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Climate variation and prediction of rapid intensification in tropical cyclones in the western North Pacific

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Summary

One of the greatest challenges in tropical weather forecasting is the rapid intensification (RI) of the tropical cyclone (TC), during which its one-minute maximum sustained wind speed increases at least 30 knots per 24 hours. Here we identify and elucidate the climatic conditions that are critical to the frequency and location of the RI on annual, intraseasonal, and interannual time scales. Whereas RI and formation share common environmental preferences, we found that the percentage of TCs with RI varies annually and from year to year. In August, only 30% of TC actually experiences RI, in contrast to the annual maximum of 47% in November. The proportion of RI in July–September is higher during El Niño years (53%) than the corresponding one in the La Niña years (37%). Three climate factors may contribute to the increase in the proportion of RI: the southward shift in the monthly or seasonal mean location of the TC formation, the increase in the low-level westerly meridional shear vorticity, and the decrease in northerly vertical shear. When the mean latitude of TC formation increases, the mixed-layer heat content decreases while TC’s inertial stability increases; both are more detrimental to the RI than to TC formation because the RI requires large amount of latent heat energy being extracted efficiently from the ocean mixed layer and requires accelerated low-level radial inflow that carries latent heat reaching the inner core region.

We further demonstrate that the RI frequency in the Philippine Sea and South China Sea can be predicted 10 to 30 days in advance based on the convective anomalies in the equatorial western Pacific (5° S–5° N, 130°–150° E) on intraseasonal time scale. The Niño 3.4 SSTA in June is a potential predictor for the peak TC season (July–September) RI activity in the southeast quadrant of the western North Pacific (0–20° N, 140–180° E).

The RI is an essential characteristic of category 4 and 5 hurricanes and super typhoons because all category 4 and 5 hurricanes in the Atlantic basin and 90% of the super typhoons in the western North Pacific experience at least one RI process in their life cycles. Over the past 40 years, the annual total of RI in the western North Pacific shows pronounced interdecadal variation but no significant trend. This result suggests that the number of supper typhoons has no upward trend in the past 40 years. Our results also suggest that when the mean latitude, where the tropical storms form, shifts southward (either seasonally or from year to year) the proportion of super typhoon or major hurricane will likely increase. This shift is determined by large scale circulation change rather than local SST effects. This idea differs from the current notion that increasing SST can lead to more frequent occurrence of category 4 or 5 hurricanes through local thermodynamics.

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References

  • M Bister (2001) ArticleTitleEffect of peripheral convection on tropical cyclone formation J Atmos Sci 58 3463–3476 Occurrence Handle10.1175/1520-0469(2001)058<3463:EOPCOT>2.0.CO;2

    Article  Google Scholar 

  • S Brand (1973) ArticleTitleRapid intensification and low-latitude weakening of tropical cyclones of the western North Pacific Ocean J Appl Meteorol 12 94–103 Occurrence Handle10.1175/1520-0450(1973)012<0094:RIALLW>2.0.CO;2

    Article  Google Scholar 

  • JCL Chan (1985) ArticleTitleTropical cyclone activity in the Northwest Pacific in relation to the El Niño/Southern Oscillation phenomenon Mon Wea Rev 113 599–606 Occurrence Handle10.1175/1520-0493(1985)113<0599:TCAITN>2.0.CO;2

    Article  Google Scholar 

  • T-C Chen S-P Weng N Yamazai S Kiehne (1998) ArticleTitleInterannual variation in the tropical cyclone formation over western North Pacific Mon Wea Rev 126 1080–1090 Occurrence Handle10.1175/1520-0493(1998)126<1080:IVITTC>2.0.CO;2

    Article  Google Scholar 

  • M DeMaria (1996) ArticleTitleThe effect of vertical shear on tropical cyclone intensity change J Atmos Sci 53 2047–2087 Occurrence Handle10.1175/1520-0469(1996)053<2076:TEOVSO>2.0.CO;2

    Article  Google Scholar 

  • M DeMaria JD Pickle (1988) ArticleTitleA simplified system of equations for simulation of tropical cyclones J Atmos Sci 45 1542–1554 Occurrence Handle10.1175/1520-0469(1988)045<1542:ASSOEF>2.0.CO;2

