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Wind regime changes in the Euro-Atlantic region driven by Late-Holocene Grand Solar Minima

Wind regime changes in the Euro-Atlantic region driven by Late-Holocene Grand Solar Minima
Wind regime changes in the Euro-Atlantic region driven by Late-Holocene Grand Solar Minima
Understanding atmospheric response to radiative forcing, including the intensity and distribution of wind patterns is critical as this might have important implications in the coming decades. Long-term episodes of reduced solar activity (i.e. Grand Solar Minima, GSM) have triggered rapid climate change in the past, recorded in proxy-based records, including varved sediments from Meerfelder Maar, Germany, where the Homeric GSM (~2800 years ago) was studied. This study reconstructs windy conditions during the same GSM from Diss Mere, another varved record in England, to support the solar-wind linkage in the North Atlantic-European region. We use diatoms as proxies for windiness and support the palaeolimnological and palaeoclimate interpretation with a multi-proxy chironomids and pollen) evidence. The diatom assemblage documents a shift from Pantocsekiella ocellata dominance to Stephanodiscus parvus and Lindavia comta, indicating a shift to more turbulent waters from ~2767 ± 28, linked to increased windiness. This shift is synchronous with changes in 14C production, linked to solar activity changes during the GSM. Both proxy records reflect a rapid and synchronous atmospheric response (i.e. stronger winds) at the onset and during the GSM in the North Atlantic and continental Europe. In order to test whether this solar-wind linkage is consistent during other GSMs and to understand the underlying climate dynamics, we analyse the wind response to solar forcing at the two study sites during the Little Ice Age, a period that includes several GSMs. For this, we have used a reconstruction based on a 1200-year-long simulation with an isotope-enabled climate model. Our study suggests that wind anomalies in the North Atlantic-European sector may relate to an anomalous atmospheric circulation in response to long-term solar forcing leading to north-easterlies modulated by the East Atlantic pattern.
0930-7575
1947–1961
Harding, Poppy
216b91a1-95b2-41ed-83ac-c62c96cc87e6
Martin Puertas, Celia
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Sjolte, J
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Walsh, Amy
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Tjallingii, Rick
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Langdon, Catherine
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Blockley, Simon
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Brauer, Achim
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Langdon, Peter
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Milner, Alice
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Muscheler, Raymond
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Perez, M
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Harding, Poppy
216b91a1-95b2-41ed-83ac-c62c96cc87e6
Martin Puertas, Celia
89864d7e-1c95-483a-8e3e-03d86f333bcf
Sjolte, J
4fa21294-66b3-4ea3-8a1e-abe5c1b68efa
Walsh, Amy
e82ca48b-37b0-4e2a-accb-854dd6733b86
Tjallingii, Rick
aa9ffc4b-cbd0-4d36-9649-13c6f886ba04
Langdon, Catherine
628b8ce9-a413-4ebb-924f-fbeb7193a021
Blockley, Simon
29959874-6887-4339-a189-f6c4a4f5f38d
Brauer, Achim
b2d4982a-a387-4e4c-a65f-98b771e99c13
Langdon, Peter
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Milner, Alice
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Muscheler, Raymond
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Perez, M
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Harding, Poppy, Martin Puertas, Celia, Sjolte, J, Walsh, Amy, Tjallingii, Rick, Langdon, Catherine, Blockley, Simon, Brauer, Achim, Langdon, Peter, Milner, Alice, Muscheler, Raymond and Perez, M (2022) Wind regime changes in the Euro-Atlantic region driven by Late-Holocene Grand Solar Minima. Climate Dynamics, 60, 1947–1961. (doi:10.1007/s00382-022-06388-w).

Record type: Article

Abstract

Understanding atmospheric response to radiative forcing, including the intensity and distribution of wind patterns is critical as this might have important implications in the coming decades. Long-term episodes of reduced solar activity (i.e. Grand Solar Minima, GSM) have triggered rapid climate change in the past, recorded in proxy-based records, including varved sediments from Meerfelder Maar, Germany, where the Homeric GSM (~2800 years ago) was studied. This study reconstructs windy conditions during the same GSM from Diss Mere, another varved record in England, to support the solar-wind linkage in the North Atlantic-European region. We use diatoms as proxies for windiness and support the palaeolimnological and palaeoclimate interpretation with a multi-proxy chironomids and pollen) evidence. The diatom assemblage documents a shift from Pantocsekiella ocellata dominance to Stephanodiscus parvus and Lindavia comta, indicating a shift to more turbulent waters from ~2767 ± 28, linked to increased windiness. This shift is synchronous with changes in 14C production, linked to solar activity changes during the GSM. Both proxy records reflect a rapid and synchronous atmospheric response (i.e. stronger winds) at the onset and during the GSM in the North Atlantic and continental Europe. In order to test whether this solar-wind linkage is consistent during other GSMs and to understand the underlying climate dynamics, we analyse the wind response to solar forcing at the two study sites during the Little Ice Age, a period that includes several GSMs. For this, we have used a reconstruction based on a 1200-year-long simulation with an isotope-enabled climate model. Our study suggests that wind anomalies in the North Atlantic-European sector may relate to an anomalous atmospheric circulation in response to long-term solar forcing leading to north-easterlies modulated by the East Atlantic pattern.

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Harding et al. Accepted CLDY-D-21-00799 - Accepted Manuscript
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Accepted/In Press date: 13 June 2022
e-pub ahead of print date: 30 July 2022

Identifiers

Local EPrints ID: 467314
URI: http://eprints.soton.ac.uk/id/eprint/467314
ISSN: 0930-7575
PURE UUID: 02a9e8f0-6950-4216-a045-3bab624a4214
ORCID for Peter Langdon: ORCID iD orcid.org/0000-0003-2724-2643

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Date deposited: 05 Jul 2022 17:05
Last modified: 17 Mar 2024 07:22

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Contributors

Author: Poppy Harding
Author: Celia Martin Puertas
Author: J Sjolte
Author: Amy Walsh
Author: Rick Tjallingii
Author: Simon Blockley
Author: Achim Brauer
Author: Peter Langdon ORCID iD
Author: Alice Milner
Author: Raymond Muscheler
Author: M Perez

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