Horizontal Temperature Fluxes in the Arctic in CMIP5 Model Results Analyzed with Self-Organizing Maps

The meridional temperature gradient between mid and high latitudes decreases by Arctic amplification. Following this decrease, the circulation in the mid latitudes may change and, therefore, the meridional flux of heat and moisture increases. This might increase the Arctic temperatures even further....

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Published in:Atmosphere
Main Authors: Daniel Mewes, Christoph Jacobi
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2020
Subjects:
Online Access:https://doi.org/10.3390/atmos11030251
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spelling ftmdpi:oai:mdpi.com:/2073-4433/11/3/251/ 2023-08-20T04:04:01+02:00 Horizontal Temperature Fluxes in the Arctic in CMIP5 Model Results Analyzed with Self-Organizing Maps Daniel Mewes Christoph Jacobi agris 2020-03-02 application/pdf https://doi.org/10.3390/atmos11030251 EN eng Multidisciplinary Digital Publishing Institute Climatology https://dx.doi.org/10.3390/atmos11030251 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 11; Issue 3; Pages: 251 self-organizing maps CMIP5 horizontal heat flux Text 2020 ftmdpi https://doi.org/10.3390/atmos11030251 2023-07-31T23:11:07Z The meridional temperature gradient between mid and high latitudes decreases by Arctic amplification. Following this decrease, the circulation in the mid latitudes may change and, therefore, the meridional flux of heat and moisture increases. This might increase the Arctic temperatures even further. A proxy for the vertically integrated atmospheric horizontal energy flux was analyzed using the self-organizing-map (SOM) method. Climate Model Intercomparison Project Phase 5 (CMIP5) model data of the historical and Representative Concentration Pathway 8.5 (RCP8.5) experiments were analyzed to extract horizontal flux patterns. These patterns were analyzed for changes between and within the respective experiments. It was found that the general horizontal flux patterns are reproduced by all models and in all experiments in comparison with reanalyses. By comparing the reanalysis time frame with the respective historical experiments, we found that the general occurrence frequencies of the patterns differ substantially. The results show that the general structure of the flux patterns is not changed when comparing the historical and RCP8.5 results. However, the amplitudes of the fluxes are decreasing. It is suggested that the amplitudes are smaller in the RCP8.5 results compared to the historical results, following a greater meandering of the jet stream, which yields smaller flux amplitudes of the cluster mean. Text Arctic MDPI Open Access Publishing Arctic Atmosphere 11 3 251
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic self-organizing maps
CMIP5
horizontal heat flux
spellingShingle self-organizing maps
CMIP5
horizontal heat flux
Daniel Mewes
Christoph Jacobi
Horizontal Temperature Fluxes in the Arctic in CMIP5 Model Results Analyzed with Self-Organizing Maps
topic_facet self-organizing maps
CMIP5
horizontal heat flux
description The meridional temperature gradient between mid and high latitudes decreases by Arctic amplification. Following this decrease, the circulation in the mid latitudes may change and, therefore, the meridional flux of heat and moisture increases. This might increase the Arctic temperatures even further. A proxy for the vertically integrated atmospheric horizontal energy flux was analyzed using the self-organizing-map (SOM) method. Climate Model Intercomparison Project Phase 5 (CMIP5) model data of the historical and Representative Concentration Pathway 8.5 (RCP8.5) experiments were analyzed to extract horizontal flux patterns. These patterns were analyzed for changes between and within the respective experiments. It was found that the general horizontal flux patterns are reproduced by all models and in all experiments in comparison with reanalyses. By comparing the reanalysis time frame with the respective historical experiments, we found that the general occurrence frequencies of the patterns differ substantially. The results show that the general structure of the flux patterns is not changed when comparing the historical and RCP8.5 results. However, the amplitudes of the fluxes are decreasing. It is suggested that the amplitudes are smaller in the RCP8.5 results compared to the historical results, following a greater meandering of the jet stream, which yields smaller flux amplitudes of the cluster mean.
format Text
author Daniel Mewes
Christoph Jacobi
author_facet Daniel Mewes
Christoph Jacobi
author_sort Daniel Mewes
title Horizontal Temperature Fluxes in the Arctic in CMIP5 Model Results Analyzed with Self-Organizing Maps
title_short Horizontal Temperature Fluxes in the Arctic in CMIP5 Model Results Analyzed with Self-Organizing Maps
title_full Horizontal Temperature Fluxes in the Arctic in CMIP5 Model Results Analyzed with Self-Organizing Maps
title_fullStr Horizontal Temperature Fluxes in the Arctic in CMIP5 Model Results Analyzed with Self-Organizing Maps
title_full_unstemmed Horizontal Temperature Fluxes in the Arctic in CMIP5 Model Results Analyzed with Self-Organizing Maps
title_sort horizontal temperature fluxes in the arctic in cmip5 model results analyzed with self-organizing maps
publisher Multidisciplinary Digital Publishing Institute
publishDate 2020
url https://doi.org/10.3390/atmos11030251
op_coverage agris
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Atmosphere; Volume 11; Issue 3; Pages: 251
op_relation Climatology
https://dx.doi.org/10.3390/atmos11030251
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos11030251
container_title Atmosphere
container_volume 11
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container_start_page 251
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