Multi-decadal pacemaker simulations with an intermediate-complexity climate model

<p>In this paper, we first describe the main features of a new version of the International Centre for Theoretical Physics global atmospheric model (SPEEDY) with improved simulation of surface fluxes and the formulation of a three-layer thermodynamic ocean model (TOM3) suitable to explore the...

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Main Authors: F. Molteni, F. Kucharski, R. Farneti
Format: Article
Language:English
Published: Copernicus Publications 2024-02-01
Series:Weather and Climate Dynamics
Online Access:https://wcd.copernicus.org/articles/5/293/2024/wcd-5-293-2024.pdf
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author F. Molteni
F. Molteni
F. Kucharski
R. Farneti
author_facet F. Molteni
F. Molteni
F. Kucharski
R. Farneti
author_sort F. Molteni
collection DOAJ
description <p>In this paper, we first describe the main features of a new version of the International Centre for Theoretical Physics global atmospheric model (SPEEDY) with improved simulation of surface fluxes and the formulation of a three-layer thermodynamic ocean model (TOM3) suitable to explore the coupled extratropical response to tropical ocean variability. Then, we present results on the atmospheric model climatology, highlighting the impact of the modifications introduced in the model code, and show how important features of interdecadal and interannual variability are simulated in a “pacemaker” coupled ensemble of 70-year runs, where portions of the tropical Indo-Pacific are constrained to follow the observed variability.</p> <p>Despite the very basic representation of variations in greenhouse forcing and heat transport to the deep ocean (below the 300 m domain of the TOM3 model), the coupled ensemble reproduces the variations in surface temperature over land and sea with very good accuracy, confirming the role of the Indo-Pacific as a “pacemaker” for the natural fluctuations of global-mean surface temperatures found in earlier studies. Atmospheric zonal-mean temperature trends over 50 years are also realistically simulated in the extratropical lower troposphere and up to 100 hPa in the tropics.</p> <p>On the interannual scale, sea-surface temperature (SST) variability in sub-tropical and tropical regions not affected by SST relaxation is underestimated (mostly because of the absence of dynamically induced variability), while extratropical SST variability during the cold seasons is comparable to that observed. Atmospheric teleconnection patterns and their connections with SST are reproduced with high fidelity, although with local differences in the amplitude of regional features (such as a larger-than-observed response of extratropical SST to North Atlantic Oscillation variability). The SPEEDY-TOM3 model also reproduces the observed connection between averages of surface heat fluxes over the oceans and land surface air temperature in the wintertime northern extratropics.</p> <p>Overall, as in earlier versions of SPEEDY, the fidelity of the simulations (both in terms of climatological means and variability) is higher near the surface and in the lower troposphere, while the negative impacts of the coarse vertical resolution and simplified parameterizations are mostly felt in the stratosphere. However, the improved simulation of surface heat fluxes and their impact on extratropical SST variability in this model version (obtained at a very modest computational cost) make the SPEEDY-TOM3 model a suitable tool to investigate the coupled response of the extratropical circulation to interannual and inter-decadal changes of tropical SST in ensemble experiments.</p>
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spelling doaj.art-b1d4f4c8defb437798f41ce63d09dbbb2024-02-27T07:15:15ZengCopernicus PublicationsWeather and Climate Dynamics2698-40162024-02-01529332210.5194/wcd-5-293-2024Multi-decadal pacemaker simulations with an intermediate-complexity climate modelF. Molteni0F. Molteni1F. Kucharski2R. Farneti3Abdus Salam International Centre for Theoretical Physics, Trieste, ItalyEuropean Centre for Medium-Range Weather Forecasts, Reading, United KingdomAbdus Salam International Centre for Theoretical Physics, Trieste, ItalyAbdus Salam International Centre for Theoretical Physics, Trieste, Italy<p>In this paper, we first describe the main features of a new version of the International Centre for Theoretical Physics global atmospheric model (SPEEDY) with improved simulation of surface fluxes and the formulation of a three-layer thermodynamic ocean model (TOM3) suitable to explore the coupled extratropical response to tropical ocean variability. Then, we present results on the atmospheric model climatology, highlighting the impact of the modifications introduced in the model code, and show how important features of interdecadal and interannual variability are simulated in a “pacemaker” coupled ensemble of 70-year runs, where portions of the tropical Indo-Pacific are constrained to follow the observed variability.</p> <p>Despite the very basic representation of variations in greenhouse forcing and heat transport to the deep ocean (below the 300 m domain of the TOM3 model), the coupled ensemble reproduces the variations in surface temperature over land and sea with very good accuracy, confirming the role of the Indo-Pacific as a “pacemaker” for the natural fluctuations of global-mean surface temperatures found in earlier studies. Atmospheric zonal-mean temperature trends over 50 years are also realistically simulated in the extratropical lower troposphere and up to 100 hPa in the tropics.</p> <p>On the interannual scale, sea-surface temperature (SST) variability in sub-tropical and tropical regions not affected by SST relaxation is underestimated (mostly because of the absence of dynamically induced variability), while extratropical SST variability during the cold seasons is comparable to that observed. Atmospheric teleconnection patterns and their connections with SST are reproduced with high fidelity, although with local differences in the amplitude of regional features (such as a larger-than-observed response of extratropical SST to North Atlantic Oscillation variability). The SPEEDY-TOM3 model also reproduces the observed connection between averages of surface heat fluxes over the oceans and land surface air temperature in the wintertime northern extratropics.</p> <p>Overall, as in earlier versions of SPEEDY, the fidelity of the simulations (both in terms of climatological means and variability) is higher near the surface and in the lower troposphere, while the negative impacts of the coarse vertical resolution and simplified parameterizations are mostly felt in the stratosphere. However, the improved simulation of surface heat fluxes and their impact on extratropical SST variability in this model version (obtained at a very modest computational cost) make the SPEEDY-TOM3 model a suitable tool to investigate the coupled response of the extratropical circulation to interannual and inter-decadal changes of tropical SST in ensemble experiments.</p>https://wcd.copernicus.org/articles/5/293/2024/wcd-5-293-2024.pdf
spellingShingle F. Molteni
F. Molteni
F. Kucharski
R. Farneti
Multi-decadal pacemaker simulations with an intermediate-complexity climate model
Weather and Climate Dynamics
title Multi-decadal pacemaker simulations with an intermediate-complexity climate model
title_full Multi-decadal pacemaker simulations with an intermediate-complexity climate model
title_fullStr Multi-decadal pacemaker simulations with an intermediate-complexity climate model
title_full_unstemmed Multi-decadal pacemaker simulations with an intermediate-complexity climate model
title_short Multi-decadal pacemaker simulations with an intermediate-complexity climate model
title_sort multi decadal pacemaker simulations with an intermediate complexity climate model
url https://wcd.copernicus.org/articles/5/293/2024/wcd-5-293-2024.pdf
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