sThe index of the North Atlantic Oscillation, the dominant mode of climatic variability in the North Atlantic region, changed in the late 1980s (1987e1989) from a negative to a positive re rel-l scale, limate ely cli-y short rily be behind hysical nt pro-ifferent s react
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| Format: | Text |
| Language: | English |
| Published: |
2005
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.573.7101 http://icesjms.oxfordjournals.org/content/62/7/1205.full.pdf |
| Summary: | sThe index of the North Atlantic Oscillation, the dominant mode of climatic variability in the North Atlantic region, changed in the late 1980s (1987e1989) from a negative to a positive re rel-l scale, limate ely cli-y short rily be behind hysical nt pro-ifferent s react |
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