Article Contents

INFLUENCE ON NORTHERN PACIFIC STORM TRACK OF EQUATO-RIAL CENTRAL AND EASTERN PACIFIC SSTA DURING WINTER

Funding:

  • Singular value decomposition (SVD) is conducted of 15 winter tropical Pacific SST with 500 hPa filtered potential height variance over the northern Pacific storm track. It is shown that the first coupled mode obtained depicts the effect on the track of SSTA over equatorial central and eastern Pacific. Further composite analysis indicates that the SSTA over there during winter can give rise to or invigorate PNA teleconnection response pattern in 500 hPa height field which, in turn, exerts crucial influence on the interannual variability in vigor and east-west displacement of the Pacific storm track, especially over its central and eastern part.
  • [1] BLACKMON M L,1976.A climatological spectral sudy of the 500 hPa geopotential height of the Northern Hemisphere[J].J.Atmos.Sci.,33:1607-1623.
    [2] BLACKMON M L,WALLACE J M,LAU N-C et al.,1977.An observation study of the Northern Hemisphere wintertime circulation[J].J.Atmos.Sci.,33:1607-1623.
    [3] BRETHERTON C S,SMITH C,WALLACE J M,1992.An intercomparison of methods for finding coupled patterns in climate data[J].J.Climate.,5:541-560.
    [4] CAI M,MAK M,1990.On the dynamics of regional cyclogenesis[J].J.Atmos.Sci.,47:1417-1442.
    [5] CHANG E K,ORLANSKI M I,1993.On the dynamics of a storm tracks[J].J.Atmos.Sci.,50:999-1015.
    [6] DENG Xing-xiu,SUN Zhao-bo,1994.Features of temporal evolution of storm track in Northern Hemisphere(in Chinese)[J].J.Nanjing Inst.Met.,17:165-170.
    [7] HELD I M,LYONS S W,NIGAM S,1989.Transients and the extratropical response to El Niño[J].J.Atmos.Sci.,46:163-174.
    [8] HOERLING M P,TING M,1994.Organization of extratropical transient during El Niño[J].J.Climate.,7:745-766.
    [9] HOSKINS B J,VALDES P J,1990.On the existence of storm tracks[J].J.Atmos.Sci.,47:1854-1864.
    [10] HUANG Rong-hui,1991.Teleconnections of atmospheric circulation(in Chinese)[A].In:Contemporary Study of Climate[C],edited by YE Du-zheng et al.Beijing:China Meteorological Press,113-136.
    [11] HU Zeng-zhen,HUANG Rong-hui,1997.The interannual variation of the convective activity in the tropical west Pacific in winter and its effect on the storm track in the north Pacific(in Chinese)[J].Sci.,Atmos. Sin.,21:513-522.
    [12] LAU N-C,1979.The structure and energetics of transient disturbance in the Northern Hemisphere wintertime circulation[J].J.Atmos.Sci.,36:982-995.
    [13] STRAUS D M,SHUKLA J,1997.Variations of midlatitude transient dynamics associated with ENSO[J].J.Atmos.Sci.,54:777-790.
    [14] SUN Zhao-bo,ZHU Wei-jun,1998.A possible mechanism for the maintenance of the Northern Hemisphere wintertime storm tracks(in Chinese)[J].J.Nanjing Inst.Met.,21:299-306.
    [15] WALLACE J M,SMITH C,BRETHERTON C S,1992.Singular value decomposition of wintertime sea surface temperature and 500-mb height anomalies[J].J.Climate.,5:561-576.
    [16] ZHU Wei-jun,SUN Zhao-bo,1998.ENSO effect on the maintenance of wintertime Pacific storm track(in Chinese)[J].J.Nanjing Inst.Met.,21:189-195.

Get Citation+

ZHU Wei-jun, SUN Zhao-bo, MIN Jin-zhong, et al. INFLUENCE ON NORTHERN PACIFIC STORM TRACK OF EQUATO-RIAL CENTRAL AND EASTERN PACIFIC SSTA DURING WINTER [J]. Journal of Tropical Meteorology, 2000, 6(1): 106-112.
ZHU Wei-jun, SUN Zhao-bo, MIN Jin-zhong, et al. INFLUENCE ON NORTHERN PACIFIC STORM TRACK OF EQUATO-RIAL CENTRAL AND EASTERN PACIFIC SSTA DURING WINTER [J]. Journal of Tropical Meteorology, 2000, 6(1): 106-112.
Export:  

Share Article

Manuscript History

Manuscript received: 20 October 1999
Manuscript revised: 06 March 2000
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

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

INFLUENCE ON NORTHERN PACIFIC STORM TRACK OF EQUATO-RIAL CENTRAL AND EASTERN PACIFIC SSTA DURING WINTER

Abstract: Singular value decomposition (SVD) is conducted of 15 winter tropical Pacific SST with 500 hPa filtered potential height variance over the northern Pacific storm track. It is shown that the first coupled mode obtained depicts the effect on the track of SSTA over equatorial central and eastern Pacific. Further composite analysis indicates that the SSTA over there during winter can give rise to or invigorate PNA teleconnection response pattern in 500 hPa height field which, in turn, exerts crucial influence on the interannual variability in vigor and east-west displacement of the Pacific storm track, especially over its central and eastern part.

ZHU Wei-jun, SUN Zhao-bo, MIN Jin-zhong, et al. INFLUENCE ON NORTHERN PACIFIC STORM TRACK OF EQUATO-RIAL CENTRAL AND EASTERN PACIFIC SSTA DURING WINTER [J]. Journal of Tropical Meteorology, 2000, 6(1): 106-112.
Citation: ZHU Wei-jun, SUN Zhao-bo, MIN Jin-zhong, et al. INFLUENCE ON NORTHERN PACIFIC STORM TRACK OF EQUATO-RIAL CENTRAL AND EASTERN PACIFIC SSTA DURING WINTER [J]. Journal of Tropical Meteorology, 2000, 6(1): 106-112.
Reference (16)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return