Abstract
The mechanism for the maintenance of Tropical Cyclone Bill (1988) after landfall is investigated through a numerical simulation. The role of the large-scale environmental flow is examined using a scale separation technique, which isolates the tropical cyclone from the environmental flow. The results show that Bill was embedded in a deep easterly-southeasterly environmental flow to the north-northeast of a large-scale depression and to the southwest of the western Pacific subtropical high. The depression had a quasibarotropic structure in the mid-lower troposphere and propagated northwestward with a speed similar to the northwestward movement of Bill.
The moisture budgets associated with both the large-scale and the tropical cyclone scale motions indicate that persistent low-level easterly-southeasterly flow transported moisture into the inner core of the tropical cyclone. The low-level circulation of the tropical cyclone transported moisture into the eyewall to support eyewall convection, providing sufficient latent heating to counteract energy loss due to surface friction and causing the storm to weaken relatively slowly after landfall.
Warming and a westward extension of the upper-level easterly flow led to westward propagation of the environmental flow in the mid-lower troposphere. As a result, Bill was persistently embedded in an environment of deep easterly flow with high humidity, weak vertical wind shear, convergence in the lower troposphere, and divergence in the upper troposphere. These conditions are favorable for both significant intensification prior to landfall and maintenance of the tropical cyclone after landfall.
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References
Betts, A. K., and M. J. Miller, 1993: The Betts-Miller scheme. The Representation of Cumulus Convection in Numerical Models of the Atmosphere. Meteor. Monogr., 46, 107–121.
Blackadar, A. K., 1979: High resolution of the planetary boundary layer. Adv. Environ. Sci. Eng., Pfafflin J., and E. Ziegler, Eds., Gordon and Breach Science Publishers, 50–85.
Braun, S. A., 2006: High-resolution simulation of Hurricane Bonnie (1998). Part II: Water budget. J. Atmos. Sci., 63, 43–64.
Bui, H. H., R. K. Smith, M. T. Montgomery, et al., 2009: Balanced and unbalanced aspects of tropical cyclone intensification. Quart. J. Roy. Meteor. Soc., 135, 1715–1731.
Chen Lianshou, Xu Xiangde, Luo Zhexian, et al., 2005: Introduction to Tropical Cyclone Dynamics. China Meteorological Press, Beijing, 300 pp. (in Chinese)
Clark, A. J., C. J. Schaffer, W. A. Gallus, et al., 2009: Climatology of storm reports relative to upper-level jet streaks. Wea. Forecasting, 24, 1032–1051.
Davis, C., W. Wang, S. Chen, et al., 2008: Prediction of landfalling hurricanes with the advanced hurricane WRF model. Mon. Wea. Rev., 136, 1990–2005.
DeMaria, M., 2009: A simplified dynamical system for tropical cyclone intensity prediction. Mon. Wea. Rev., 137, 68–82.
—, J. A. Knaff, and B. H. Conell, 2001: A tropical cyclone genesis parameter for the tropical Atlantic. Wea. Forecasting, 16, 219–233.
Doswell, C. A., 1977: Obtaining meteorologically significant surface divergence fields through the filtering property of objective analysis. Mon. Wea. Rev., 105, 885–892.
Dudhia, J., 1993: A nonhydrostatic version of the Penn State-NCAR mesoscale model: Validation tests and simulation of an Atlantic cyclone and cold front. Mon. Wea. Rev., 121, 1493–1515.
Elsberry, R. L., 2005: Achievement of USWRP hurricane landfall research goal. Bull. Amer. Meteor. Soc., 86, 643–645.
Emanuel, K. A., 1986: An air-sea interaction theory for tropical cyclones. Part I: Steady-state maintenance. J. Atmos. Sci., 43, 585–604.
—, 1987: The dependence of hurricane intensity on climate. Nature, 326, 483–485.
—, 2003: Tropical cyclones. Ann. Rev. Earth Planet. Sci., 31, 75–104.
—, C. DesAutels, C. Holloway, et al., 2004: Environmental control of tropical cyclone intensity. J. Atmos. Sci., 61, 843–858.
Gray, W. M., 1968: Global view of the origin of tropical disturbances and storms. Mon. Wea. Rev., 96, 669–700.
Grell, G. A., J. Dudhia, and D. R. Stauffer, 1995: A description of the Fifth-generation Penn State/NCAR Mesoscale Model (MM5). NCAR/TN-398+STR. National Center for Atmospheric Research, Boulder, CO, 107 pp.
