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Volume 18 Issue 5

Sep.  2001

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Article >  ADVANCES IN ATMOSPHERIC SCIENCES  > 2001 >  18(5): 1029-1042

The Impact of Pacific SSTA on the Interannual Variability of Northern Pacific Storm Track during Winter

  • 1.

    Nanjing Institute of Meteorology, Nanjing 210044,Nanjing Institute of Meteorology, Nanjing 210044,LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029

  • Investigation is conducted of the interannual variability of the northern Pacific storm track and its con current association with 500 hPa height and Pacific sea surface temperature (SST) during winter. Evidence suggests that during the studying period the center of the northern winter Pacific storm track experiences substantial interannual variability in the variation of its latitude, longitude and intensity. Singular value de composition (SVD) of 15 winter 500 hPa filtered geopotential height variance over the storm track with the tropical and northern Pacific SST shows that the first coupled mode depicts the effect on the track of SSTA over the equatorial central and eastern Pacific, while the second one reflects the impact of Kuroshio SSTA on the track. Further Composite analysis indicates, moreover, that the SSTA over Kuroshio (equatorial cen tral and eastern Pacific) during winter, which is relative to WP (PNA) teleconnection response pattern in 500 hPa height field, respectively, exerts crucial influence on the interannual variability in vigor and meridianal (zonal) displacement of the track over its central and western (eastern) part.
  • [1] LIU Chengji, REN Xuejuan*, and YANG Xiuqun, 2014: Mean FlowStorm Track Relationship and RossbyWave Breaking in Two Types of El-Nio, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 197-210.  doi: 10.1007/s00376-013-2297-7
    [2] WANG Hai, and LIU Qinyu, 2014: Boreal Winter Rainfall Anomaly over the Tropical Indo-Pacific and Its Effect on Northern Hemisphere Atmospheric Circulation in CMIP5 Models, ADVANCES IN ATMOSPHERIC SCIENCES, 31, 916-925.  doi: 10.1007/s00376-013-3174-0
    [3] ZHU Weijun, Yongsheng ZHANG, 2009: Summertime Atmospheric Teleconnection Pattern Associated with a Warming over the Eastern Tibetan Plateau, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 413-422.  doi: 10.1007/s00376-009-0413-5
    [4] Chao ZHANG, Hailong LIU, Jinbo XIE, Chongyin LI, Pengfei LIN, 2020: Impacts of Increased SST Resolution on the North Pacific Storm Track in ERA-Interim, ADVANCES IN ATMOSPHERIC SCIENCES, 37, 1256-1266.  doi: 10.1007/s00376-020-0072-0
    [5] Guidi ZHOU, Xuhua CHENG, 2022: Impacts of Oceanic Fronts and Eddies in the Kuroshio-Oyashio Extension Region on the Atmospheric General Circulation and Storm Track, ADVANCES IN ATMOSPHERIC SCIENCES, 39, 22-54.  doi: 10.1007/s00376-021-0408-4
    [6] Zhu Weijun, Sun Zhaobo, 1999: Influence of ENSO Event on the Maintenance of Pacific Storm Track in the Northern Winter, ADVANCES IN ATMOSPHERIC SCIENCES, 16, 630-640.  doi: 10.1007/s00376-999-0037-9
    [7] Li Zhijin, Ji Liren, 1996: Internal Dynamics of the Generation of Atmospheric Teleconnection Patterns, ADVANCES IN ATMOSPHERIC SCIENCES, 13, 19-32.  doi: 10.1007/BF02657025
    [8] Jinling PIAO, Wen CHEN, Ke WEI, Yong LIU, Hans-F. GRAF, Joong-Bae AHN, Alexander POGORELTSEV, 2017: An Abrupt Rainfall Decrease over the Asian Inland Plateau Region around 1999 and the Possible Underlying Mechanism, ADVANCES IN ATMOSPHERIC SCIENCES, 34, 456-468.  doi: 10.1007/s00376-016-6136-5
    [9] Zhuozhuo Lü, Shengping HE, Fei LI, Huijun WANG, 2019: Impacts of the Autumn Arctic Sea Ice on the Intraseasonal Reversal of the Winter Siberian High, ADVANCES IN ATMOSPHERIC SCIENCES, 36, 173-188.  doi: 10.1007/s00376-017-8089-8
    [10] Huang Fei, Zhou Faxiu, Qian Xiaodan, 2002: Interannual and Decadal Variability of the North Pacific Blocking and Its Relationship to SST,Teleconnection and Storm Tracks, ADVANCES IN ATMOSPHERIC SCIENCES, 19, 807-820.  doi: 10.1007/s00376-002-0046-4
    [11] Xiaozhen LIN, Chaofan LI, Riyu LU, Adam A. SCAIFE, 2018: Predictable and Unpredictable Components of the Summer East Asia-Pacific Teleconnection Pattern, ADVANCES IN ATMOSPHERIC SCIENCES, 35, 1372-1380.  doi: 10.1007/s00376-018-7305-5
    [12] WANG Huijun, 2005: The Circum-Pacific Teleconnection Pattern in Meridional Wind in the High Troposphere, ADVANCES IN ATMOSPHERIC SCIENCES, 22, 463-466.  doi: 10.1007/BF02918759
    [13] WANG Yafei, Fujiyaoshi YASUSHI, Kato KURANOSHIN, 2003: A Teleconnection Pattern Related with the Development of the Okhotsk High and the Northward Progress of the Subtropical High in East Asian Summer, ADVANCES IN ATMOSPHERIC SCIENCES, 20, 237-244.  doi: 10.1007/s00376-003-0009-4
    [14] Junhu ZHAO, Liu YANG, Bohui GU, Jie YANG, Guolin FENG, 2016: On the Relationship between the Winter Eurasian Teleconnection Pattern and the Following Summer Precipitation over China, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 743-752.  doi: 10.1007/s00376-015-5195-3
    [15] SONG Jie, LI Chongyin, ZHOU Wen, PAN Jing, 2009: The Linkage between the Pacific-North American Teleconnection Pattern and the North Atlantic Oscillation, ADVANCES IN ATMOSPHERIC SCIENCES, 26, 229-239.  doi: 10.1007/s00376-009-0229-3
    [16] K. Gambo, Lu Li, Li Weijing, 1987: NUMERICAL SIMULATION OF EURASIAN TELECONNECTION PATTERN IN ATMOSPHERIC CIRCULATION DURING THE NORTHERN HEMISPHERE WINTER, ADVANCES IN ATMOSPHERIC SCIENCES, 4, 385-394.  doi: 10.1007/BF02656739
    [17] Chang-Hoi HO, Joo-Hong KIM, Hyeong-Seog KIM, Woosuk CHOI, Min-Hee LEE, Hee-Dong YOO, Tae-Ryong KIM, Sangwook PARK, 2013: Technical Note on a Track-pattern-based Model for Predicting Seasonal Tropical Cyclone Activity over the Western North Pacific, ADVANCES IN ATMOSPHERIC SCIENCES, 30, 1260-1274.  doi: 10.1007/s00376-013-2237-6
    [18] Hong HUANG, Dan WU, Yuan WANG, Zhen WANG, Yu LIU, 2024: Track-Pattern-Based Characteristics of Extratropical Transitioning Tropical Cyclones in the Western North Pacific, ADVANCES IN ATMOSPHERIC SCIENCES.  doi: 10.1007/s00376-023-2330-4
    [19] Minghao YANG, Chongyin LI, Xin LI, Xiong CHEN, Lifeng LI, 2022: The Linkage between Midwinter Suppression of the North Pacific Storm Track and Atmospheric Circulation Features in the Northern Hemisphere, ADVANCES IN ATMOSPHERIC SCIENCES, 39, 502-518.  doi: 10.1007/s00376-021-1145-4
    [20] Jingchao LONG, Suping ZHANG, Yang CHEN, Jingwu LIU, Geng HAN, 2016: Impact of the Pacific-Japan Teleconnection Pattern on July Sea Fog over the Northwestern Pacific: Interannual Variations and Global Warming Effect, ADVANCES IN ATMOSPHERIC SCIENCES, 33, 511-521.  doi: 10.1007/s00376-015-5097-4
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    • Manuscript History

