Changes of tropical cyclone size in three oceanic basins of the northern hemisphere from 2001 to 2021

Banglin ZHANG , Jeremy Cheuk-Hin LEUNG , Shengyuan LIU , Jianjun XU

Front. Earth Sci. ›› 2024, Vol. 18 ›› Issue (2) : 312 -323.

PDF (10283KB)
Front. Earth Sci. ›› 2024, Vol. 18 ›› Issue (2) : 312 -323. DOI: 10.1007/s11707-022-1064-4
RESEARCH ARTICLE

Changes of tropical cyclone size in three oceanic basins of the northern hemisphere from 2001 to 2021

Author information +
History +
PDF (10283KB)

Abstract

In this study the changes of tropical cyclone (TC) size from 2001 to 2021 are analyzed based on linear and quadratic curve fittings of the National Hurricane Center (NHC) / Joint Typhoon Warning Center (JTWC) best track data, based on the radius of maximum wind (RMW) and the average radius of 34-kt wind (AR34), in three oceanic basins of the North Atlantic (NATL), the Western North Pacific (WPAC) and the Eastern North Pacific (EPAC). The computations are done separately for two categories of tropical cyclones: tropical storms (TS) and hurricanes (HT). Size changes of landfalling and non-landfalling TCs are also discussed. Results show that there is a great inter-basin variability among the changes in TC sizes. Major conclusions include: 1) overall, the inner cores of TSs have become larger in all three basins, with the increasing tendencies being significant in the NATL and WAPC, while those of HTs mostly get smaller or remain similar; 2) meanwhile, comparatively large inter-basin differences are observed for the TC outer core sizes, and the sizes of landfalling TCs; 3) particularly, a significant decrease in landfalling HT outer core size is observed over the EPAC; 4) in contrast, significant increases in landfalling TS inner core size are found over the NATL and WPAC. The presented analysis results could benefit future research about TC forecasts, storm surge studies, and the cyclone climate and its changes.

Graphical abstract

Keywords

tropical cyclone / storm size / frequency / intensity / duration

Cite this article

Download citation ▾
Banglin ZHANG, Jeremy Cheuk-Hin LEUNG, Shengyuan LIU, Jianjun XU. Changes of tropical cyclone size in three oceanic basins of the northern hemisphere from 2001 to 2021. Front. Earth Sci., 2024, 18(2): 312-323 DOI:10.1007/s11707-022-1064-4

登录浏览全文

4963

注册一个新账户 忘记密码

References

[1]

Barbosa S M (2011). Testing for deterministic trends in global sea surface temperature.J Clim, 24(10): 2516–2522

[2]

Carrasco C, Landsea C, Lin Y (2014). The influence of tropical cyclone size on its intensification.Weather Forecast, 29(3): 582–590

[3]

Chan K T F, Chan J C L (2015). Global climatology of tropical cyclone size as inferred from QuikSCAT data.Int J Climatol, 35(15): 4843–4848

[4]

Chavas D R, Emanuel K A (2010). A QuikSCAT climatology of tropical cyclone size.Geophys Res Lett, 37(18): L18816

[5]

Chavas D R, Lin N, Emanuel K (2015). A model for the complete radial structure of the tropical cyclone wind field. Part I: Comparison with observed structure.J Atmos Sci, 72(9): 3647–3662

[6]

Chen D Y C, Cheung K K W, Lee C S (2011). Some implications of core regime wind structures in western North Pacific tropical cyclones.Weather Forecast, 26(1): 61–75

[7]

Demuth J, DeMaria M, Knaff J A (2006). Improvement of advanced microwave sounder unit tropical cyclone intensity and size estimation algorithms.J Appl Meteorol Climatol, 45(11): 1573–1581

[8]

Doocy S, Dick A, Daniels A, Kirsch T D (2013). The human impact of tropical cyclones: a historical review of events 1980–2009 and systematic literature review. PLoS Curr, doi: 10.1371/currents.dis.2664354a5571512063ed29ed29d25ffbce74

[9]

Emanuel K (2005). Increasing destructiveness of tropical cyclones over the past 30 years.Nature, 436(7051): 686–688

[10]

Emanuel K A (2012). Self-stratification of tropical cyclone outflow. Part II: implications for storm intensification.J Atmos Sci, 69(3): 988–996

[11]

Emanuel K A, Sobel A (2013). Response of tropical sea surface temperature, precipitation, and tropical cyclone–related variables to changes in global and local forcing.J Adv Model Earth Syst, 5(2): 447–458

[12]

Emanuel K A, Sundararajan R, Williams J (2008). Hurricanes and global warming: results from downscaling IPCC AR4 simulations.Bull Am Meteorol Soc, 89(3): 347–368

[13]

Grinsted A, Moore J C, Jevrejeva S (2012). Homogeneous record of Atlantic hurricane surge threat since 1923.Proc Natl Acad Sci USA, 109(48): 19601–19605

[14]

Irish J L, Resio D T, Ratcliff J J (2008). The influence of storm size on hurricane surge.J Phys Oceanogr, 38(9): 2003–2013

[15]

Islam M R, Lee C Y, Mandli K T, Takagi H (2021). A new tropical cyclone surge index incorporating the effects of coastal geometry, bathymetry and storm information.Sci Rep, 11(1): 16747

[16]

Islam M R, Satoh M, Takagi H (2022). Tropical cyclones affecting Japan central coast and changing storm surge hazard since 1980.J Meteorol Soc Jpn, 100(3): 493–507

[17]

