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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ETH Zurich
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Online Access: | https://dx.doi.org/10.3929/ethz-b-000494820 http://hdl.handle.net/20.500.11850/494820 |
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ftdatacite:10.3929/ethz-b-000494820 2024-04-28T08:21:52+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 article-journal Text ScholarlyArticle Journal Article 2021 ftdatacite https://doi.org/10.3929/ethz-b-000494820 2024-04-02T12:34:54Z 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 Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
TSI solar forcing last millennium paleoclimate simulations CESM-LME North Atlantic surface climatic response |
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 ... |
topic_facet |
TSI solar forcing last millennium paleoclimate simulations CESM-LME North Atlantic surface climatic response |
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 |
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 |
title |
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_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_sort |
surface and tropospheric response of north atlantic summer climate from paleoclimate simulations of the past millennium ... |
publisher |
ETH Zurich |
publishDate |
2021 |
url |
https://dx.doi.org/10.3929/ethz-b-000494820 http://hdl.handle.net/20.500.11850/494820 |
genre |
Greenland North Atlantic |
genre_facet |
Greenland North Atlantic |
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 |
op_doi |
https://doi.org/10.3929/ethz-b-000494820 |
_version_ |
1797583922765234176 |