Impact of the Scandinavian Pattern on Long-Lived Cold Surges over the South China Sea
This study investigates the influence of the Scandinavian (SCA) pattern on long-lived cold surges over the South China Sea (SCS). The results show that, different from the short-lived ones, the majority of long-lived cold surges over the SCS are preceded by a negative phase of the quasi-stationary S...
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Veröffentlicht in: | Journal of climate 2022-03, Vol.35 (6), p.1773-1785 |
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description | This study investigates the influence of the Scandinavian (SCA) pattern on long-lived cold surges over the South China Sea (SCS). The results show that, different from the short-lived ones, the majority of long-lived cold surges over the SCS are preceded by a negative phase of the quasi-stationary SCA pattern in the extratropics, which is characterized as a primary cyclonic center over the Scandinavian Peninsula and two anticyclonic ones over the North Atlantic and central Siberia. This connection is mainly conducted through a continuous amplification of the high pressure anomalies over East Asia. On the other hand, the SCA-related anomalies also reveal identical responses as an increase in sea level pressure over East Asia and northerly flows over the SCS. Besides, the SCA pattern may influence the long-lived cold surges over the SCS by facilitating blocking occurrences through the extensive and quasi-stationary anticyclone over central Siberia. The present results have an implication for the extended weather forecast: long-lasting circulation anomalies, such as the SCA pattern, can affect long-lasting weather phenomena in the regions that are located remotely in both the zonal and meridional directions, such as long-lived cold surges over the SCS. |
doi_str_mv | 10.1175/JCLI-D-21-0607.1 |
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The results show that, different from the short-lived ones, the majority of long-lived cold surges over the SCS are preceded by a negative phase of the quasi-stationary SCA pattern in the extratropics, which is characterized as a primary cyclonic center over the Scandinavian Peninsula and two anticyclonic ones over the North Atlantic and central Siberia. This connection is mainly conducted through a continuous amplification of the high pressure anomalies over East Asia. On the other hand, the SCA-related anomalies also reveal identical responses as an increase in sea level pressure over East Asia and northerly flows over the SCS. Besides, the SCA pattern may influence the long-lived cold surges over the SCS by facilitating blocking occurrences through the extensive and quasi-stationary anticyclone over central Siberia. The present results have an implication for the extended weather forecast: long-lasting circulation anomalies, such as the SCA pattern, can affect long-lasting weather phenomena in the regions that are located remotely in both the zonal and meridional directions, such as long-lived cold surges over the SCS.</description><identifier>ISSN: 0894-8755</identifier><identifier>EISSN: 1520-0442</identifier><identifier>DOI: 10.1175/JCLI-D-21-0607.1</identifier><language>eng</language><publisher>Boston: American Meteorological Society</publisher><subject>Anomalies ; Anticyclones ; Brittleness ; Circulation anomalies ; Cold ; Cold surges ; High pressure ; Pressure anomalies ; Sea level ; Sea level pressure ; Surges ; Weather forecasting</subject><ispartof>Journal of climate, 2022-03, Vol.35 (6), p.1773-1785</ispartof><rights>2022 American Meteorological Society</rights><rights>Copyright American Meteorological Society Mar 2022</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c208t-8401fdadbdf29d059cfebfbdbeaead10f720d68ee01ebfd40beab3a80dfb1e583</citedby><cites>FETCH-LOGICAL-c208t-8401fdadbdf29d059cfebfbdbeaead10f720d68ee01ebfd40beab3a80dfb1e583</cites><orcidid>0000-0003-3502-9797</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,3667,27903,27904</link.rule.ids></links><search><creatorcontrib>Pang, Bo</creatorcontrib><creatorcontrib>Lu, Riyu</creatorcontrib><creatorcontrib>Ren, Rongcai</creatorcontrib><title>Impact of the Scandinavian Pattern on Long-Lived Cold Surges over the South China Sea</title><title>Journal of climate</title><description>This study investigates the influence of the Scandinavian (SCA) pattern on long-lived cold surges over the South China Sea (SCS). The results show that, different from the short-lived ones, the majority of long-lived cold surges over the SCS are preceded by a negative phase of the quasi-stationary SCA pattern in the extratropics, which is characterized as a primary cyclonic center over the Scandinavian Peninsula and two anticyclonic ones over the North Atlantic and central Siberia. This connection is mainly conducted through a continuous amplification of the high pressure anomalies over East Asia. On the other hand, the SCA-related anomalies also reveal identical responses as an increase in sea level pressure over East Asia and northerly flows over the SCS. Besides, the SCA pattern may influence the long-lived cold surges over the SCS by facilitating blocking occurrences through the extensive and quasi-stationary anticyclone over central Siberia. The present results have an implication for the extended weather forecast: long-lasting circulation anomalies, such as the SCA pattern, can affect long-lasting weather phenomena in the regions that are located remotely in both the zonal and meridional directions, such as long-lived cold surges over the SCS.