Abstract
Preliminary investigations show regional differences in atmospheric C-14 activity archived in tree-ring cellulose may reflect oceanic and atmospheric shifts associated with ENSO (El Nino-Southern Oscillation) events. Much of the shared variation between sites in Washington and Arizona can be attributed to global forcings such as anthropogenic
C-14-depleted CO2 emissions and modulation of C-14 production. The contrasted residual variation between the Washington and Arizona data sets correlates with the annual Southern Oscillation Index (SOI) of the previous year. The spatial differences between DELTAC-14 data sets may provide a proxy indicator of ENSO phenomenon.
Original language | English |
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Pages (from-to) | 439-442 |
Number of pages | 3 |
Journal | Geophysical Research Letters |
Volume | 20 |
Issue number | 6 |
Publication status | Published - Mar 1993 |
Keywords
- tree-ring cellulose
- oceanic and atmospheric shifts
- ENSO events
- El Nino-Southern Oscillation events