Pre-Signal and Influencing Sources of the Extreme Cold Surges at the Beijing 2022 Winter Olympic Competition Zones
The 24th Olympic and Paralympic Winter Games will take place in Beijing in 2022. All three competition zones are vulnerable to extreme cold surges (ECSs), owing to the occurrence of the East Asian winter monsoon. In this paper, a representative competition domain (37.5–42.5° N, 110–120° E) is adopte...
Published in: | Atmosphere |
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Main Authors: | , , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2020
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Subjects: | |
Online Access: | https://doi.org/10.3390/atmos11050436 |
_version_ | 1821667200839188480 |
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author | Ting Ding Hui Gao Yuan Yuan |
author_facet | Ting Ding Hui Gao Yuan Yuan |
author_sort | Ting Ding |
collection | MDPI Open Access Publishing |
container_issue | 5 |
container_start_page | 436 |
container_title | Atmosphere |
container_volume | 11 |
description | The 24th Olympic and Paralympic Winter Games will take place in Beijing in 2022. All three competition zones are vulnerable to extreme cold surges (ECSs), owing to the occurrence of the East Asian winter monsoon. In this paper, a representative competition domain (37.5–42.5° N, 110–120° E) is adopted, with a view to avoiding the differences in both the geographies and the thresholds of ECSs among different zones by considering the probability of simultaneous occurrences. Since 2009, the ECSs in the domain have displayed higher frequency and extremity. Based on all ECS cases in the domain, the dominant circulation is revealed by a quasi “reverse-Ω” pattern, with two strong ridges over the east of the Ural Mountain and the Okhotsk Sea, and a broad, deep trough in East Asia. The influencing sources of the ECSs at the domain could be traced to the Novaya Zemlya by a day-by-day backward analysis. The oblique latitude/longitude–time profiles of both the 500 hPa geopotential height and the 850 hPa air temperature anomalies from the source to the domain clearly indicate that the pre-signal could have a leading influence that exceeds ten days, with a slow accumulation in the first stage and a rapid outburst in the second stage. |
format | Text |
genre | Novaya Zemlya okhotsk sea |
genre_facet | Novaya Zemlya okhotsk sea |
geographic | Okhotsk |
geographic_facet | Okhotsk |
id | ftmdpi:oai:mdpi.com:/2073-4433/11/5/436/ |
institution | Open Polar |
language | English |
op_collection_id | ftmdpi |
op_coverage | agris |
op_doi | https://doi.org/10.3390/atmos11050436 |
op_relation | Meteorology https://dx.doi.org/10.3390/atmos11050436 |
op_rights | https://creativecommons.org/licenses/by/4.0/ |
op_source | Atmosphere; Volume 11; Issue 5; Pages: 436 |
publishDate | 2020 |
publisher | Multidisciplinary Digital Publishing Institute |
record_format | openpolar |
spelling | ftmdpi:oai:mdpi.com:/2073-4433/11/5/436/ 2025-01-16T23:59:07+00:00 Pre-Signal and Influencing Sources of the Extreme Cold Surges at the Beijing 2022 Winter Olympic Competition Zones Ting Ding Hui Gao Yuan Yuan agris 2020-04-26 application/pdf https://doi.org/10.3390/atmos11050436 EN eng Multidisciplinary Digital Publishing Institute Meteorology https://dx.doi.org/10.3390/atmos11050436 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 11; Issue 5; Pages: 436 extreme cold surge Olympic Games pre-signals Novaya Zemlya Text 2020 ftmdpi https://doi.org/10.3390/atmos11050436 2023-07-31T23:25:27Z The 24th Olympic and Paralympic Winter Games will take place in Beijing in 2022. All three competition zones are vulnerable to extreme cold surges (ECSs), owing to the occurrence of the East Asian winter monsoon. In this paper, a representative competition domain (37.5–42.5° N, 110–120° E) is adopted, with a view to avoiding the differences in both the geographies and the thresholds of ECSs among different zones by considering the probability of simultaneous occurrences. Since 2009, the ECSs in the domain have displayed higher frequency and extremity. Based on all ECS cases in the domain, the dominant circulation is revealed by a quasi “reverse-Ω” pattern, with two strong ridges over the east of the Ural Mountain and the Okhotsk Sea, and a broad, deep trough in East Asia. The influencing sources of the ECSs at the domain could be traced to the Novaya Zemlya by a day-by-day backward analysis. The oblique latitude/longitude–time profiles of both the 500 hPa geopotential height and the 850 hPa air temperature anomalies from the source to the domain clearly indicate that the pre-signal could have a leading influence that exceeds ten days, with a slow accumulation in the first stage and a rapid outburst in the second stage. Text Novaya Zemlya okhotsk sea MDPI Open Access Publishing Okhotsk Atmosphere 11 5 436 |
spellingShingle | extreme cold surge Olympic Games pre-signals Novaya Zemlya Ting Ding Hui Gao Yuan Yuan Pre-Signal and Influencing Sources of the Extreme Cold Surges at the Beijing 2022 Winter Olympic Competition Zones |
title | Pre-Signal and Influencing Sources of the Extreme Cold Surges at the Beijing 2022 Winter Olympic Competition Zones |
title_full | Pre-Signal and Influencing Sources of the Extreme Cold Surges at the Beijing 2022 Winter Olympic Competition Zones |
title_fullStr | Pre-Signal and Influencing Sources of the Extreme Cold Surges at the Beijing 2022 Winter Olympic Competition Zones |
title_full_unstemmed | Pre-Signal and Influencing Sources of the Extreme Cold Surges at the Beijing 2022 Winter Olympic Competition Zones |
title_short | Pre-Signal and Influencing Sources of the Extreme Cold Surges at the Beijing 2022 Winter Olympic Competition Zones |
title_sort | pre-signal and influencing sources of the extreme cold surges at the beijing 2022 winter olympic competition zones |
topic | extreme cold surge Olympic Games pre-signals Novaya Zemlya |
topic_facet | extreme cold surge Olympic Games pre-signals Novaya Zemlya |
url | https://doi.org/10.3390/atmos11050436 |