    Article  Google Scholar 

  • DeMaria M, Zehr RM, Kossin JP, Knaff JA (2002) The use of GOES imagery in statistical hurricane intensity prediction. 25th Conf. on Hurricanes and Tropical Meteorology, San Diego, CA. Amer Meteor Soc, pp 120–121

  • VF Dvorak (1975) ArticleTitleTropical cyclone intensity analysis and forecasting from satellite imagery Mon Wea Rev 103 420–430 Occurrence Handle10.1175/1520-0493(1975)103<0420:TCIAAF>2.0.CO;2

    Article  Google Scholar 

  • KA Emanuel (1986) ArticleTitleAn air-sea interaction theory for tropical cyclones. Part I: Steady-state maintenance J Atmos Sci 43 585–604 Occurrence Handle10.1175/1520-0469(1986)043<0585:AASITF>2.0.CO;2

    Article  Google Scholar 

  • KA Emanuel (2005) ArticleTitleIncreasing destructiveness of tropical cyclones over the past 30 years Nature 436 686–688 Occurrence Handle10.1038/nature03906

    Article  Google Scholar 

  • WM Frank (1977a) ArticleTitleThe structure and energetics of the tropical cyclone I. Storm structure Mon Wea Rev 105 1119–1135 Occurrence Handle10.1175/1520-0493(1977)105<1119:TSAEOT>2.0.CO;2

    Article  Google Scholar 

  • WM Frank (1977b) ArticleTitleThe structure and energetic of the tropical cyclone II. Dynamics and energetics Mon Wea Rev 105 1136–1150 Occurrence Handle10.1175/1520-0493(1977)105<1136:TSAEOT>2.0.CO;2

    Article  Google Scholar 

  • WM Gray (1968) ArticleTitleGlobal view of the origin of tropical disturbances and storms Mon Wea Rev 96 669–700 Occurrence Handle10.1175/1520-0493(1968)096<0669:GVOTOO>2.0.CO;2

    Article  Google Scholar 

  • WM Gray (1984) ArticleTitleAtlantic seasonal hurricane frequency. Part I: El Niño and 30 mb quasi-bieniial osillation influences Mon Wea Rev 112 1649–1668 Occurrence Handle10.1175/1520-0493(1984)112<1649:ASHFPI>2.0.CO;2

    Article  Google Scholar 

  • WM Gray (1998) ArticleTitleThe formation of tropical cyclones Meteorol Atmos Phys 67 37–69 Occurrence Handle10.1007/BF01277501

    Article  Google Scholar 

  • Gross JM (2001) North Atlantic and East Pacific track and intensity verification for 2000. Minutes of the 55th Interdepartmental Hurricane Conf., Miami, FL, Office of the Federal Coordinator for Meteorological Services and Supporting Research, NOAA, B12–B15. [Available from Federal Coordinator for Meteorological Services and Supporting Research, 6101 Executive Blvd, Ste. 900, Rockville, MD 20852]

  • JD Hall AJ Mathews DJ Karoly (2001) ArticleTitleThe modulation of tropical cyclone activity in the Australian region by Madden-Julian Oscillation Mon Wea Rev 129 2970–2982 Occurrence Handle10.1175/1520-0493(2001)129<2970:TMOTCA>2.0.CO;2

    Article  Google Scholar 

  • Harr PA (2006) Temporal clustering of tropical cyclone occurrence on intraseasonal time. 27th Conf. on Hurricanes and Tropical Meteorology, Monterey, CA. Amer Meteor Soc, 3D.2

  • HH Hendon B Liebmann (1994) ArticleTitleOrganization of convection within the Madden-Julian oscillation J Geophys Res 99 8073–8083 Occurrence Handle10.1029/94JD00045

    Article  Google Scholar 

  • GJ Holland (1995) ArticleTitleScale interaction in the western Pacific monsoon Meteor Atmos Phys 56 57–79 Occurrence Handle10.1007/BF01022521

