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...

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Published in:Scientific Reports
Main Authors: Nicoli', Dario, Bellucci, Alessio, Iovino, Doroteaciro, Ruggieri, Paolo, Gualdi, Silvio
Other Authors: Fondazione Centro Euro-Mediterraneo Sui Cambiamenti Climatici (CMCC), Bologna, Italy, Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia
Format: Article in Journal/Newspaper
Language:English
Published: Nature P.G. 2020
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
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op_doi https://doi.org/10.1038/s41598-020-71464-2
op_relation Scientific Reports
/10 (2020)
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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