Holland, G. J., 1997: The maximum potential intensity of tropical cyclone. J. Atmos. Sci., 54, 2519–2541.
Hoskins, B. J., M. E. McIntyre, and A. W. Robertson, 1985: On the use and significance of isentropic potential vorticity maps. Quart. J. Roy. Meteor. Soc., 111, 877–946.
JTWC, 1988: Annual tropical cyclone report. http://www.usno.navy.mil/nooc/nmfc/nmfc~ph/rss/jtwc/atcr/1988atcr/pdf/1988~complete.pdf, 61–64.
Kaplan, J., and M. DeMaria, 1995: A simple empirical model for predicting the decay of tropical cyclone winds after landfall. J. Appl. Meteor., 34, 2499–2512.
—, and —, 2003: Large-scale characteristics of rapidly intensifying tropical cyclones in the North Atlantic basin. Wea. Forecasting, 18, 1093–1108.
Kurihara, Y., 1975: Budget analysis of a tropical cyclone simulated in an axisymmetric numerical model. J. Atmos. Sci., 32, 25–59.
Liu, Y. B., D. L. Zhang, and M. K. Yau, 1997: A multiscale numerical study of Hurricane Andrew (1992). Part I: Explicit simulation and verification. Mon. Wea. Rev., 125, 3073–3093.
Maddox, R. A., 1980: An objective technique for separating macroscale and mesoscale features in meteorological data. Mon. Wea. Rev., 108, 1108–1121.
Marks, F. D., and L. K. Shay, 1998: Landfalling tropical cyclones: Forecasting problem and associated research opportunities. Bull. Amer. Meteor. Soc., 79, 305–323.
Molinari, J., and D. Vollaro, 1989: External influences on hurricane intensity. Part I: Outflow layer eddy angular momentum fluxes. J. Atmos. Sci., 46, 1093–1105.
Montgomery, M. T., and R. J. Kallenbach, 1997: A theory for vortex Rossby-waves and its application to spiral bands and intensity changes in hurricanes. Quart. J. Roy. Meteor. Soc., 123, 435–465.
—, R. K. Smith, and S. V. Nguyen, 2010: Sensitivity of tropical-cyclone models to the surface drag coefficient. Quart. J. Roy. Meteor. Soc., 136, 1945–1953.
—, and —, 2011: Paradigms for tropical-cyclone intensification. Quart. J. Roy. Meteor. Soc., 137, 1–31.
Nolan, D. S., Y. Moon, and D. P. Stern, 2007: Tropical cyclone intensification from asymmetric convection: Energetics and efficiency. J. Atmos. Sci., 64, 3377–3405.
Pyle, M. E., D. Keyser, and L. F. Bosart, 2004: A diagnostic study of jet streaks: Kinematic signatures and relationship to coherent tropopause disturbances. Mon. Wea. Rev., 132, 297–319.
Ramsay, H. A., and L. M. Leslie, 2008: The effects of complex terrain on severe landfalling tropical cyclone Larry (2006) over Northeast Australia. Mon. Wea. Rev., 136, 4334–4354.
Rappaport, E. N., J. L. Grankin, A. B. Schumacher, et al., 2010: Tropical cyclone intensity change before U.S. coast landfall. Wea. Forecasting, 25, 1380–1396.
Schmidlin, T. W., 2006: On evacuation and deaths from Hurricane Katrina. Bull. Amer. Meteor. Soc., 87, 754–756.
Weinkle, J., R. Maue, and R. Pielke, 2012: Historical global tropical cyclone landfalls. J. Climate, 25, 4729–4735.
Xu Yamei, 2007: The numerical study of landfalling Typhoon Bill (1988): Inner core structures and budgets of energy and moisture. Acta Meteor. Sinica, 65(6), 877–887. (in Chinese)
—, 2011: The genesis of tropical cyclone Bilis (2000) associated with cross-equatorial surges. Adv. Atmos. Sci., 28, 665–681.
Yang, M.-J., S. A. Braun, and D.-S. Chen, 2011: Water budget of Typhoon Nari (2001). Mon. Wea. Rev., 139, 3809–3828.
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Supported by the National Natural Science Foundation of China (40675026) and National (Key) Basic Research and Development (973) Program of China (2009CB421504).
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Xu, Y. Maintenance of Tropical Cyclone Bill (1988) after landfall. Acta Meteorol Sin 27, 486–501 (2013). https://doi.org/10.1007/s13351-013-0412-4
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DOI: https://doi.org/10.1007/s13351-013-0412-4