The impact of the AMV on Eurasian summer hydrological cycle
Impact studies of the Atlantic Multidecadal Variability (AMV) on the climate system are severely limited by the lack of sufficiently long observational records. Relying on a model-based approach is therefore mandatory to overcome this limitation. Here, a novel experimental setup, designed in the fra...
Published in: | Scientific Reports |
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Main Authors: | , , , , |
Other Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Nature P.G.
2020
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Subjects: | |
Online Access: | https://www.earth-prints.org/handle/2122/14446 https://doi.org/10.1038/s41598-020-71464-2 |
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author | Nicoli', Dario Bellucci, Alessio Iovino, Doroteaciro Ruggieri, Paolo Gualdi, Silvio |
author2 | Fondazione Centro Euro-Mediterraneo Sui Cambiamenti Climatici (CMCC), Bologna, Italy Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia |
author_facet | Nicoli', Dario Bellucci, Alessio Iovino, Doroteaciro Ruggieri, Paolo Gualdi, Silvio |
author_sort | Nicoli', Dario |
collection | Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) |
container_issue | 1 |
container_title | Scientific Reports |
container_volume | 10 |
description | Impact studies of the Atlantic Multidecadal Variability (AMV) on the climate system are severely limited by the lack of sufficiently long observational records. Relying on a model-based approach is therefore mandatory to overcome this limitation. Here, a novel experimental setup, designed in the framework of the CMIP6-endorsed Decadal Climate Prediction Project, is applied to the CMCC climate model to analyse the remote climate impact of the AMV on the Northern Eurasian continent. Model results show that, during Boreal summer, an enhanced warming associated to a positive phase of the AMV, induces a hemispheric-scale wave-train response in the atmospheric circulation, affecting vast portions of Northern Eurasia. The overall AMV-induced response consists in an upper-tropospheric anomalous flows leading to a rainfall increase over Scandinavia and Siberia and to an intensified river runoff by the major Siberian rivers. A strengthening of Eurasian shelves' stratification, broadly consistent with the anomalous river discharge, is found in the proximity of the river mouths during positive-AMV years. Considering that Siberian rivers (Ob', Yenisei and Lena) account for almost half of the Arctic freshwater input provided by terrestrial sources, the implications of these findings for decadal variability and predictability of the Arctic environment are also discussed. Published 14444 4A. Oceanografia e clima JCR Journal |
format | Article in Journal/Newspaper |
genre | Arctic Siberia |
genre_facet | Arctic Siberia |
geographic | Arctic |
geographic_facet | Arctic |
id | ftingv:oai:earth-prints.org:2122/14446 |
institution | Open Polar |
language | English |
op_collection_id | ftingv |
op_doi | https://doi.org/10.1038/s41598-020-71464-2 |
op_relation | Scientific Reports /10 (2020) |
op_rights | Attribution-NoDerivs 3.0 United States http://creativecommons.org/licenses/by-nd/3.0/us/ |
publishDate | 2020 |
publisher | Nature P.G. |
record_format | openpolar |
spelling | ftingv:oai:earth-prints.org:2122/14446 2025-01-16T20:29:05+00:00 The impact of the AMV on Eurasian summer hydrological cycle Nicoli', Dario Bellucci, Alessio Iovino, Doroteaciro Ruggieri, Paolo Gualdi, Silvio Fondazione Centro Euro-Mediterraneo Sui Cambiamenti Climatici (CMCC), Bologna, Italy Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia 2020 application/pdf https://www.earth-prints.org/handle/2122/14446 https://doi.org/10.1038/s41598-020-71464-2 English eng Nature P.G. Scientific Reports /10 (2020) Attribution-NoDerivs 3.0 United States http://creativecommons.org/licenses/by-nd/3.0/us/ article Peer-reviewed 2020 ftingv https://doi.org/10.1038/s41598-020-71464-2 2024-12-18T15:48:59Z Impact studies of the Atlantic Multidecadal Variability (AMV) on the climate system are severely limited by the lack of sufficiently long observational records. Relying on a model-based approach is therefore mandatory to overcome this limitation. Here, a novel experimental setup, designed in the framework of the CMIP6-endorsed Decadal Climate Prediction Project, is applied to the CMCC climate model to analyse the remote climate impact of the AMV on the Northern Eurasian continent. Model results show that, during Boreal summer, an enhanced warming associated to a positive phase of the AMV, induces a hemispheric-scale wave-train response in the atmospheric circulation, affecting vast portions of Northern Eurasia. The overall AMV-induced response consists in an upper-tropospheric anomalous flows leading to a rainfall increase over Scandinavia and Siberia and to an intensified river runoff by the major Siberian rivers. A strengthening of Eurasian shelves' stratification, broadly consistent with the anomalous river discharge, is found in the proximity of the river mouths during positive-AMV years. Considering that Siberian rivers (Ob', Yenisei and Lena) account for almost half of the Arctic freshwater input provided by terrestrial sources, the implications of these findings for decadal variability and predictability of the Arctic environment are also discussed. Published 14444 4A. Oceanografia e clima JCR Journal Article in Journal/Newspaper Arctic Siberia Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Arctic Scientific Reports 10 1 |
spellingShingle | Nicoli', Dario Bellucci, Alessio Iovino, Doroteaciro Ruggieri, Paolo Gualdi, Silvio The impact of the AMV on Eurasian summer hydrological cycle |
title | The impact of the AMV on Eurasian summer hydrological cycle |
title_full | The impact of the AMV on Eurasian summer hydrological cycle |
title_fullStr | The impact of the AMV on Eurasian summer hydrological cycle |
title_full_unstemmed | The impact of the AMV on Eurasian summer hydrological cycle |
title_short | The impact of the AMV on Eurasian summer hydrological cycle |
title_sort | impact of the amv on eurasian summer hydrological cycle |
url | https://www.earth-prints.org/handle/2122/14446 https://doi.org/10.1038/s41598-020-71464-2 |