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The 1991–1992 atmospheric methane anomaly: Southern hemisphere 13 C decrease and growth rate fluctuations
Author(s) -
Lowe David C.,
Manning Martin R.,
Brailsford G. W.,
Bromley A. M.
Publication year - 1997
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/97gl00830
Subject(s) - mixing ratio , anomaly (physics) , southern hemisphere , atmospheric sciences , growth rate , methane , amplitude , environmental science , atmospheric methane , northern hemisphere , mixing (physics) , climatology , physics , chemistry , geology , mathematics , geometry , organic chemistry , condensed matter physics , quantum mechanics
Measurements of atmospheric methane from 1989–1996 at Baring Head, New Zealand, and at Scott Base, Antarctica show a seasonal cycle in the mixing ratio with a peak to peak amplitude of 28 ppb. This is superposed on a trend varying between 16 ppb yr −1 and near zero. δ 13 C values also show a seasonal cycle, with an amplitude of 0.1–0.3‰, approximately 6 months out of phase with the mixing ratio cycle. A pronounced negative anomaly in δ 13 C occurred in 1992 with annual average values dropping from −47.08‰ to −47.28‰. From 1992 to 1996, average δ 13 C values recovered slowly at an average rate of about 0.04‰ yr −1 . The simultaneous changes in the mixing ratio growth rate and δ 13 C together with the rapid drop and slow recovery in the latter provide a stringent test of possible causes. Although a combination of causes cannot be ruled out, decreased emissions from an isotopically heavy source such as biomass burning best meet the constraints of the data.

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