Mid-Latitude Jet Response to Pan-Arctic and Regional Arctic Warming in Idealized GCM
To study the dynamical mechanism by which Arctic amplification affects extreme weather events in mid-latitude, we investigated the local and remote circulation response to pan-Arctic and regional Arctic thermal forcing. A comprehensive atmospheric GCM (General Circulation Model) coupled to a slab mi...
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ftmdpi:oai:mdpi.com:/2073-4433/14/3/510/ 2023-08-20T04:03:22+02:00 Mid-Latitude Jet Response to Pan-Arctic and Regional Arctic Warming in Idealized GCM Gun-Hwan Yang Woosok Moon Hayeon Noh Baek-Min Kim agris 2023-03-06 application/pdf https://doi.org/10.3390/atmos14030510 EN eng Multidisciplinary Digital Publishing Institute Climatology https://dx.doi.org/10.3390/atmos14030510 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 14; Issue 3; Pages: 510 Arctic amplification atmospheric circulation jet climate change idealized model Text 2023 ftmdpi https://doi.org/10.3390/atmos14030510 2023-08-01T09:08:25Z To study the dynamical mechanism by which Arctic amplification affects extreme weather events in mid-latitude, we investigated the local and remote circulation response to pan-Arctic and regional Arctic thermal forcing. A comprehensive atmospheric GCM (General Circulation Model) coupled to a slab mixed-layer ocean model is used for the experiment. With the increasing thermal forcing in the pan-Arctic configuration, the mid-latitude jet tends to shift equatorward, mainly due to the southward shift of the convergence zone of eddy-heat flux and eddy-momentum flux. From the regional Arctic forced experiments, zonal mean response is similar to the response from the pan-Arctic configuration. The non-zonal response is characterized by the 300 hPa circumpolar zonal wind of wavenumber-1 structure, which establishes an enhanced wavier mid-latitude jet. In the polar region at 300 hPa, regional thermal forcing drives a distinct east–west dipole circulation pattern, in which anticyclonic circulation is located to the west of the thermal forcing, and cyclonic circulation is located to the east. The lower-level circulation shows the opposite pattern to the upper-level circulation in the polar region. While the strength of circulation increases with gradual thermal forcing, the overall dipole pattern is unchanged. In regional warming simulation, compared to the pan-Arctic warming, increasing residual heat flux in a dipole pattern causes enhanced heat advection to mid-latitude. Text Arctic Climate change MDPI Open Access Publishing Arctic Atmosphere 14 3 510 |
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Open Polar |
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MDPI Open Access Publishing |
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ftmdpi |
language |
English |
topic |
Arctic amplification atmospheric circulation jet climate change idealized model |
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Arctic amplification atmospheric circulation jet climate change idealized model Gun-Hwan Yang Woosok Moon Hayeon Noh Baek-Min Kim Mid-Latitude Jet Response to Pan-Arctic and Regional Arctic Warming in Idealized GCM |
topic_facet |
Arctic amplification atmospheric circulation jet climate change idealized model |
description |
To study the dynamical mechanism by which Arctic amplification affects extreme weather events in mid-latitude, we investigated the local and remote circulation response to pan-Arctic and regional Arctic thermal forcing. A comprehensive atmospheric GCM (General Circulation Model) coupled to a slab mixed-layer ocean model is used for the experiment. With the increasing thermal forcing in the pan-Arctic configuration, the mid-latitude jet tends to shift equatorward, mainly due to the southward shift of the convergence zone of eddy-heat flux and eddy-momentum flux. From the regional Arctic forced experiments, zonal mean response is similar to the response from the pan-Arctic configuration. The non-zonal response is characterized by the 300 hPa circumpolar zonal wind of wavenumber-1 structure, which establishes an enhanced wavier mid-latitude jet. In the polar region at 300 hPa, regional thermal forcing drives a distinct east–west dipole circulation pattern, in which anticyclonic circulation is located to the west of the thermal forcing, and cyclonic circulation is located to the east. The lower-level circulation shows the opposite pattern to the upper-level circulation in the polar region. While the strength of circulation increases with gradual thermal forcing, the overall dipole pattern is unchanged. In regional warming simulation, compared to the pan-Arctic warming, increasing residual heat flux in a dipole pattern causes enhanced heat advection to mid-latitude. |
format |
Text |
author |
Gun-Hwan Yang Woosok Moon Hayeon Noh Baek-Min Kim |
author_facet |
Gun-Hwan Yang Woosok Moon Hayeon Noh Baek-Min Kim |
author_sort |
Gun-Hwan Yang |
title |
Mid-Latitude Jet Response to Pan-Arctic and Regional Arctic Warming in Idealized GCM |
title_short |
Mid-Latitude Jet Response to Pan-Arctic and Regional Arctic Warming in Idealized GCM |
title_full |
Mid-Latitude Jet Response to Pan-Arctic and Regional Arctic Warming in Idealized GCM |
title_fullStr |
Mid-Latitude Jet Response to Pan-Arctic and Regional Arctic Warming in Idealized GCM |
title_full_unstemmed |
Mid-Latitude Jet Response to Pan-Arctic and Regional Arctic Warming in Idealized GCM |
title_sort |
mid-latitude jet response to pan-arctic and regional arctic warming in idealized gcm |
publisher |
Multidisciplinary Digital Publishing Institute |
publishDate |
2023 |
url |
https://doi.org/10.3390/atmos14030510 |
op_coverage |
agris |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Climate change |
genre_facet |
Arctic Climate change |
op_source |
Atmosphere; Volume 14; Issue 3; Pages: 510 |
op_relation |
Climatology https://dx.doi.org/10.3390/atmos14030510 |
op_rights |
https://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.3390/atmos14030510 |
container_title |
Atmosphere |
container_volume |
14 |
container_issue |
3 |
container_start_page |
510 |
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1774713742128316416 |