The Bølling–Allerød Interstadial
The Bølling–Allerød (B-A), the terrestrial counterpart of Dansgaard–Oeschger 1, is the first abrupt northern hemisphere climate warming episode of the last deglaciation. Several hypotheses have been proposed to explain this event: all involve the strengthening of the Atlantic Meridional Overturning...
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ftccsdartic:oai:HAL:hal-04309710v1 2023-12-31T10:07:28+01:00 The Bølling–Allerød Interstadial Naughton, Filipa Sánchez-Goñi, María F. Landais, Amaelle Rodrigues, Teresa Vazquez Riveiros, Natalia Toucanne, Samuel Geo-Ocean (GEO-OCEAN) Université de Bretagne Sud (UBS)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS) 2023 https://hal.science/hal-04309710 https://doi.org/10.1016/B978-0-323-91899-2.00015-2 en eng HAL CCSD info:eu-repo/semantics/altIdentifier/doi/10.1016/B978-0-323-91899-2.00015-2 hal-04309710 https://hal.science/hal-04309710 doi:10.1016/B978-0-323-91899-2.00015-2 European Glacial Landscapes. The Last Deglaciation. 2023. Palacios David, Garcia-Ruiz José m., Hughes Philip D., Andrés Nuria (Eds.). ISBN 978-0-323-91899-2, DOI 10.1016/C2021-0-00331-X. Part II Climate changes during the Last Deglaciation in the Eastern North Atlantic region, Chap.6, pp.45-50 https://hal.science/hal-04309710 European Glacial Landscapes. The Last Deglaciation. 2023. Palacios David, Garcia-Ruiz José m., Hughes Philip D., Andrés Nuria (Eds.). ISBN 978-0-323-91899-2, DOI 10.1016/C2021-0-00331-X. Part II Climate changes during the Last Deglaciation in the Eastern North Atlantic region, Chap.6, pp.45-50, 2023, ⟨10.1016/B978-0-323-91899-2.00015-2⟩ [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/bookPart Book sections 2023 ftccsdartic https://doi.org/10.1016/B978-0-323-91899-2.00015-210.1016/C2021-0-00331-X 2023-12-02T23:33:46Z The Bølling–Allerød (B-A), the terrestrial counterpart of Dansgaard–Oeschger 1, is the first abrupt northern hemisphere climate warming episode of the last deglaciation. Several hypotheses have been proposed to explain this event: all involve the strengthening of the Atlantic Meridional Overturning Circulation (AMOC) prior or during the Heinrich Stadial 1/B-A transition and the consequent warming of the northern hemisphere. Terrestrial proxies (mainly pollen and speleothems) reflect a progressive increase in moisture availability from the Bølling to the Allerød in Europe contrasting with Greenland isotope records which show maxima in temperature and precipitation at the onset of the Bølling and a gradual decrease to the end of the Allerød. Changes in moisture availability in Europe are triggered by coupled interactions between the AMOC and changes in atmospheric dynamics led by the westerlies. Book Part Greenland Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
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Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
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ftccsdartic |
language |
English |
topic |
[SDU]Sciences of the Universe [physics] |
spellingShingle |
[SDU]Sciences of the Universe [physics] Naughton, Filipa Sánchez-Goñi, María F. Landais, Amaelle Rodrigues, Teresa Vazquez Riveiros, Natalia Toucanne, Samuel The Bølling–Allerød Interstadial |
topic_facet |
[SDU]Sciences of the Universe [physics] |
description |
The Bølling–Allerød (B-A), the terrestrial counterpart of Dansgaard–Oeschger 1, is the first abrupt northern hemisphere climate warming episode of the last deglaciation. Several hypotheses have been proposed to explain this event: all involve the strengthening of the Atlantic Meridional Overturning Circulation (AMOC) prior or during the Heinrich Stadial 1/B-A transition and the consequent warming of the northern hemisphere. Terrestrial proxies (mainly pollen and speleothems) reflect a progressive increase in moisture availability from the Bølling to the Allerød in Europe contrasting with Greenland isotope records which show maxima in temperature and precipitation at the onset of the Bølling and a gradual decrease to the end of the Allerød. Changes in moisture availability in Europe are triggered by coupled interactions between the AMOC and changes in atmospheric dynamics led by the westerlies. |
author2 |
Geo-Ocean (GEO-OCEAN) Université de Bretagne Sud (UBS)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS) |
format |
Book Part |
author |
Naughton, Filipa Sánchez-Goñi, María F. Landais, Amaelle Rodrigues, Teresa Vazquez Riveiros, Natalia Toucanne, Samuel |
author_facet |
Naughton, Filipa Sánchez-Goñi, María F. Landais, Amaelle Rodrigues, Teresa Vazquez Riveiros, Natalia Toucanne, Samuel |
author_sort |
Naughton, Filipa |
title |
The Bølling–Allerød Interstadial |
title_short |
The Bølling–Allerød Interstadial |
title_full |
The Bølling–Allerød Interstadial |
title_fullStr |
The Bølling–Allerød Interstadial |
title_full_unstemmed |
The Bølling–Allerød Interstadial |
title_sort |
bølling–allerød interstadial |
publisher |
HAL CCSD |
publishDate |
2023 |
url |
https://hal.science/hal-04309710 https://doi.org/10.1016/B978-0-323-91899-2.00015-2 |
genre |
Greenland |
genre_facet |
Greenland |
op_source |
European Glacial Landscapes. The Last Deglaciation. 2023. Palacios David, Garcia-Ruiz José m., Hughes Philip D., Andrés Nuria (Eds.). ISBN 978-0-323-91899-2, DOI 10.1016/C2021-0-00331-X. Part II Climate changes during the Last Deglaciation in the Eastern North Atlantic region, Chap.6, pp.45-50 https://hal.science/hal-04309710 European Glacial Landscapes. The Last Deglaciation. 2023. Palacios David, Garcia-Ruiz José m., Hughes Philip D., Andrés Nuria (Eds.). ISBN 978-0-323-91899-2, DOI 10.1016/C2021-0-00331-X. Part II Climate changes during the Last Deglaciation in the Eastern North Atlantic region, Chap.6, pp.45-50, 2023, ⟨10.1016/B978-0-323-91899-2.00015-2⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/B978-0-323-91899-2.00015-2 hal-04309710 https://hal.science/hal-04309710 doi:10.1016/B978-0-323-91899-2.00015-2 |
op_doi |
https://doi.org/10.1016/B978-0-323-91899-2.00015-210.1016/C2021-0-00331-X |
_version_ |
1786839850967629824 |