Bray cycle effects.pdf
Summary of the climatic effects of low solar activity associated to the Bray 2500-year cycle. Most effects derive from an atmospheric reorganization that contracts the Hadley cells and expands the Polar cells steepening the latitudinal temperature gradient and causing global cooling. Monsoon pattern...
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ftdatacite:10.6084/m9.figshare.7831244 2023-05-15T16:21:23+02:00 Bray cycle effects.pdf Vinós, Javier 2019 https://dx.doi.org/10.6084/m9.figshare.7831244 https://figshare.com/articles/Bray_cycle_effects_pdf/7831244 unknown figshare Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Climate Science Image Figure graphic ImageObject 2019 ftdatacite https://doi.org/10.6084/m9.figshare.7831244 2021-11-05T12:55:41Z Summary of the climatic effects of low solar activity associated to the Bray 2500-year cycle. Most effects derive from an atmospheric reorganization that contracts the Hadley cells and expands the Polar cells steepening the latitudinal temperature gradient and causing global cooling. Monsoon patterns are restricted, causing sub-tropical drying. El Niño is less frequent altering global precipitation patterns. The North Atlantic displays more AO/NAO winter negative conditions shifting the winter European storm track southwards. Weaker westerlies reduce the sub-polar gyre contribution to the North Atlantic current, increasing winter precipitation over Scandinavia and promoting glacier growth. A stronger Siberian High activates polar circulation and southward drift-ice, cooling northern Eurasia. Greenland undergoes a temperature inversion. Black dots represent proxy locations displaying a prominent 2500-year periodicity. Still Image glacier Greenland north atlantic current North Atlantic DataCite Metadata Store (German National Library of Science and Technology) Bray ENVELOPE(-114.067,-114.067,-74.833,-74.833) Greenland |
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DataCite Metadata Store (German National Library of Science and Technology) |
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topic |
Climate Science |
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Climate Science Vinós, Javier Bray cycle effects.pdf |
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Climate Science |
description |
Summary of the climatic effects of low solar activity associated to the Bray 2500-year cycle. Most effects derive from an atmospheric reorganization that contracts the Hadley cells and expands the Polar cells steepening the latitudinal temperature gradient and causing global cooling. Monsoon patterns are restricted, causing sub-tropical drying. El Niño is less frequent altering global precipitation patterns. The North Atlantic displays more AO/NAO winter negative conditions shifting the winter European storm track southwards. Weaker westerlies reduce the sub-polar gyre contribution to the North Atlantic current, increasing winter precipitation over Scandinavia and promoting glacier growth. A stronger Siberian High activates polar circulation and southward drift-ice, cooling northern Eurasia. Greenland undergoes a temperature inversion. Black dots represent proxy locations displaying a prominent 2500-year periodicity. |
format |
Still Image |
author |
Vinós, Javier |
author_facet |
Vinós, Javier |
author_sort |
Vinós, Javier |
title |
Bray cycle effects.pdf |
title_short |
Bray cycle effects.pdf |
title_full |
Bray cycle effects.pdf |
title_fullStr |
Bray cycle effects.pdf |
title_full_unstemmed |
Bray cycle effects.pdf |
title_sort |
bray cycle effects.pdf |
publisher |
figshare |
publishDate |
2019 |
url |
https://dx.doi.org/10.6084/m9.figshare.7831244 https://figshare.com/articles/Bray_cycle_effects_pdf/7831244 |
long_lat |
ENVELOPE(-114.067,-114.067,-74.833,-74.833) |
geographic |
Bray Greenland |
geographic_facet |
Bray Greenland |
genre |
glacier Greenland north atlantic current North Atlantic |
genre_facet |
glacier Greenland north atlantic current North Atlantic |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.6084/m9.figshare.7831244 |
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1766009390867939328 |