Abstract
In several regions of the world, tropical cyclones have been known to maintain or increase strength after landfall without transitioning to extratropical systems. It is hypothesized that these inland areas help sustain tropical cyclones when there has been plentiful rainfall, leading to unusually wet soil and strong latent heat release. Additionally, given the symmetric structure of warm-core cyclones, the atmosphere should tend toward barotropic conditions that mimic an ocean environment. Observational and modeling studies support this “brown ocean” concept, providing a global climatology of inland tropical cyclones, pinpointing regions that are more favorable for re-intensification, and analyzing individual cyclones to better understand the associated land-atmosphere feedbacks.
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References
Andersen T, Shepherd JM (2013) A global spatio-temporal analysis of inland tropical cyclone maintenance or intensification. Int J Climatol 34:391–402. doi:10.1002/joc.3693
Andersen T, Radcliffe D, Shepherd JM (2013) Quantifying surface energy fluxes in the vicinity of inland-tracking tropical cyclones. J Appl Meteorol Climatol 52:2797–2808. doi:10.1175/JAMC-D-13-035
Arndt DS, Basara JB, McPherson RA et al (2009) Observations of the overland reintensification of tropical storm Erin, 2007. Bull Am Meteorol Soc 90:1079–1093. doi:10.1175/2009BAMS2644.1
Au-Yeung AYM, Chan JCL (2010) The effect of a river delta and coastal roughness variation on a landfalling tropical cyclone. J Geophys Res Atmos 115:D19121. doi:10.1029/2009JD013631
Bender MA, Knutson TR, Tuleya RE et al (2010) Modeled impact of anthropogenic warming on the frequency of intense Atlantic hurricanes. Science 327:454–458. doi:10.1126/science.1180568
Bosilovich MG, Sun WY (1999) Numerical simulation of the 1993 midwestern flood: land atmosphere interactions. J Climate 12:1490–1505. doi:10.1175/1520-0442(1999)012<1490:NSOTMF>2.0.CO;2
Bozeman ML, Niyogi D, Gopalakrishnan S et al (2012) An HWRF-based ensemble assessment of the land surface feedback on the post-landfall intensification of tropical storm Fay (2008). Nat Hazards 63:1543–1571. doi:10.1007/s11069-011-9841-5
Chang H, Niyogi D, Kumar A et al (2009) Possible relation between land surface feedback and the post-landfall structure of monsoon depressions. Geophys Res Let 36:1–6. doi:10.1029/2009GL037781
Chen LS (2012) Research progress on the structure and intensity change for the landfalling tropical cyclones. J Trop Meteor 18:113–118. doi:10.3969/j.issn.10068775.2012.02.001
Chen F, Dudhia J (2001) Coupling an advanced land-surface/hydrology model with the Penn State–NCAR MM5 modeling system. Part I: model description and implementation. Mon Weather Rev 129:569–585. doi:10.1175/1520-0493(2001)129<0569:CAALSH>2.0.CO;2
Chen SH, Sun WY (2002) A one-dimensional time dependent cloud model. J Meteorol Soc Jpn 80:99–118. doi:10.2151/jmsj.80.99
Clark CA, Arritt RW (1995) Numerical simulations of the effect of soil moisture and vegetation cover on the development of deep convection. J Appl Meteorol 34:2029–2045. doi:10.1175/1520-0450(1995)034<2029:NSOTEO>2.0.CO;2
Deshpande MS, Pattnaik S, Salvekar PS (2012) Impact of cloud parameterization on the numerical simulation of a super cyclone. Ann Geophys 30:775–795. doi:10.5194/angeo-30-775-2012
Dong M, Chen L, Li Y et al (2010) Rainfall reinforcement associated with landfalling tropical cyclones. J Atmos Sci 67:3541–3558. doi:10.1175/2010JAS3268.1
Dudhia J (1989) Numerical study of convection observed during the winter monsoon experiment using a mesoscale two-dimensional model. J Atmos Sci 46:3077–3107. doi:10.1175/1520-0469(1989)046<3077:NSOCOD>2.0.CO;2
Emanuel K, Callaghan J, Otto P (2008) A hypothesis for the redevelopment of warm-core cyclones over northern Australia. Mon Weather Rev 136:3863–3872. doi:10.1175/2008MWR2409.1