    Manuscript received: 10 September 2001
    Manuscript revised: 10 September 2001
    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

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    The Impact of Pacific SSTA on the Interannual Variability of Northern Pacific Storm Track during Winter

    • 1. Nanjing Institute of Meteorology, Nanjing 210044,Nanjing Institute of Meteorology, Nanjing 210044,LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029
    • Manuscript received: 2001-09-10
    • Manuscript revised: 2001-09-10

    Abstract: Investigation is conducted of the interannual variability of the northern Pacific storm track and its con current association with 500 hPa height and Pacific sea surface temperature (SST) during winter. Evidence suggests that during the studying period the center of the northern winter Pacific storm track experiences substantial interannual variability in the variation of its latitude, longitude and intensity. Singular value de composition (SVD) of 15 winter 500 hPa filtered geopotential height variance over the storm track with the tropical and northern Pacific SST shows that the first coupled mode depicts the effect on the track of SSTA over the equatorial central and eastern Pacific, while the second one reflects the impact of Kuroshio SSTA on the track. Further Composite analysis indicates, moreover, that the SSTA over Kuroshio (equatorial cen tral and eastern Pacific) during winter, which is relative to WP (PNA) teleconnection response pattern in 500 hPa height field, respectively, exerts crucial influence on the interannual variability in vigor and meridianal (zonal) displacement of the track over its central and western (eastern) part.

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