Abstract
Tropical cyclogenesis and rapid weakening are subjects of considerable interest in the literature. This paper addresses the genesis and rapid weakening of a North Indian Ocean tropical cyclone Lehar (November 23–28, 2013). High-resolution analysis has been created by assimilating GPSRO observations using WRF and 3DVAR assimilation techniques. The parent disturbance of tropical cyclone Lehar is traced back using a moisture variable, and it is found to be originating from a westward-moving disturbance. The pathway of genesis is found to be bottom-up, with the vorticity developing from below. Tropical cyclone Lehar weakened from a Category 1 cyclone on November 26, 2013. We analyzed the prospects that contributed to the abrupt drop of tropical cyclone Lehar’s intensity in view of this. The analysis shows dust in the post-genesis (rapid weakening) environment of tropical cyclone Lehar. The analysis of total precipitable water in the post-genesis environment shows that the environment is very dry (< 45 kgm−2), and the spiral bands started disappearing under the influence of dry air intrusion. It has been found that the tropical cyclone Lehar is interacting with the dry air coming from the northern part of the Indian region during the post-genesis (rapid weakening) evolution, and the cyclone started weakening rapidly. The dry air advection from the north of the storm is a primary contributor to the weakening and high deep layer shear in the weakening environment.
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Code availability
Mesoscale model viz. Weather Research and Forecasting Model used in this research work is available from https://www.mmm.ucar.edu/weather-research-and-forecasting-model
Availability of data and material
Global Forecast System model (GFS) dataset used for initialization is available from ftp://nomads.ncdc.noaa.gov/GFS/analysis_only/. GPSRO observations are taken from the Research Data Archive (RDA, http:// rda.ucar.edu). Tropical Cyclone Heat Potential (TCHP) data have been obtained from the Bhuvan data archive (http://bhuvan.nrsc.gov.in/data/download).
References
Anthes RA, Rocken C, Kuo Y-H (2000) Applications of COSMIC to meteorology and climate. Terrestr Atmos Ocean Sci 11:115–156
Anthes RA, Ector D, Hunt DC, Kuo YH, Rocken C, Schreiner WS, Sokolovskiy SV, Syndergaard S, Wee TK, Zeng Z et al (2008) The COSMIC/FORMOSAT-3 mission: early results. Bull Am Meteor Soc 89:313–333
Barker DM, Huang W, Guo Y-R, Bourgeois AJ, Xiao QN (2004) A three-dimensional variational data assimilation system for MM5: implementation and initial results. Mon Weather Rev 132:897–914
Curtis L (2004) Midlevel dry intrusions as a factor in tornado outbreaks associated with landfalling tropical cyclones from the Atlantic and Gulf of Mexico. Weather Forecast 19:411–427
DeMott PJ, Sassen K, Poellot MR et al (2003) African dust aerosols as atmospheric ice nuclei: African dust aerosols as ice nuclei. Geophys Res Lett. https://doi.org/10.1029/2003GL017410
Draxler RR, Hess GD (1998) An overview of the HYSPLIT\_4 modelling system for trajectories. Aust Meteorol Mag 47:295–308
Dunion JP, Velden CS (2004) The Impact of the Saharan Air Layer on Atlantic tropical cyclone activity. Bull Amer Meteor Soc 85:353–366. https://doi.org/10.1175/BAMS-85-3-353
Dunkerton TJ, Montgomery MT, Wang Z (2009) Tropical cyclogenesis in a tropical wave critical layer: easterly waves. Atmos Chem Phys 9(15):5587–5646
Frederick WJ (2003) The rapid intensification and subsequent rapid weakening of Hurricane Lili as compared with historical hurricanes. Weather Forecast 18:1295–1298
Fridlind AM (2004) Evidence for the predominance of mid-tropospheric aerosols as subtropical anvil cloud nuclei. Science 304:718–722. https://doi.org/10.1126/science.1094947
Gallina GM, Velden CS (2002) 3C. 5 Environmental vertical wind shear and tropical cyclone intensity change utilizing enhanced satellite derived wind information. Atlantic 58:12
Hanley D, Molinari J, Keyser D (2001) A composite study of the interactions between tropical cyclones and upper-tropospheric troughs. Mon Weather Rev 129:2570–2584
Ho S-P, Kuo Y-H, Zeng Z, Peterson TC (2007) A comparison of lower stratosphere temperature from microwave measurements with CHAMP GPS RO data: microwave measurements with champ gps ro data. Geophys Res Lett. https://doi.org/10.1029/2007GL030202
Kimball SK (2006) A modeling study of hurricane landfall in a dry environment. Mon Weather Rev 134:1901–1918
Jayakrishnan KU, Kutty G, George B (2020) On the predictability and dynamics of tropical cyclone: Nargis (2008). J Geophys Res Atmos. https://doi.org/10.1029/2019JD032040
Kutty G, Gohil K (2017) The role of mid-level vortex in the intensification and weakening of tropical cyclones. J Earth Syst Sci 126:94. https://doi.org/10.1007/s12040-017-0879-y
