {{GFDL}} Category:Global warming

下列頁面有用到此檔案:

全域檔案使用狀況

以下其他 wiki 使用了這個檔案:

檢視此檔案的更多全域使用狀況