Skip to main content

Advertisement

Log in

Large scale features and energetics of the hybrid subtropical low ‘Duck’ over the Tasman Sea

  • Published:
Climate Dynamics Aims and scope Submit manuscript

Abstract

New aspects of the genesis and partial tropical transition of a rare hybrid subtropical cyclone on the eastern Australian coast are presented. The ‘Duck’ (March 2001) attracted more recent attention due to its underlying genesis mechanisms being remarkably similar to the first South Atlantic hurricane (March 2004). Here we put this cyclone in climate perspective, showing that it belongs to a class within the 1 % lowest frequency percentile in the Southern Hemisphere as a function of its thermal evolution. A large scale analysis reveals a combined influence from an existing tropical cyclone and a persistent mid-latitude block. A Lagrangian tracer showed that the upper level air parcels arriving at the cyclone’s center had been modified by the blocking. Lorenz energetics is used to identify connections with both tropical and extratropical processes, and reveal how these create the large scale environment conducive to the development of the vortex. The results reveal that the blocking exerted the most important influence, with a strong peak in barotropic generation of kinetic energy over a large area traversed by the air parcels just before genesis. A secondary peak also coincided with the first time the cyclone developed an upper level warm core, but with insufficient amplitude to allow for a full tropical transition. The applications of this technique are numerous and promising, particularly on the use of global climate models to infer changes in environmental parameters associated with severe storms.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8

Similar content being viewed by others

References

  • Allan JT, Pezza AB, Black MT (2010) Explosive cyclogenesis: a global climatology comparing multiple reanalysis. J Clim 23:6468–6484. doi:10.1175/2010JCLI3437.1

    Article  Google Scholar 

  • Barras V, Simmonds I (2009) Observation and modelling of stable water isotopes as diagnostics of rainfall dynamics over southeastern Australia. J Geophys Res 114:D23308. doi:10.1029/2009JD012132

    Article  Google Scholar 

  • Bluestein HB (1993) Synoptic-dynamic meteorology in midlatitudes, vol 2. Oxford University Press, New York, p 594

    Google Scholar 

  • Cordeira JM, Bosart L (2010) The antecedent large-scale conditions of the ‘perfect storms’ of late October and early November 1991. Mon Weather Rev 138:2546–2569

    Article  Google Scholar 

  • Covey C, Dai A, Marsh D, Lindzen RS (2011) The surface-pressure signature of atmospheric tides in modern climate models. J Atmos Sci 68:495–514. doi:10.1175/2010jas3560.1

    Article  Google Scholar 

  • Dal Piva E, Gan MA, Rao VB (2010) Energetics of winter troughs entering South America. Mon Weather Rev 138:1084–1103

    Article  Google Scholar 

  • Davis CA (2010) Simulations of subtropical cyclones in a baroclinic channel model. J Atmos Sci 67:2871–2892

    Article  Google Scholar 

  • Decker SG, Martin JE (2005) A local energetic analysis of the life cycle differences between consecutive, explosive deepening, continental cyclones. Mon Weather Rev 133:295–316

    Article  Google Scholar 

  • Dee DP, Uppala SM, Simmons AJ, Berrisford P, Poli P, Kobayashi S, Andrae U, Balmaseda MA, Balsamo G, Bauer P, Bechtold P, Beljaars ACM, van de Berg L, Bidlot J, Bormann N, Delsol C, Dragani R, Fuentes M, Geer AJ, Haimberger L, Healy SB, Hersbach H, Hólm EV, Isaksen L, Kållberg P, Köhler M, Matricardi M, McNally AP, Monge-Sanz BM, Morcrette J–J, Park B-K, Peubey C, de Rosnay P, Tavolato C, Thépaut J-N, Vitart F (2011) The ERA-Interim reanalysis: configuration and performance of the data assimilation system. Q J R Meteorol Soc 137:553–597. doi:10.1002/qj.828

    Article  Google Scholar 

  • Dvorak VF (1984) Tropical cyclone intensity analysis using satellite data. NOAA Tech Rep NESDIS 11:45

    Google Scholar 

  • Evans JL, Guishard MP (2009) Atlantic subtropical storms. Part I: diagnostic criteria and composite analysis. Mon Weather Rev 137:2065–2080. doi:10.1175/2009MWR2468.1

    Article  Google Scholar 

  • Favre A, Hewitson B, Tadross M, Lennard C, Cerezo-Mota R (2012) Relationships between cut-off lows and the semiannual and Southern Oscillations. Clim Dyn 38:1473–1487

    Article  Google Scholar 

  • Garde LA, Pezza AB, Bye JAT (2010) Tropical transition of the 2001 Australian Duck. Mon Weather Rev 138:2038–2057

