Persistent Solar Influence on North Atlantic Climate During the Holocene
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Summary
A solar forcing mechanism therefore may underlie at least the Holocene segment of the North Atlantic's “1500-year” cycle, potentially providing an additional mechanism for amplifying the solar signals and transmitting them globally.
- Type
- article
- Published
- 2001-11-15
- Cited by
- 3,368
- References
- 52
- OpenAlex
- https://openalex.org/W1990899433
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:38179371
Keywords
Holocene, Hydrography, Oceanography, Geology, Atlantic Equatorial mode
References
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- Changes in Atmospheric Carbon-14 Attributed to a Variable Sun
- Holocene Climatic Variations—Their Pattern and Possible Cause
- Solar Forcing of Regional Climate Change During the Maunder Minimum
- The Little Ice Age and Medieval Warm Period in the Sargasso Sea
- Variability of Fram Strait ice flux and North Atlantic Oscillation
- Climate, history, and the modern world
- VARIATIONS IN RADIOCARBON CONCENTRATION AND SUNSPOT ACTIVITY
- Little Ice Age clearly recorded in northern Greenland ice cores
- Past temperatures directly from the greenland ice sheet
- Global ice-volume fluctuations, North Atlantic ice-rafting events, and deep-ocean circulation changes between 130 and 70 ka
- Deglacial meltwater discharge, North Atlantic Deep Circulation, and abrupt climate change
- The Impact of Solar Variability on Climate
- Slope water current over the laurentian fan on interannual to millennial time scales
- Uptake of excess CO2 by an outcrop-diffusion model of the ocean
Cited by
- Atmospheric Production and Transport of Cosmogenic 7Be and 10Be
- Holocene glacial history of Renland Ice Cap, East Greenland, reconstructed from lake sediments
- Modern Climatology - Full Text
- Extinction may not be forever
- Late Quaternary ice-ocean interactions in central West Greenland
- High-Resolution Speleothem-Based Palaeoclimate Records From New Zealand Reveal Robust Teleconnection To North Atlantic During MIS 1-4
- The contemporary distribution of benthic foraminifera in the Pearl River estuary, southeast China, and their use in reconstructing mid‐ to late‐Holocene fluvial flux
- Role of climatic and anthropogenic factors accelerating soil erosion and fluvial activity in central Europe
- Late Pleistocene and Holocene hydroclimate change in the Southeastern United States: Sedimentary, pedogenic, and stable carbon isotope evidence in Tennessee River floodplain paleosols
- Plio-Pleistocene imprint of natural climate cycles in marine sediments
- Climate Change in Prehistory: The End of the Reign of Chaos
- Time-Series Analysis and Cyclostratigraphy: Acknowledgements
- High resolution stalagmite δ18O records over the past 1000 years from Dongge Cave in Guizhou
- Registros fluviales en la Península ibérica durante la Pequeña Edad del Hielo
- North Atlantic climate
- Analysis of soluble ions from dust and sea salt over the last glacial cycle in polar deep ice cores
- Natural Climate Change:A Geological Perspective
- Peatland responses to Holocene climate change in a temperate poor fen, northeastern Pennsylvania
- Climate Change and the Great Plague Pandemics of History: Causal Link between Global Climate Fluctuations and Yersinia Pestis Contagion?
- Adaptation and human migration, and evidence of agriculture coincident with changes in the Indian summer monsoon during the Holocene
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