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Record #125154:

Reconstruction of atmospheric CO₂ and δ13CO₂ over the last 1000 years from air of the GISP2 ice core / M. Wahlen, D. Mastroianni, B. Deck, R. Bacastow.

Title: Reconstruction of atmospheric CO₂ and δ13CO₂ over the last 1000 years from air of the GISP2 ice core / M. Wahlen, D. Mastroianni, B. Deck, R. Bacastow.
Author(s): Wahlen, M.
Mastroianni, D.
Deck, B.
Bacastow, R.
Date: 1993.
In: Eos : transactions, American Geophysical Union. (1993.), Vol. 74(43, supplement) (1993)
Abstract: Abstract. CO₂ mixing ratio was measured in air of Greenland Ice Sheet Project 2 ice core for period between 1600 and 1100 AD. Changes broadly paralleled temperature variations reconstructed for northern Europe; thus atmospheric CO₂ appears to have been lower during Little Ice Age than during Medieval Climatic Optimum. δ ¹³CO₂ between 1600 and 1100 AD was also investigated and carbon cycle model used to examine CO₂ and δ¹³CO₂ variations.
Notes:

Eos : transactions, American Geophysical Union. Vol. 74(43, supplement) :78 (1993).

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.82 -- Bubbles in glaciers and ice.
546.264-31 -- Carbon dioxide.
551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.
622.14 -- Core sampling, ice and snow.
551.58 -- Climatology.
551.583 -- Climatic changes.
551.583.2 -- Climatic changes, historic.
001.89 -- Research programmes: Greenland Ice Sheet Project 2 (GISP2).
E9 -- Glaciology: meteorology and climatology.
(*38) -- Greenland.
SPRI record no.: 125154

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245 00 ‡aReconstruction of atmospheric CO₂ and δ13CO₂ over the last 1000 years from air of the GISP2 ice core /‡cM. Wahlen, D. Mastroianni, B. Deck, R. Bacastow.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1993.
300 ## ‡ap. 78.
500 ## ‡aEos : transactions, American Geophysical Union. Vol. 74(43, supplement) :78 (1993).
520 3# ‡aAbstract. CO₂ mixing ratio was measured in air of Greenland Ice Sheet Project 2 ice core for period between 1600 and 1100 AD. Changes broadly paralleled temperature variations reconstructed for northern Europe; thus atmospheric CO₂ appears to have been lower during Little Ice Age than during Medieval Climatic Optimum. δ ¹³CO₂ between 1600 and 1100 AD was also investigated and carbon cycle model used to examine CO₂ and δ¹³CO₂ variations.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.82 -- Bubbles in glaciers and ice.‡2udc
650 07 ‡a546.264-31 -- Carbon dioxide.‡2udc
650 07 ‡a551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.‡2udc
650 07 ‡a622.14 -- Core sampling, ice and snow.‡2udc
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.583.2 -- Climatic changes, historic.‡2udc
650 07 ‡a001.89 -- Research programmes: Greenland Ice Sheet Project 2 (GISP2).‡2udc
650 07 ‡aE9 -- Glaciology: meteorology and climatology.‡2local
651 #7 ‡a(*38) -- Greenland.‡2udc
700 1# ‡aWahlen, M.
700 1# ‡aMastroianni, D.
700 1# ‡aDeck, B.
700 1# ‡aBacastow, R.
773 0# ‡7nnas ‡tEos : transactions, American Geophysical Union. ‡gVol. 74(43, supplement) (1993) ‡wSPRI-1028
917 ## ‡aUnenhanced record from Muscat, imported 2019
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