    Article  Google Scholar 

  • Gutierrez ER, Silva Dias PL, Veiga JA, Camayo R, dos Santos A (2009) Multivariate analysis of the energy cycle of the South American rainy season. Int J Climatol 29:2256–2269

    Article  Google Scholar 

  • Harr PA, Dea J (2009) Downstream development associated with the extratropical transition of tropical cyclones over the western north Pacific. Mon Weather Rev 137:1295–1319

    Article  Google Scholar 

  • Hart RE (2003) A cyclone phase space derived from thermal wind and thermal asymmetry. Mon Weather Rev 131:585–616

    Article  Google Scholar 

  • Holland GJ, Lynch AH, Leslie LM (1987) Australian east coast cyclones. Part I: synoptic overview and case study. Mon Weather Rev 115:3024–3036

    Article  Google Scholar 

  • Lim E-P, Simmonds I (2002) Explosive cyclone development in the Southern Hemisphere and a comparison with Northern Hemisphere events. Mon Weather Rev 130:2188–2209

    Article  Google Scholar 

  • Lim E-P, Simmonds I (2007) Southern Hemisphere winter extratropical cyclone characteristics and vertical organization observed with the ERA-40 reanalysis data in 1979–2001. J Clim 20:2675–2690

    Article  Google Scholar 

  • Lorenz EN (1967) The nature and theory of the general circulation of the atmosphere. World Meteorological Organization, Geneva, p 161

    Google Scholar 

  • Lovenduski NS, Gruber N (2005) Impact of the southern annular mode on southern ocean circulation and biology. Geophys Res Lett 32:L11603. doi:10.1029/2005GL022727

    Article  Google Scholar 

  • Marquet P (2003) The available-enthalpy cycle. II: applications to idealized baroclinic waves. Q J R Meteorol Soc 129:2467–2494

    Article  Google Scholar 

  • Montgomery MT, Van Sang N, Smith RK, Persing J (2009) Do tropical cyclones intensify by WISHE? Q J R Meteorol Soc 135:1697–1714

    Article  Google Scholar 

  • Pezza AB, Simmonds I (2005) The first South Atlantic hurricane: unprecedented blocking, low shear and climate change. Geophys Res Lett 32:L15712. doi:10.1029/2005GL023390

    Article  Google Scholar 

  • Pezza AB, Veiga JAP, Simmonds I, Keay K, Mesquita MDS (2010) Environmental energetics of an exceptional high-latitude storm. Atmos Sci Lett 11:39–45

    Article  Google Scholar 

  • Qi L, Leslie LM, Speer MS (2006) Climatology of cyclones over the southwest Pacific: 1992–2001. Meteorol Atmos Phys 91:201–209

    Article  Google Scholar 

  • Rasmussen EA, Turner J (2003) Polar lows. Mesoscale weather systems in the polar regions. Cambridge University Press, Cambridge, p 612

    Book  Google Scholar 

  • Reale O, Atlas R (2001) Tropical cyclone–like vortices in the extratropics: observational evidence and synoptic analysis. Weather Forecast 16:7–34

    Article  Google Scholar 

  • Simmonds I (2000) Size changes over the life of sea level cyclones in the NCEP reanalysis. Mon Weather Rev 128:4118–4125

    Article  Google Scholar 

  • Simmonds I, Keay K, Lim E-P (2003) Synoptic activity in the seas around Antarctica. Mon Weather Rev 131:272–288

    Article  Google Scholar 

  • Ulbrich U, Leckebusch GC, Pinto JG (2009) Extra-tropical cyclones in the present and future climate: a review. Theor Appl Climatol 96:117–131

    Article  Google Scholar 

  • Veiga JAP, Pezza AB, Simmonds I, Silva Dias PL (2008) An analysis of the environmental energetics associated with the transition of the first South Atlantic hurricane. Geophys Res Lett 35:L15806. doi:10.1029/2008GL034511

    Article  Google Scholar 

  • Wahab MA, Basset HA, Lasheen AM (2002) On the mechanism of winter cyclogenesis in relation to vertical axis tilt. Meteorol Atmos Phys 81:103–127

    Article  Google Scholar 

Download references

Acknowledgments

We would like to thank Kevin Keay (The Centre for Australian Weather and Climate Research, Australian Bureau of Meteorology) for technical guidance with the use of the Lagrangian Advective Tracking Scheme and Noel Davidson (The Centre for Australian Weather and Climate Research, Australian Bureau of Meteorology) for input and discussions during an earlier stage of this work. ABP would like to thank the Australian Research Council for funding parts of this work.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Alexandre Bernardes Pezza.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Pezza, A.B., Garde, L.A., Veiga, J.A.P. et al. Large scale features and energetics of the hybrid subtropical low ‘Duck’ over the Tasman Sea. Clim Dyn 42, 453–466 (2014). https://doi.org/10.1007/s00382-013-1688-x

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00382-013-1688-x

Keywords

Navigation