</description><subject>Anomalies</subject><subject>Anticyclones</subject><subject>Brittleness</subject><subject>Circulation anomalies</subject><subject>Cold</subject><subject>Cold surges</subject><subject>High pressure</subject><subject>Pressure anomalies</subject><subject>Sea level</subject><subject>Sea level pressure</subject><subject>Surges</subject><subject>Weather forecasting</subject><issn>0894-8755</issn><issn>1520-0442</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2022</creationdate><recordtype>article</recordtype><recordid>eNo9kF1LwzAUhoMoOKf33ggBrzNPsqZJL6V-TQoKc9chbZKtY2tmkg7893ZUvDrwnuc5B16EbinMKBX84b2sFuSJMEogBzGjZ2hCOQMCWcbO0QRkkREpOL9EVzFuASjLASZotdgfdJOwdzhtLF42ujNtp4-t7vCnTsmGDvsOV75bk6o9WoNLvzN42Ye1jdgfbRg936cNLjeDipdWX6MLp3fR3vzNKVq9PH-Vb6T6eF2UjxVpGMhEZAbUGW1q41hhgBeNs7WrTW211YaCEwxMLq0FOuQmg2FRz7UE42pquZxP0f149xD8d29jUlvfh254qVgueF4IAXygYKSa4GMM1qlDaPc6_CgK6lSeOpWnnhSj6lSeooNyNyrbmHz455lgWUY5n_8C1eNtFA</recordid><startdate>20220315</startdate><enddate>20220315</enddate><creator>Pang, Bo</creator><creator>Lu, Riyu</creator><creator>Ren, Rongcai</creator><general>American Meteorological Society</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7TG</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0003-3502-9797</orcidid></search><sort><creationdate>20220315</creationdate><title>Impact of the Scandinavian Pattern on Long-Lived Cold Surges over the South China Sea</title><author>Pang, Bo ; Lu, Riyu ; Ren, Rongcai</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c208t-8401fdadbdf29d059cfebfbdbeaead10f720d68ee01ebfd40beab3a80dfb1e583</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2022</creationdate><topic>Anomalies</topic><topic>Anticyclones</topic><topic>Brittleness</topic><topic>Circulation anomalies</topic><topic>Cold</topic><topic>Cold surges</topic><topic>High pressure</topic><topic>Pressure anomalies</topic><topic>Sea level</topic><topic>Sea level pressure</topic><topic>Surges</topic><topic>Weather forecasting</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Pang, Bo</creatorcontrib><creatorcontrib>Lu, Riyu</creatorcontrib><creatorcontrib>Ren, Rongcai</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Journal of climate</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Pang, Bo</au><au>Lu, Riyu</au><au>Ren, Rongcai</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Impact of the Scandinavian Pattern on Long-Lived Cold Surges over the South China Sea</atitle><jtitle>Journal of climate</jtitle><date>2022-03-15</date><risdate>2022</risdate><volume>35</volume><issue>6</issue><spage>1773</spage><epage>1785</epage><pages>1773-1785</pages><issn>0894-8755</issn><eissn>1520-0442</eissn><abstract>This study investigates the influence of the Scandinavian (SCA) pattern on long-lived cold surges over the South China Sea (SCS). The results show that, different from the short-lived ones, the majority of long-lived cold surges over the SCS are preceded by a negative phase of the quasi-stationary SCA pattern in the extratropics, which is characterized as a primary cyclonic center over the Scandinavian Peninsula and two anticyclonic ones over the North Atlantic and central Siberia. This connection is mainly conducted through a continuous amplification of the high pressure anomalies over East Asia. On the other hand, the SCA-related anomalies also reveal identical responses as an increase in sea level pressure over East Asia and northerly flows over the SCS. Besides, the SCA pattern may influence the long-lived cold surges over the SCS by facilitating blocking occurrences through the extensive and quasi-stationary anticyclone over central Siberia. The present results have an implication for the extended weather forecast: long-lasting circulation anomalies, such as the SCA pattern, can affect long-lasting weather phenomena in the regions that are located remotely in both the zonal and meridional directions, such as long-lived cold surges over the SCS.</abstract><cop>Boston</cop><pub>American Meteorological Society</pub><doi>10.1175/JCLI-D-21-0607.1</doi><tpages>13</tpages><orcidid>https://orcid.org/0000-0003-3502-9797</orcidid></addata></record> |
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source | American Meteorological Society; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals |
subjects | Anomalies Anticyclones Brittleness Circulation anomalies Cold Cold surges High pressure Pressure anomalies Sea level Sea level pressure Surges Weather forecasting |
title | Impact of the Scandinavian Pattern on Long-Lived Cold Surges over the South China Sea |
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