Possible Associations between the Number of Cold Days over East Asia and Arctic Oscillation and Arctic Warming

Based on the NECP/NCAR reanalysis dataset, the associations between the number of cold days (NCD) over East Asia (100–150° E, 25–55° N) and Arctic Oscillation (AO)/Arctic warming during 1956–2015 are explored. The results show the NCD was closely associated with AO during 1956–1990 and Arctic warmin...

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Published in:Atmosphere
Main Authors: Wei Song, Xiaochen Ye
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2021
Subjects:
Online Access:https://doi.org/10.3390/atmos12070842
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spelling ftmdpi:oai:mdpi.com:/2073-4433/12/7/842/ 2023-08-20T04:03:25+02:00 Possible Associations between the Number of Cold Days over East Asia and Arctic Oscillation and Arctic Warming Wei Song Xiaochen Ye agris 2021-06-29 application/pdf https://doi.org/10.3390/atmos12070842 EN eng Multidisciplinary Digital Publishing Institute Meteorology https://dx.doi.org/10.3390/atmos12070842 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 12; Issue 7; Pages: 842 number of cold days East Asia Arctic Oscillation Arctic warming Text 2021 ftmdpi https://doi.org/10.3390/atmos12070842 2023-08-01T02:04:18Z Based on the NECP/NCAR reanalysis dataset, the associations between the number of cold days (NCD) over East Asia (100–150° E, 25–55° N) and Arctic Oscillation (AO)/Arctic warming during 1956–2015 are explored. The results show the NCD was closely associated with AO during 1956–1990 and Arctic warming during 1991–2015. It reveals NCD over East Asia showed a downward trend and a significantly negative correlation with AO in the previous stage, while it presented an upward trend and notably positive association with Arctic warming in the later period. Meanwhile the increase in the earlier-stage AO will often be accompanied by the weakness of the Siberian high (SH), the Ural Mountains Blocking high (UBH), and the East Asian trough (EAT), and a “positive–negative–positive” wave band exist in the upper troposphere, which is linked with weakened northerly wind over East Asia. All these anomalies are unfavorable for the southward transportation of cold air, eventually leading to the decrease in NCD over East Asia. Additionally, when the near-surface temperature over the Arctic rises in the later period, on the one hand, SH reinforces and further results in more NCD over East Asia; on the other hand, the 1000–500 hPa thickness field displays a “north positive–south negative” pattern, which is conducive to the deceleration of the westerlies at mid-latitudes over Eurasia, and further bring about the enhancement of EAT and UBH, favoring the southward intrusion of cold air, finally, more NCD are generated. Text Arctic MDPI Open Access Publishing Arctic Atmosphere 12 7 842
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic number of cold days
East Asia
Arctic Oscillation
Arctic warming
spellingShingle number of cold days
East Asia
Arctic Oscillation
Arctic warming
Wei Song
Xiaochen Ye
Possible Associations between the Number of Cold Days over East Asia and Arctic Oscillation and Arctic Warming
topic_facet number of cold days
East Asia
Arctic Oscillation
Arctic warming
description Based on the NECP/NCAR reanalysis dataset, the associations between the number of cold days (NCD) over East Asia (100–150° E, 25–55° N) and Arctic Oscillation (AO)/Arctic warming during 1956–2015 are explored. The results show the NCD was closely associated with AO during 1956–1990 and Arctic warming during 1991–2015. It reveals NCD over East Asia showed a downward trend and a significantly negative correlation with AO in the previous stage, while it presented an upward trend and notably positive association with Arctic warming in the later period. Meanwhile the increase in the earlier-stage AO will often be accompanied by the weakness of the Siberian high (SH), the Ural Mountains Blocking high (UBH), and the East Asian trough (EAT), and a “positive–negative–positive” wave band exist in the upper troposphere, which is linked with weakened northerly wind over East Asia. All these anomalies are unfavorable for the southward transportation of cold air, eventually leading to the decrease in NCD over East Asia. Additionally, when the near-surface temperature over the Arctic rises in the later period, on the one hand, SH reinforces and further results in more NCD over East Asia; on the other hand, the 1000–500 hPa thickness field displays a “north positive–south negative” pattern, which is conducive to the deceleration of the westerlies at mid-latitudes over Eurasia, and further bring about the enhancement of EAT and UBH, favoring the southward intrusion of cold air, finally, more NCD are generated.
format Text
author Wei Song
Xiaochen Ye
author_facet Wei Song
Xiaochen Ye
author_sort Wei Song
title Possible Associations between the Number of Cold Days over East Asia and Arctic Oscillation and Arctic Warming
title_short Possible Associations between the Number of Cold Days over East Asia and Arctic Oscillation and Arctic Warming
title_full Possible Associations between the Number of Cold Days over East Asia and Arctic Oscillation and Arctic Warming
title_fullStr Possible Associations between the Number of Cold Days over East Asia and Arctic Oscillation and Arctic Warming
title_full_unstemmed Possible Associations between the Number of Cold Days over East Asia and Arctic Oscillation and Arctic Warming
title_sort possible associations between the number of cold days over east asia and arctic oscillation and arctic warming
publisher Multidisciplinary Digital Publishing Institute
publishDate 2021
url https://doi.org/10.3390/atmos12070842
op_coverage agris
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source Atmosphere; Volume 12; Issue 7; Pages: 842
op_relation Meteorology
https://dx.doi.org/10.3390/atmos12070842
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos12070842
container_title Atmosphere
container_volume 12
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