Surface and Tropospheric Response of North Atlantic Summer Climate from Paleoclimate Simulations of the Past Millennium ...

We investigate the effects of solar forcing on the North Atlantic (NA) summer climate, in climate simulations with Earth System Models (ESMs), over the preindustrial past millennium (AD 850–1849). We use one simulation and a four-member ensemble performed with the MPI-ESM-P and CESM-LME models, resp...

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Main Authors: Pyrina, Maria, Moreno-Chamarro, Eduardo, Wagner, Sebastian, Zorita, Eduardo
Format: Article in Journal/Newspaper
Language:English
Published: ETH Zurich 2021
Subjects:
Online Access:https://dx.doi.org/10.3929/ethz-b-000494820
http://hdl.handle.net/20.500.11850/494820
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author Pyrina, Maria
Moreno-Chamarro, Eduardo
Wagner, Sebastian
Zorita, Eduardo
author_facet Pyrina, Maria
Moreno-Chamarro, Eduardo
Wagner, Sebastian
Zorita, Eduardo
author_sort Pyrina, Maria
collection DataCite
description We investigate the effects of solar forcing on the North Atlantic (NA) summer climate, in climate simulations with Earth System Models (ESMs), over the preindustrial past millennium (AD 850–1849). We use one simulation and a four-member ensemble performed with the MPI-ESM-P and CESM-LME models, respectively, forced only by low-scaling variations in Total Solar Irradiance (TSI). We apply linear methods (correlation and regression) and composite analysis to estimate the NA surface and tropospheric climatic responses to decadal solar variability. Linear methods in the CESM ensemble indicate a weak summer response in sea-level pressure (SLP) and 500-hPa geopotential height to TSI, with decreased values over Greenland and increased values over the NA subtropics. Composite analysis indicates that, during high-TSI periods, SLP decreases over eastern Canada and the geopotential height at 500-hPa increases over the subtropical NA. The possible summer response of SSTs is overlapped by model internal variability. ... : Atmosphere, 12 (5) ...
format Article in Journal/Newspaper
genre Greenland
North Atlantic
genre_facet Greenland
North Atlantic
geographic Canada
Greenland
geographic_facet Canada
Greenland
id ftdatacite:10.3929/ethz-b-000494820
institution Open Polar
language English
op_collection_id ftdatacite
op_doi https://doi.org/10.3929/ethz-b-000494820
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
publishDate 2021
publisher ETH Zurich
record_format openpolar
spelling ftdatacite:10.3929/ethz-b-000494820 2025-04-20T14:37:59+00:00 Surface and Tropospheric Response of North Atlantic Summer Climate from Paleoclimate Simulations of the Past Millennium ... Pyrina, Maria Moreno-Chamarro, Eduardo Wagner, Sebastian Zorita, Eduardo 2021 application/pdf https://dx.doi.org/10.3929/ethz-b-000494820 http://hdl.handle.net/20.500.11850/494820 en eng ETH Zurich info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 TSI solar forcing last millennium paleoclimate simulations CESM-LME North Atlantic surface climatic response ScholarlyArticle Journal Article article-journal Text 2021 ftdatacite https://doi.org/10.3929/ethz-b-000494820 2025-04-02T13:07:23Z We investigate the effects of solar forcing on the North Atlantic (NA) summer climate, in climate simulations with Earth System Models (ESMs), over the preindustrial past millennium (AD 850–1849). We use one simulation and a four-member ensemble performed with the MPI-ESM-P and CESM-LME models, respectively, forced only by low-scaling variations in Total Solar Irradiance (TSI). We apply linear methods (correlation and regression) and composite analysis to estimate the NA surface and tropospheric climatic responses to decadal solar variability. Linear methods in the CESM ensemble indicate a weak summer response in sea-level pressure (SLP) and 500-hPa geopotential height to TSI, with decreased values over Greenland and increased values over the NA subtropics. Composite analysis indicates that, during high-TSI periods, SLP decreases over eastern Canada and the geopotential height at 500-hPa increases over the subtropical NA. The possible summer response of SSTs is overlapped by model internal variability. ... : Atmosphere, 12 (5) ... Article in Journal/Newspaper Greenland North Atlantic DataCite Canada Greenland
spellingShingle TSI
solar forcing
last millennium
paleoclimate simulations
CESM-LME
North Atlantic
surface climatic response
Pyrina, Maria
Moreno-Chamarro, Eduardo
Wagner, Sebastian
Zorita, Eduardo
Surface and Tropospheric Response of North Atlantic Summer Climate from Paleoclimate Simulations of the Past Millennium ...
title Surface and Tropospheric Response of North Atlantic Summer Climate from Paleoclimate Simulations of the Past Millennium ...
title_full Surface and Tropospheric Response of North Atlantic Summer Climate from Paleoclimate Simulations of the Past Millennium ...
title_fullStr Surface and Tropospheric Response of North Atlantic Summer Climate from Paleoclimate Simulations of the Past Millennium ...
title_full_unstemmed Surface and Tropospheric Response of North Atlantic Summer Climate from Paleoclimate Simulations of the Past Millennium ...
title_short Surface and Tropospheric Response of North Atlantic Summer Climate from Paleoclimate Simulations of the Past Millennium ...
title_sort surface and tropospheric response of north atlantic summer climate from paleoclimate simulations of the past millennium ...
topic TSI
solar forcing
last millennium
paleoclimate simulations
CESM-LME
North Atlantic
surface climatic response
topic_facet TSI
solar forcing
last millennium
paleoclimate simulations
CESM-LME
North Atlantic
surface climatic response
url https://dx.doi.org/10.3929/ethz-b-000494820
http://hdl.handle.net/20.500.11850/494820