ON THE LINK BETWEEN NORTHERN FENNOSCANDIAN CLIMATE AND LENGTH OF THE QUASI-ELEVEN-YEAR CYCLE IN GALACTIC COSMIC-RAY FLUX
Abstract. Bidecadal fluctuations in terrestrial climate were analyzed. It was shown that this variability might arise if Earth’s climate reacts to galactic cosmic-ray intensity, integrated over its full quasi-11-year cycle. It was further shown that this integral effect should also lead to an effect...
Main Authors: | , , , , , |
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Other Authors: | |
Format: | Text |
Language: | English |
Published: |
2002
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Subjects: | |
Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.306.3683 http://ruby.fgcu.edu/courses/twimberley/EnviroPhilo/Flux.pdf |
Summary: | Abstract. Bidecadal fluctuations in terrestrial climate were analyzed. It was shown that this variability might arise if Earth’s climate reacts to galactic cosmic-ray intensity, integrated over its full quasi-11-year cycle. It was further shown that this integral effect should also lead to an effective link between climate and the duration of the quasi-11-year cycle in cosmic ray flux. That, in turn, must result in appearance of some connection between climate and the length of the solar cycle, which is currently a topic of active debate. Analyses of temperature proxies, obtained for northern Fennoscandia, confirmed the connection of the climate in this region and the length of the cycle in galactic cosmic-ray intensity. Decadal and bidecadal variability of integrated cosmic-ray flux was |
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