Journal
GEOPHYSICAL RESEARCH LETTERS
Volume 35, Issue 5, Pages -Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2007GL032137
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Funding
- NERC [NE/E003990/1] Funding Source: UKRI
- Natural Environment Research Council [NE/E003990/1] Funding Source: researchfish
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The tropical tape recorder is an effect in which a seasonal cycle in the mixing ratio of a gas is imposed on air entering the stratosphere and is then transported upwards by the Brewer-Dobson circulation. We report the observation of this effect in the mixing ratio of HCN, as measured by two satellite instruments: MLS on Aura and ACE-FTS on SCISAT-1. The cycle does not repeat every year; the data so far suggest that the dominant period is about two years. The reason for this periodicity is not yet fully understood. Comparisons with MODIS fire-count data suggest that it may be connected to inter-annual variations in biomass burning in Indonesia and the surrounding region.
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