    Article  Google Scholar 

  • CR Holliday AH Thompson (1979) ArticleTitleClimatological characteristics of rapidly intensification typhoons Mon Wea Rev 107 1022–1034 Occurrence Handle10.1175/1520-0493(1979)107<1022:CCORIT>2.0.CO;2

    Article  Google Scholar 

  • Hsu H-H, Lo A-K, Hung C-H, Wu C-C (2006) Possible feedback of tropical cyclone on climate variability. 27th Conf. on Hurricanes and Tropical Meteorology, Monterey, CA. Amer Meteor Soc, 11C.6

  • C Jones LMV Carvalho RW Higgins DE Waliser J-KE Schemm (2004) ArticleTitleClimatology of tropical intraseasonal convective anomalies: 1979–2002 J Climate 17 523–539 Occurrence Handle10.1175/1520-0442(2004)017<0523:COTICA>2.0.CO;2

    Article  Google Scholar 

  • J Kaplan M DeMaria (2003) ArticleTitleLarge-scale characteristics of rapidly intensifying tropical cyclones in the north Atlantic basin Wea Forecast 18 1093–1108 Occurrence Handle10.1175/1520-0434(2003)018<1093:LCORIT>2.0.CO;2

    Article  Google Scholar 

  • S Kemball-Cook B Wang (2001) ArticleTitleEquatorial waves and air-sea interaction in the boreal summer intraseasonal oscillation J Climate 14 2923–2942 Occurrence Handle10.1175/1520-0442(2001)014<2923:EWAASI>2.0.CO;2

    Article  Google Scholar 

  • MA Lander (1994a) ArticleTitleAn exploratory analysis of the relationship between tropical storm formation in the western North Pacific and ENSO Mon Wea Rev 122 636–651 Occurrence Handle10.1175/1520-0493(1994)122<0636:AEAOTR>2.0.CO;2

    Article  Google Scholar 

  • MA Lander (1994b) ArticleTitleDescription of a monsoon gyre and its effects on the tropical cyclones in western North Pacific during August 1991 Wea Forecast 9 640–654 Occurrence Handle10.1175/1520-0434(1994)009<0640:DOAMGA>2.0.CO;2

    Article  Google Scholar 

  • Landsea CW (2000) El Niño/Southern Oscillation and the Seasonal Predictability of Tropical Cyclones. In: El Niño and the Southern Oscillation: multiscale variability and global and regional impacts (Diaz HF, Markgraf V, eds). Cambridge University Press, pp 149–181

  • KM Lau PH Chan (1986) ArticleTitleAspects of 40–50 day oscillation during the northern summer as inferred from outgoing longwave radiation Mon Wea Rev 114 1354–1367 Occurrence Handle10.1175/1520-0493(1986)114<1354:AOTDOD>2.0.CO;2

    Article  Google Scholar 

  • N-C Lau B Wang (2006) Interactions between the Asian monsoon and the El Niño/Southern Oscillation The Asian Monsoon Praxis Berlin 479–511 Occurrence Handle10.1007/3-540-37722-0_12

    Chapter  Google Scholar 

  • X Li B Wang (1996) ArticleTitleAcceleration of the hurricane beta drift by shear strain rate of an environmental flow J Atmos Sci 53 327–334 Occurrence Handle10.1175/1520-0469(1996)053<0327:AOTHBD>2.0.CO;2

    Article  Google Scholar 

  • B Liebmann HH Hendon JJ Glick (1994) ArticleTitleThe relationship between tropical cylones of the Western Pacific and Indian Oceans and the Madden-Julian Oscillation J Meteor Soc Japan 72 401–412

    Google Scholar 

  • I-I Lin C-C Wu KA Emanuel I-H Lee C-R Wu I-F Pun (2005) ArticleTitleThe interaction of Supertyphoon Maemi (2003) with a warm ocean Eddy Mon Wea Rev 133 2635–2649 Occurrence Handle10.1175/MWR3005.1

    Article  Google Scholar 

  • ED Maloney DL Hartmann (2000) ArticleTitleModulation of eastern North Pacific hurricanes by the Madden-Julian oscillation J Climate 13 1451–1460 Occurrence Handle10.1175/1520-0442(2000)013<1451:MOENPH>2.0.CO;2