Jin F F, Boucharel J, Lin I I (2014). Eastern Pacific tropical cyclones intensified by El Niño delivery of subsurface ocean heat.Nature, 516(7529): 82–85

[18]

Kimball S K, Mulekar M S (2004). A 15-year climatology of North Atlantic tropical cyclones. Part I: Size parameters.J Climate, 17: 3555–3575

[19]

Kishimoto K (2008). Revision of JMA’s early stage Dvorak analysis and its use to analyze tropical cyclones in the early developing stage.RSMC Tokyo-Typhoon Center Technical Review, 10: 1–12

[20]

Klotzbach P J (2006). Trends in global tropical cyclone activity over the past twenty years (1986–2005).Geophys Res Lett, 33(10): L10805

[21]

Klotzbach P J, Bell M M, Bowen S G, Gibney E J, Knapp K R, Schreck C J (2020). Surface pressure a more skillful predictor of normalized hurricane damage than maximum sustained wind.Bull Am Meteorol Soc, 101(6): E830–E846

[22]

Klotzbach P J, Landsea C W (2015). Extremely intense hurricanes: revisiting Webster et al. (2005) after 10 Years.J Clim, 28(19): 7621–7629

[23]

Knaff J A, Longmore S P, Molenar D A (2014). An objective satellite-based tropical cyclone size climatology.J Clim, 27(1): 455–476

[24]

Knapp K R, Kruk M C, Levinson D H, Diamond H J, Neumann C J (2010). The International Best Track Archive for Climate Stewardship (IBTrACS): unifying tropical cyclone best track data.Bull Am Meteorol Soc, 91(3): 363–376

[25]

Kossin J P (2017). Hurricane intensification along United States coast suppressed during active hurricane periods.Nature, 541(7637): 390–393

[26]

Landsea C W, Franklin J L (2013). Atlantic hurricane database uncertainty and presentation of a new database format.Mon Weather Rev, 141(10): 3576–3592

[27]

Landsea C W, Pielke Jr R A, Mestas-Nunez A M, Knaff J A (1999). Atlantic basin hurricanes: indices of climatic changes.Climatic Change, 42(1): 89–129

[28]

Landsea C W, Vecchi G A, Bengtsson L, Knutson T R (2010). Impact of duration thresholds on Atlantic tropical cyclone counts.J Clim, 23(10): 2508–2519

[29]

Lin Y, Zhao M, Zhang M (2015). Tropical cyclone rainfall area controlled by relative sea surface temperature.Nat Commun, 6(1): 6591

[30]

Martinez-Sanchez J N, Cavazos T (2014). Eastern Tropical Pacific hurricane variability and landfalls on Mexican coasts.Clim Res, 58(3): 221–234

[31]

McDonald J H (2014). Handbook of Biological Statistics (3rd ed.). Baltimore: Sparky House Publishing

[32]

Mei W, Xie S P, Primeau F, McWilliams J C, Pasquero C (2015). Northwestern Pacific typhoon intensity controlled by changes in ocean temperatures.Sci Adv, 1(4): e1500014

[33]

Merrill R T (1984). A comparison of large and small tropical cyclones.Mon Weather Rev, 112(7): 1408–1418

[34]

Nekkali Y S, Osuri K K, Das A K (2022). Numerical modeling of tropical cyclone size over the Bay of Bengal: influence of microphysical processes and horizontal resolution.Meteorol Atmos Phys, 134(4): 72

[35]

Rotunno R, Emanuel K A (1987). An air–sea interaction theory for tropical cyclones. Part II: evolutionary study using a nonhydrostatic axisymmetric numerical model.J Atmos Sci, 44(3): 542–561

[36]

Shen W (2006). Does the size of hurricane eye matter with its intensity?.Geophys Res Lett, 33(18): L18813

[37]

Shou H R, Li T, Sun Y, Wang L, Liu J (2021). Decreasing trend of western North Pacific tropical cyclone inner-core size over the past decades.J Meteorol Res, 35(4): 635–645

[38]

Stern D P, Vigh J L, Nolan D S, Zhang F (2015). Revisiting the relationship between eyewall contraction and intensification.J Atmos Sci, 72(4): 1283–1306

[39]

Takagi H, Wu W (2016). Maximum wind radius estimated by the 50 kt radius: improvement of storm surge forecasting over the western North Pacific.Nat Hazards Earth Syst Sci, 16(3): 705–717

[40]

Wang B, Yang Y, Ding Q H, Murakami H, Huang F (2010). Climate control of the global tropical storm days (1965–2008).Geophys Res Let, 37: L07704

[41]

Webster P J, Holland G J, Curry J A, Chang H R (2005). Changes in tropical cyclone number, duration, and intensity in a warming environment.Science, 309(5742): 1844–1846

[42]

Xu J, Wang Y (2010a). Sensitivity of the simulated tropical cyclone inner-core size to the initial vortex size.Mon Weather Rev, 138(11): 4135–4157

[43]

Xu J, Wang Y (2010b). Sensitivity of tropical cyclone inner-core size and intensity to the radial distribution of surface entropy flux.J Atmos Sci, 67(6): 1831–1852

[44]

Xu J, Wang Y, Tan Z M (2016). The relationship between sea surface temperature and maximum intensification rate of tropical cyclones in the North Atlantic.J Atmos Sci, 73(12): 4979–4988

RIGHTS & PERMISSIONS

Higher Education Press

AI Summary AI Mindmap
PDF (10283KB)

538

Accesses

0

Citation

Detail

Sections
Recommended

AI思维导图

/