Evans C, Schumacher RS, Galarneau TJ (2011) Sensitivity in the overland reintensification of tropical cyclone Erin (2007) to near-surface soil moisture characteristics. Mon Weather Rev 139:3848–3870. doi:10.1175/2011MWR3593.1
Frank W (1977) The structure and energetics of the tropical cyclone II. Dynamics and energetics. Mon Weather Rev 105:1136–1150. doi:10.1175/15200493(1977)105<1136:TSAEOT>2.0.CO;2
Gao S, Chiu LS (2010) Surface latent heat flux and rainfall associated with rapidly intensifying tropical cyclones over the western North Pacific. Int J Remote Sens 31:4699–4710. doi:10.1080/01431161.2010.485149
Guimond SR, Bourassa MA, Reasor PD (2011) A latent heat retrieval and its effects on the intensity and structure change of hurricane Guillermo (1997). Part I: the algorithm and observations. J Atmos Sci 68:1549–1567. doi:10.1175/2011JAS3700.1
Hart RE, Evans JL (2001) A climatology of the extratropical transition of Atlantic tropical cyclones. J Climate 14:546–564. doi:10.1175/1520-0442(2001)014<0546:ACOTET>2.0.CO;2
Hill KA, Lackmann GM (2011) The impact of future climate change on TC intensity and structure: a downscaling approach. J Climate 24:4644–4661. doi:10.1175/2011JCLI3761.1
Hong SY, Noh Y, Dudhia J (2006) A new vertical diffusion package with an explicit treatment of entrainment processes. Mon Weather Rev 134:318–2341. doi:10.1175/MWR3199.1
Kain JS, Fritsch JM (1990) A one-dimensional entraining/detraining plume model and its application in convective parameterization. J Atmos Sci 47:2784–2802. doi:10.1175/1520-0469(1990)047<2784:AODEPM>2.0.CO;2
Kantha L (2010) Discussion of “A hydrodynamics-based surge scale for hurricanes”. Ocean Eng 37:1081–1084. doi:10.1016/j.oceaneng.2010.04.003
Kellner O, Niyogi D, Lei M et al (2012) The role of anomalous soil moisture on the inland reintensification of tropical storm Erin (2007). Nat Hazards 139:1573–1600. doi:10.1007/s11069-011-9966-6
Kishtawal CM, Niyogi D, Kumar A et al (2012) Sensitivity of inland decay of North Atlantic tropical cyclones to soil parameters. Nat Hazards 63:1527–1542. doi:10.1007/s11069-011-0015-2
Klein P, Harr P, Elsberry R (2000) Extratropical transition of western North Pacific tropical cyclones: an overview and conceptual model of the transformation stage. Weather Forecast 15:373–395. doi:10.1175/1520-0434(2000)015<0373:ETOWNP>2.0.CO;2
Knapp KR, Kruk MC, Levinson DH et al (2010) The International Best Track Archive for Climate Stewardship (IBTrACS): unifying tropical cyclone best track data. Bull Am Meteorol Soc 91:363–376. doi:10.1175/2009BAMS2755.1
Kossin JP, Emanuel KA, Vecchi GA (2014) The poleward migration of the location of tropical cyclone maximum intensity. Nature 509:349–352. doi:10.1038/nature13278
Lee SW, Lee DK, Chang DE (2011) Impact of horizontal resolution and cumulus parameterization scheme on the simulation of heavy rainfall events over the Korean Peninsula. Adv Atmos Sci 28:1–15. doi:10.1007/s00376-010-9217-x
Lin N, Smith JA, Villarini G et al (2010) Modeling extreme rainfall, winds, and surge from hurricane Isabel (2003). Weather Forecast 25:1342–1361. doi:10.1175/2010WAF2222349.1
Liu J, Curry JA, Clayson CA et al (2011) High-resolution satellite surface latent heat fluxes in North Atlantic hurricanes. Mon Weather Rev 139:2735–2747. doi:10.1175/2011MWR3548.1
Lynn BH, Tao WK, Wetzel PJ (1998) A study of landscape-generated deep moist convection. Mon Weather Rev 126:928–942. doi:10.1175/1520-0493(1998)126<0928:ASOLGD>2.0.CO;2
Ma LM, Tan ZM (2009) Improving the behavior of the cumulus parameterization for tropical cyclone prediction: convection trigger. Atmos Res 92:190–211. doi:10.1016/j.atmosres.2008.09.022
Mlawer EJ, Taubman SJ, Brown PD et al (1997) Radiative transfer for inhomogeneous atmospheres: RRTM, a validated correlated-k model for the longwave. J Geophys Res Atmos 102:16663–16682. doi:10.1029/97JD00237
Murakami H, Wang Y, Yoshimura H et al (2012) Future changes in tropical cyclone activity projected by the new high-resolution MRI-AGCM. J Climate 25:3237–3260. doi:10.1175/JCLI-D-11-00415.1