Léon J-F, Legrand M (2003) Mineral dust sources in the surroundings of the north Indian Ocean: satellite remote sensing of mineral dust. Geophys Res Lett. https://doi.org/10.1029/2002GL016690
Montgomery MT, Lussier LL III, Moore RW, Wang Z (2010) The genesis of Typhoon Nuri as observed during the Tropical Cyclone Structure 2008 (TCS-08) field experiment—Part 1: the role of the easterly wave critical layer. Atmos Chem Phys 10:9879–9900. https://doi.org/10.5194/acp-10-9879-2010
Palmer CK, Barnes GM (2002) The effect of vertical wind shear as diagnosed by the NCEP/NCAR reanalysis data on northeast Pacific hurricane intensity. In: Preprints, 25th Conf. on Hurricanes and Tropical Meteorology. Amer. Meteor. Soc., San Diego, CA
Pasch RJ, Lawrence MB, Avila LA, Beven JL, Franklin JL, Stewart SR (2004) Atlantic hurricane season of 2002. Mon Weather Rev 132:1829–1859
Paterson LA, Hanstrum BN, Davidson NE, Weber HC (2005) Influence of environmental vertical wind shear on the intensity of hurricane-strength tropical cyclones in the Australian region. Mon Weather Rev 133:3644–3660
Rajasree VPM, Kesarkar AP, Bhate JN, Singh V, Umakanth U, Varma TH (2016a) A comparative study on the genesis of North Indian Ocean tropical cyclone Madi (2013) and Atlantic Ocean tropical cyclone Florence (2006): genesis of Madi (NIO) and Florence (AO). J Geophys Res Atmos 121:13826–13858. https://doi.org/10.1002/2016JD025412
Rajasree VPM, Kesarkar AP, Bhate JN, Umakanth U, Singh V, Harish Varma T (2016b) Appraisal of recent theories to understand cyclogenesis pathways of tropical cyclone Madi (2013): genesis of tropical cyclone MADI. J Geophys Res Atmos 121:8949–8982. https://doi.org/10.1002/2016JD025188
Rajasree VPM, Routray A, George JP et al (2021) Study of cyclogenesis of developing and non-developing tropical systems of NIO using NCUM forecasting system. Meteorol Atmos Phys 133:379–397. https://doi.org/10.1007/s00703-020-00756-z
Sharma R, Mohapatra M (2017) Rapid weakening of very severe cyclonic storm “Lehar”–A case study. Tropical cyclone activity over the North Indian Ocean. Springer, Cham, pp 131–147
Skamarock WC, Klemp JB, Dudhia J et al (2019) A description of the advanced research WRF model version 4. Natl Cent Atmos Res Boulder, CO, USA, p 145
Sreekanth V, Kulkarni P (2013) Spatio-temporal variations in columnar aerosol optical properties over Bay of Bengal: signatures of elevated dust. Atmos Environ 69:249–257. https://doi.org/10.1016/j.atmosenv.2012.12.031
Wang Z, Dunkerton TJ, Montgomery MT (2012) Application of the marsupial paradigm to tropical cyclone formation from northwestward-propagating disturbances. Mon Weather Rev 140:66–76. https://doi.org/10.1175/2011MWR3604.1
Wang Z, Montgomery MT, Dunkerton TJ (2009) A dynamically-based method for forecasting tropical cyclogenesis location in the Atlantic sector using global model products: tropical cyclogenesis forecast. Geophysical Research Letters. https://doi.org/10.1029/2008GL035586
Wang Z, Montgomery MT, Dunkerton TJ (2010a) Genesis of Pre-Hurricane Felix (2007). Part I: the role of the easterly wave critical layer. J Atmos Sci 67:1711–1729. https://doi.org/10.1175/2009JAS3420.1
Wang Z, Montgomery MT, Dunkerton TJ (2010b) Genesis of Pre-Hurricane Felix (2007). Part II: warm core formation, precipitation evolution, and predictability. J Atmos Sci 67:1730–1744. https://doi.org/10.1175/2010JAS3435.1
Wood KM, Ritchie EA (2015) A definition for rapid weakening of North Atlantic and eastern North Pacific tropical cyclones: rapid weakening of tropical cyclones. Geophys Res Lett 42:10091–10097. https://doi.org/10.1002/2015GL066697
Wong S (2005) Suppression of deep convection over the tropical North Atlantic by the Saharan Air Layer. Geophys Res Lett 32:L09808. https://doi.org/10.1029/2004GL022295
Yunck T, Hajj G, Kursinski E, LaBrecque J, Lowe S, Watkins M, McCormick C (2000) AMORE: an autonomous constellation concept for atmospheric and ocean observation. Acta Astronaut 46:355–364
Zehr RM (1992) Tropical cyclogenesis in the western North Pacific
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We thank Dr. Amit Kumar Patra, Director, National Atmospheric Research Laboratory, for supporting this research work. We gratefully acknowledge the use of the computational facility at NARL.
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VPMR contributed to conceptualization, simulations, methodology, visualization. JB contributed to assimilation methodology, simulation, initial writing, visualization. AK contributed to conceptualization, writing draft correction, modification, visualization. VS contributed to methodology, visualization.
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Rajasree, V.P.M., Bhate, J.N., Kesarkar, A.P. et al. Genesis and rapid weakening of tropical cyclone Lehar (2013). Nat Hazards 109, 371–388 (2021). https://doi.org/10.1007/s11069-021-04840-4
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DOI: https://doi.org/10.1007/s11069-021-04840-4