Interannual and interdecadal variability of the summertime western North Pacific subtropical high
The western North Pacific Subtropical High (WNPSH) in summer exhibits significant 2–3 years and 3–5 years oscillations with interdecadal variability. The 2–3‐year oscillation is most evident after 1990. It is accompanied by anomalous meridional overturning circulation characterized by warm SST anoma...
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| Veröffentlicht in: | Geophysical research letters 2007-06, Vol.34 (11), p.n/a |
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| creator | Sui, Chung-Hsiung Chung, Pei-Hsuan Li, Tim |
| description | The western North Pacific Subtropical High (WNPSH) in summer exhibits significant 2–3 years and 3–5 years oscillations with interdecadal variability. The 2–3‐year oscillation is most evident after 1990. It is accompanied by anomalous meridional overturning circulation characterized by warm SST anomalies (SSTA) and ascending motion in the maritime continent and anomalous descending motion near the Philippine Sea, and by evolving warm to cold SSTA in the central‐eastern Pacific from the preceding winter to the summer. The 3–5‐year oscillation is most pronounced during the 1980s. It is accompanied by anomalous descending motion over the maritime continent and warm SSTA in the central‐eastern equatorial Pacific that persists from the preceding winter to the summer; the complementary cooling and descending motion in the western Pacific are related to anomalous east‐west circulation associated with ENSO. |
| doi_str_mv | 10.1029/2006GL029204 |
| format | Article |
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The 2–3‐year oscillation is most evident after 1990. It is accompanied by anomalous meridional overturning circulation characterized by warm SST anomalies (SSTA) and ascending motion in the maritime continent and anomalous descending motion near the Philippine Sea, and by evolving warm to cold SSTA in the central‐eastern Pacific from the preceding winter to the summer. The 3–5‐year oscillation is most pronounced during the 1980s. 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Res. Lett</addtitle><description>The western North Pacific Subtropical High (WNPSH) in summer exhibits significant 2–3 years and 3–5 years oscillations with interdecadal variability. The 2–3‐year oscillation is most evident after 1990. It is accompanied by anomalous meridional overturning circulation characterized by warm SST anomalies (SSTA) and ascending motion in the maritime continent and anomalous descending motion near the Philippine Sea, and by evolving warm to cold SSTA in the central‐eastern Pacific from the preceding winter to the summer. The 3–5‐year oscillation is most pronounced during the 1980s. It is accompanied by anomalous descending motion over the maritime continent and warm SSTA in the central‐eastern equatorial Pacific that persists from the preceding winter to the summer; the complementary cooling and descending motion in the western Pacific are related to anomalous east‐west circulation associated with ENSO.</description><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>interannual variability</subject><subject>interdecadal variability</subject><subject>WNP subtropical high</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2007</creationdate><recordtype>article</recordtype><recordid>eNp9kMtOwzAQRS0EEuWx4wOygRWB8SNxskQFClIFCIrozpo4DjXkUeyU0r_HqAhYsfLYOudqfAk5oHBCgeWnDCAdjcPEQGyQAc2FiDMAuUkGAHmYmUy3yY73LwDAgdMBweu2Nw7bdoF1hG0Z2a97aTSW4eEdncXC1rZfRV0V9TMT-UXTGNfbxkRL4wPbRjed62fRHWpbWR2Aonfd3Orgz-zzbI9sVVh7s_997pLHy4vJ8Coe346uh2fjWCdMQCy4loVMIIXKGJC84ChYjkakogCeSlYlFcsLBFkkOdWGSZPRpKSgAbAoJd8lR-vcueveFmE11VivTV1ja7qFV4yGdjJIA3i8BrXrvHemUnNnG3QrRUF99aj-9hjww-9c9OFPVShLW__rZDlNhaCBY2tuaWuz-jdTje7HjGUZBCleSzZU-fEjoXtVqeQyUU83IwV0ej58yKZqwj8BUU6QkA</recordid><startdate>200706</startdate><enddate>200706</enddate><creator>Sui, Chung-Hsiung</creator><creator>Chung, Pei-Hsuan</creator><creator>Li, Tim</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>200706</creationdate><title>Interannual and interdecadal variability of the summertime western North Pacific subtropical high</title><author>Sui, Chung-Hsiung ; Chung, Pei-Hsuan ; Li, Tim</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c5240-43c7b75060fee073b3a429ae464b03672f5f29ba07b591ce27e815d10c00abd73</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2007</creationdate><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>interannual variability</topic><topic>interdecadal variability</topic><topic>WNP subtropical high</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Sui, Chung-Hsiung</creatorcontrib><creatorcontrib>Chung, Pei-Hsuan</creatorcontrib><creatorcontrib>Li, Tim</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</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>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Sui, Chung-Hsiung</au><au>Chung, Pei-Hsuan</au><au>Li, Tim</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Interannual and interdecadal variability of the summertime western North Pacific subtropical high</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>2007-06</date><risdate>2007</risdate><volume>34</volume><issue>11</issue><epage>n/a</epage><issn>0094-8276</issn><eissn>1944-8007</eissn><coden>GPRLAJ</coden><abstract>The western North Pacific Subtropical High (WNPSH) in summer exhibits significant 2–3 years and 3–5 years oscillations with interdecadal variability. The 2–3‐year oscillation is most evident after 1990. It is accompanied by anomalous meridional overturning circulation characterized by warm SST anomalies (SSTA) and ascending motion in the maritime continent and anomalous descending motion near the Philippine Sea, and by evolving warm to cold SSTA in the central‐eastern Pacific from the preceding winter to the summer. The 3–5‐year oscillation is most pronounced during the 1980s. 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| source | Wiley Journals; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Wiley Free Content; Wiley-Blackwell AGU Digital Library |
| subjects | Earth sciences Earth, ocean, space Exact sciences and technology interannual variability interdecadal variability WNP subtropical high |
| title | Interannual and interdecadal variability of the summertime western North Pacific subtropical high |
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