National Centers for Environmental Prediction/National Weather Service/NOAA/U.S. Department of Commerce (2000, updated daily) NCEP FNL operational model global tropospheric analyses, continuing from July 1999. Research Data Archive at the National Center for Atmospheric Research, Computational and Information Systems Laboratory. doi:10.5065/D6M043C6
Prater BE, Evans JL (2002) Sensitivity of modeled tropical cyclone track and structure of hurricane Irene (1999) to the convective parameterization scheme. Meteorol Atmos Phys 80:103–115. doi:10.1007/s007030200018
Radcliffe DE, Šimůnek J (2010) Soil physics with HYDRUS: modeling and applications. CRC Press, Boca Raton, p 373
Rakhecha P, Singh VP (2009) Applied hydrometeorology, 1st edn. Springer-Verlag, New York, p 364, LLC
Rappaport EN (2014) Fatalities in the United States from Atlantic tropical cyclones: new data and interpretation. Bull Am Meteorol Soc 95:341–346. doi:10.1175/BAMS-D-12-00074.1
Senkbeil JC, Sheridan SC (2006) A post landfall hurricane classification system for the United States. J Coast Res 22:1025–1034. doi:10.2112/05-0532.1
Shen W, Ginis I, Tuleya R (2002) A numerical investigation of land surface water on landfalling hurricanes. J Atmos Sci 59:789–802. doi:10.1175/1520-0469(2002)059<0789:ANIOLS>2.0.CO;2
Shepherd JM (2012) What we can learn from the satellite-based rainfall footprint of superstorm Sandy: a preliminary synopsis. In: Earthzine. http://www.earthzine.org/2012/12/16/what-we-can-learn-from-the-satellite-based-rainfall-footprint-of-superstorm-sandy-a-preliminary-synopsis/. Accessed 16 Dec 2012
Shepherd JM, Knutson T (2007) The current debate on the linkage between global warming and hurricanes. Geog Compass 1:1–24. doi:10.1111/j.1749-8198.2006.00002.x
Shepherd JM, Grundstein A, Mote TL (2007) Quantifying the contribution of tropical cyclones to extreme rainfall along the coastal southeastern United States. Geophys Res Lett 34:1–5. doi:10.1029/2007GL031694
Skamarock WC, Klemp JB, Dudhia J et al (2008) A description of the advanced research WRF version 3. NCAR Tech. Note NCAR/TN-4751STR, p 125
Trenberth KE, Fasullo J (2007) Water and energy budgets and hurricanes and implications for climate change. J Geophys Res 112:1–10. doi:10.1029/2006JD008304
Tuleya RE (1994) Tropical storm development and decay: sensitivity to surface boundary conditions. Mon Weather Rev 122:291–304. doi:10.1175/1520-0493(1994)122<0291:TSDADS>2.0.CO;2
Tuleya RE, Kurihara Y (1978) A numerical simulation of the landfall of tropical cyclones. J Atmos Sci 35:242–257
Wang JF, Bras RL, Eltahir EAB (2000) The impact of observed deforestation on the mesoscale distribution of rainfall and clouds in Amazonia. J Hydrometeorol 1:267–286. doi:10.1175/1525-7541(2000)001<0267:TIOODO>2.0.CO;2
Xie BG, Zhang FQ (2012) Impacts of typhoon track and island topography on the heavy rainfalls in Taiwan associated with Morakot (2009). Mon Weather Rev 140:3379–3394. doi:10.1175/MWR-D-11-00240.1
Zhang YC, Rossow WB (1997) Estimating meridional energy transports by the atmospheric and oceanic general circulations using boundary fluxes. J Climate 10:2358–2373. doi:10.1175/1520-0442(1997)010<2358:EMETBT>2.0.CO;2
Zhang Y, Cassardo C, Ye CA et al (2011) The role of the land surface processes in the rainfall generated by a landfall typhoon: a simulation of the typhoon Sepat (2007). Asia-Pacific J Atmos Sci 47:63–77. doi:10.1007/s13143-011-1006-7
Zhu P (2008) Impact of land-surface roughness on surface winds during hurricane landfall. Q J R Meteor Soc 134:1051–1057. doi:10.1002/qj.265
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Andersen, T., Shepherd, M. (2017). Inland Tropical Cyclones and the “Brown Ocean” Concept. In: Collins, J., Walsh, K. (eds) Hurricanes and Climate Change. Springer, Cham. https://doi.org/10.1007/978-3-319-47594-3_5
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