    Article  Google Scholar 

  • ED Maloney DL Hartmann (2001) ArticleTitleThe Madden-Julian oscillation, barotropic dynamics, and north Pacific tropical cyclone formation. Part I: Observation J Atmos Sci 58 2545–2558 Occurrence Handle10.1175/1520-0469(2001)058<2545:TMJOBD>2.0.CO;2

    Article  Google Scholar 

  • J Molinari D Vollaro KL Corbosiero (2004) ArticleTitleTropical cyclone formation in a sheared environment: a case study J Atmos Sci 61 2493–2509 Occurrence Handle10.1175/JAS3291.1

    Article  Google Scholar 

  • MT Montgomery J Enagonio (1998) ArticleTitleTropical cyclogenesis via convectively forced vortex Rossby waves in three-dimensional quasi–geostrophic model J Atmos Sci 55 3176–3207 Occurrence Handle10.1175/1520-0469(1998)055<3176:TCVCFV>2.0.CO;2

    Article  Google Scholar 

  • T Nakazawa (1988) ArticleTitleTropical super clusters within intraseasonal variations over the western Pacific J Meteor Soc Japan 66 823–839

    Google Scholar 

  • Ventham JD, Wang B (2007) Large scale flow patterns and their influence on the intensification rates of western north Pacific tropical stroms. Mon Wea Rev (in press)

  • B Wang JCL Chan (2002) ArticleTitleHow strong ENSO events affect tropical storm activity over the western North Pacific J Climate 15 1643–1658 Occurrence Handle10.1175/1520-0442(2002)015<1643:HSEEAT>2.0.CO;2

    Article  Google Scholar 

  • B Wang Z Fan (1999) ArticleTitleChoice of south Asian summer monsoon indices Bull Amer Meteor Sci 80 629–638 Occurrence Handle10.1175/1520-0477(1999)080<0629:COSASM>2.0.CO;2

    Article  Google Scholar 

  • B Wang H Rui (1990) ArticleTitleSynoptic climatology of transient tropical intraseasonal convection anomalies: 1975–1985 Meteorol Atmos Phys 44 43–61 Occurrence Handle10.1007/BF01026810

    Article  Google Scholar 

  • B Wang R Wu K-M Lau (2001) ArticleTitleInterannual variability of Asian summer monsoon: contrast between the Indian and western North Pacific–West Asian monsoon J Climate 14 4073–4090 Occurrence Handle10.1175/1520-0442(2001)014<4073:IVOTAS>2.0.CO;2

    Article  Google Scholar 

  • B Wang L Ho Y Zhang M-M Lu (2004) ArticleTitleDefinition of South China Sea monsoon onset and commencement of East Asia summer monsoon J Climate 17 699–710

    Google Scholar 

  • Wang B, Webster P, Kikuchi K, Yasunari T, Qi Y (2006) Boreal summer quasi–monthly oscillation in the global tropics. Clim Dynam (DOI: 10.1007/s00382-006-0163-3)

  • PJ Webster GJ Holland JA Curry HR Chang (2005) ArticleTitleChanges in tropical cyclone number, duration, and intensity in a warming environment Science 309 1844–1846 Occurrence Handle10.1126/science.1116448

    Article  Google Scholar 

  • L Wu B Wang (2004) ArticleTitleAssessing impacts of global warming on tropical cyclone tracks J Climate 17 1686–1698 Occurrence Handle10.1175/1520-0442(2004)017<1686:AIOGWO>2.0.CO;2

    Article  Google Scholar 

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Authors and Affiliations

  1. Department of Meteorology, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, Honolulu, Hawaii, USA

    B. Wang & X. Zhou

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  1. B. Wang
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Correspondence to B. Wang.

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Corresponding author’s address: Bin Wang, Department of Meteorology, University of Hawaii, 2525 Correa Rd., Honolulu, Hawaii 96822, USA (also visiting professor at the Ocean University of China)

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Wang, B., Zhou, X. Climate variation and prediction of rapid intensification in tropical cyclones in the western North Pacific. Meteorol Atmos Phys 99, 1–16 (2008). https://doi.org/10.1007/s00703-006-0238-z

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