A possible paleoclimatic enso indicator in the spatial variation of annual tree-ring C-14
Jirikowic, J.L. and Kalin, R. (1993) A possible paleoclimatic enso indicator in the spatial variation of annual tree-ring C-14. Geophysical Research Letters, 20 (6). pp. 439-442. ISSN 0094-8276
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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.
ORCID iDs
Jirikowic, J.L. and Kalin, R. ORCID: https://orcid.org/0000-0003-3768-3848;-
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Item type: Article ID code: 16301 Dates: DateEventMarch 1993PublishedSubjects: Technology > Engineering (General). Civil engineering (General) Department: Faculty of Engineering > Civil and Environmental Engineering Depositing user: Prof Robert M Kalin Date deposited: 17 Nov 2010 14:54 Last modified: 11 Nov 2024 09:14 URI: https://strathprints.strath.ac.uk/id/eprint/16301