Marine hydrology

Relationship between typhoon activity in the northwestern Pacific and the up-per-ocean heat content on interdecadal time scale

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  • 1. Key Laboratory of Tropical Marine Environmental Dynamics, South China Sea Institute of Oceanology, CAS, Guangzhou 510301, China; 2. Guy Carpenter Asia-Pacific Climate Impact Centre, School of Energy and Environment, City University of Hong Kong, Hong Kong 00852, China
刘钦燕(1976—), 女, 山东省青岛市人, 博士, 从事海洋-大气相互作用相关研究。E-mail: qyliu66@scsio.ac.cn

Received date: 2009-04-02

  Revised date: 2010-05-17

  Online published: 2010-12-15

Supported by

广东省联合基金项目(U0733002); 国家自然科学基金项目(40806005); 中国科学院南海海洋研究所青年基金项目(SQ200814)

Abstract

The typhoon activity in the northwestern Pacific region (5º-30ºN, 121ºE-180º) is analyzed using the tropical cy-clone data from 1945 to 2003 provided by the Joint Typhoon Warning Center. The results show that the typhoon activity in the northwestern Pacific has evident interdecadal variability. The number of typhoons occurred in 1958-1968 is more than that occurred in 1985-1995, and both numbers are more than that occurred in 1970-1980. Combining the analysis of the up-per-ocean heat content data and temperature data at 11 standard levels provided by the Scripps Institute of Oceanography, it is found that the typhoon activity in the northwestern Pacific has a relationship with the ocean thermal structures. The sea-surface temperature is not the key factor affecting the typhoon number occurred during 1958-1968. The decadal variation of the typhoons occurred in the northwestern Pacific is positively correlated with the upper-ocean heat content in the equatorial central Pacific. There is a sea-surface temperature increase in the central Pacific in 1958-1968 and 1985-1995 compared with 1970-1980 by the mean-temperature profile along the equator, which exists in the surface in 1985-1995 and in the subsurface in 1958-1968. This difference may imply that the subsurface temperature warming played an important role in increased number of typhoon in 1958-1968.

Cite this article

LIU Qin-yan,ZHOU Wen . Relationship between typhoon activity in the northwestern Pacific and the up-per-ocean heat content on interdecadal time scale[J]. Journal of Tropical Oceanography, 2010 , 29(6) : 8 -14 . DOI: 10.11978/j.issn.1009-5470.2010.06.008

References

[1]       CHAN J C L. Tropical cyclone activity in the Northwest Pacific in relation to the El Niño/Southern Oscillation phenomenon [J]. Mon Wea Rev, 1985, 113(4): 599-606.

[2]       LANDER M A. An exploratory analysis of the relationship between tropical storm formation in the Western North Pacific and ENSO [J]. Mon Wea Rev, 1994, 122(4): 636-651.

[3]       CHAN J C L. Tropical cyclone activity over the western North Pacific associated with El Niño and La Niña events [J]. J Climate, 2000, 13: 2960-2972.

[4]       CHIA H H, ROPELEWSKI C F. The interannual variability in the gene-sis location of tropical cyclones in the Northwest Pacific [J]. J Clim, 2002, 15(20): 2934-2944.

[5]       WU M C, ChANG W L, LEUNG W M. Impacts of El Niño-Southern Oscillation events on tropical cyclone land-falling activity in the Western North Pacific [J]. J Clim, 2004, 17(6): 1419-1428.

[6]       CAMARGO S J, SOBEL A H. Western North Pacific tropical cyclone intensity and ENSO [J]. J Clim, 2005, 18(15): 2996-3006.

[7]       陈光华, 黄荣辉. 西北太平洋暖池热状态对热带气旋活动的影响[J]. 热带气象学报, 2006, 22(6): 527-532.

[8]       黄荣辉,陈光华. 西北太平洋热带气旋移动路径的年际变化及其机理研究[J]. 气象学报, 2007, 65(5): 683-694.

[9]       WANG B, CHAN J C L. How strong ENSO events affect tropical storm activity over the Western North Pacific [J]. J Clim, 2002, 15(13): 1643-1658.

[10]    袁金南 林爱兰 刘春霞. 60年来西北太平洋上不同强度热带气旋的变化特征[J]. 气象学报, 2008, 66(2): 213-223.

[11]    MAO Q, CHANG S W, PFEFFER R L. Influence of Large-Scale Initial Oceanic Mixed Layer Depth on Tropical Cyclones [J]. Mon Wea Rev, 2000, 128(12): 4058-4070.

[12]    CHAN J C L, DUAN Y H, SHAY L K. Tropical cyclone intensity change from a simple ocean-atmosphere coupled model [J]. J Atmos Sci, 2001, 58: 154-172.

[13]    HONG X, CHANG S W, RAMAN S, et al. The interaction between Hurricane Opal (1995) and a warm core ring in the Gulf of Mexico [J]. Mon Wea Rev, 2000, 128: 1347-1365.

[14]    LIN I-I, WU C C, EMANUEL K A, et al. The interaction of supertyphoon Maemi (2003) with a warm ocean eddy [J]. Mon Wea Rev, 2005, 133(9): 2635-2649.

[15]    蒋小平. 南海热带气旋过程中的海气相互作用研究 [D].南京: 中国人民解放军理工大学, 2008.

[16]    EMANUEL K A. Thermodynamic control of hurricane intensity [J]. Nature, 1999, 401: 665-669.

[17]    CLAUDIA PASQUERO, KERRY EMANUEL. Tropical cyclones and transient upper-ocean warming [J]. Journal of Climate, 2008, 21: 149-162.

[18]    LEIPPER D F. Observed ocean conditions and Hurricane Hilda (1964) [J]. J Atmos Sci, 1967, 24: 182-196.

[19]    GRAY W M. Hurricanes: Their formation, structure, and likely role in the tropical circulation. Meteorology over the Tropical Oceans [M]//SHAW D B. Royal Meteorological Society, 1979: 155-199.

[20]    WADA A, USUI N. Importance of tropical cyclone heat potential for tropical cyclone intensity and intensification in the Western North Pacific [J]. J Oceanogr, 2007, 63: 427-447.

[21]    WANG L, FUNG C H, LAU K H. The upper ocean thermal structure and the genesis location of tropical cyclones in the South China Sea [J]. J Ocean Univ Chin, 2007, 6(2): 125-131.

[22]    王会军, 范可. 西北太平洋台风生成频次与南极涛动的关系[J]. 科学通报, 2006, 51(24): 2910-2914.

[23]    CHAN J C L. Comments on “Changes in tropical cyclone number, duration, and intensity in a warming environment” [J]. Science, 311, 1713b.

[24]    储惠芸, 王元, 伍荣生. 上层海洋热力异常对西北太平洋热带气旋气候特征的影响 [J].南京大学学报, 2007, 43(6): 581-588.

[25]    HO C H, BAIK J J, KIM J H, et al. Interdecadal changes in summertime typhoon tracks [J]. J Clim, 2004, 17: 1767-1776.

[26]    GRAY W M. Global view of the origin of tropical disturbances and storms [J]. Mon Wea Rev, 1968, 96: 669-700.


 

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