File:MilankovitchCyclesOrbitandCores-sr.png

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Српски / srpski: Орбитални параметри за Земљу:

http://aom.giss.nasa.gov/srorbpar.html

Израчунавање осунчаности се врши помоћу орбиталних параметара

Подаци за Восточко ледено језгро:

  • Petit, J.R., et al., 2001,

Vostok Ice Core Data for 420,000 Years, IGBP PAGES/World Data Center for Paleoclimatology Data Contribution Series #2001-076. NOAA/NGDC Paleoclimatology Program, Boulder CO, USA. ftp://ftp.ncdc.noaa.gov/pub/data/paleo/icecore/antarctica/vostok/deutnat.txt Температурска реконструкција је понуђена заједно са сетом података.

Подаци за бентоску фораминиферу:

  • Lisiecki, L. E., and M. E. Raymo (2005), A Pliocene-

Pleistocene stack of 57 globally distributed benthic d18O records, Paleoceanography,20, PA1003, doi:10.1029/2004PA001071. http://lorraine-lisiecki.com/stack.html

Дефинитивна температурска реконструкција није понуђена заједно са сетом података. Понуђена је на: http://lorraine-lisiecki.com/thesis_appendix.html#2-Appendix-B-The-d18O-of-Foraminifera где се налази тврдња:

„Велика промена у делу за d18Oc белешке мисли се да резултује секвестрацијом изотопски лаког кисеоника (16O) у великим континенталним леденим плочама у океанским водама које имају велик удео 18O.”
Према томе, редукција кисеоника 18 (која је према горе на графику) указује на топлије услове и већу надморску висину.
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Other versions File:MilankovitchCyclesOrbitandCores-sr.png
File:MilankovitchCyclesOrbitandCoresRecaptioned.png, File:MilankovitchCyclesOrbitandCoresRecaptioned-sr.png
File:Milankovic.jpg, File:Milankovic-sr.jpg

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current08:37, 30 September 2016Thumbnail for version as of 08:37, 30 September 20161,000 × 1,044 (125 KB)Cmdrjameson (talk | contribs)Compressed with pngout. Reduced by 69kB (35% decrease).
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