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Record #116947:

Black carbon concentration in Byrd station ice core: from 700 to 12,900 BP / Petr Chýlek, B. Johnson, H. Wu.

Title: Black carbon concentration in Byrd station ice core: from 700 to 12,900 BP / Petr Chýlek, B. Johnson, H. Wu.
Author(s): Chýlek, Petr.
Johnson, B.
Wu, H.
Date: 1992.
In: Eos : transactions, American Geophysical Union. (1992.), Vol. 73(14, spring meeting supplement) (1992)
Abstract: Abstract only. Current concentration in fresh snow at South Pole is not higher than average Holocene concentration in Byrd samples, suggesting that anthropogenic black carbon production has not yet affected concentrations of soot in polar regions. At beginning of Holocene, there was probably increase in black carbon production because of increase in land biomass after Late Wisconsin ice age.
Notes:

Eos : transactions, American Geophysical Union. Vol. 73(14, spring meeting supplement) :107-108 (1992).

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.24 -- Ice sheets and caps.
551.324.84 -- Land ice, impurities.
54 -- Chemistry.
551.578.46 -- Snow cover and snow patches.
551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.
622.14 -- Core sampling, ice and snow.
E5 -- Glaciology: land ice.
(*7) -- Antarctic regions.
(*701) -- South Pole.
(*772) -- Byrd Land.
SPRI record no.: 116947

MARCXML

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001 SPRI-116947
005 20240329101619.0
007 ta
008 240329s1992####xx####|##|###|0||#0|eng#d
035 ## ‡aSPRI-116947
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aChýlek, Petr.
245 10 ‡aBlack carbon concentration in Byrd station ice core :‡bfrom 700 to 12,900 BP /‡cPetr Chýlek, B. Johnson, H. Wu.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1992.
300 ## ‡ap. 107-108.
500 ## ‡aEos : transactions, American Geophysical Union. Vol. 73(14, spring meeting supplement) :107-108 (1992).
520 3# ‡aAbstract only. Current concentration in fresh snow at South Pole is not higher than average Holocene concentration in Byrd samples, suggesting that anthropogenic black carbon production has not yet affected concentrations of soot in polar regions. At beginning of Holocene, there was probably increase in black carbon production because of increase in land biomass after Late Wisconsin ice age.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.24 -- Ice sheets and caps.‡2udc
650 07 ‡a551.324.84 -- Land ice, impurities.‡2udc
650 07 ‡a54 -- Chemistry.‡2udc
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡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 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*701) -- South Pole.‡2udc
651 #7 ‡a(*772) -- Byrd Land.‡2udc
700 1# ‡aJohnson, B.
700 1# ‡aWu, H.
773 0# ‡7nnas ‡tEos : transactions, American Geophysical Union. ‡gVol. 73(14, spring meeting supplement) (1992) ‡wSPRI-1028
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240329