參考文獻 |
Bender, M. A., I. Ginis, and Y. Kurihara, 1993: Numerical simulations of tropical cyclone-ocean interaction with a high‐resolution coupled model. J. Geophys. Res., 98(D12), 23, 245–23, 263, https://doi.org/10.1029/93JD02370.
, and I. Ginis, 2000: Real‐case simulations of hurricane–ocean interaction using a high-resolution coupled model: Effects on hurricane intensity. Mon. Wea. Rev., 128, 917–946, https://doi.org/10.1175/1520-0493(2000)128%3C0917:RCSOHO%3E2.0.CO;2.
Chan, J. C. L., R. T. Williams, 1987: Analytical and Numerical Studies of the Beta-Effect in Tropical Cyclone Motion. Part I: Zero Mean Flow. J. Atmos. Sci., 44, 1257-1265, https://doi.org/10.1175/1520-0469(1987)044%3C1257:AANSOT%3E2.0.CO;2
, F. M. Ko, and Y. M. Lei, 2002: Relationship between potential vorticity tendency and tropical cyclone motion. J. Atmos. Sci., 59, 1317–1336, https://doi.org/10.1175/1520-0469(2002)059%3C1317:RBPVTA%3E2.0.CO;2
Chandrasekar, R., C. Balaji, 2012: Sensitivity of tropical cyclone Jal simulations to physics parameterizations. J. Earth Syst. Sci., 121, 923–946, https://doi.org/10.1007/s12040-012-0212-8
Chang, Y.-T., I-I Lin, H.-C. Huang, Y.-C. Liao and C.-C. Lien, 2019: The association of typhoon intensity increase with translation speed increase in the South China Sea. Sustainability. 12, 939, https://doi.org/10.3390/su12030939
Chang, S. W., and R. V. Madala, 1980: Numerical simulation of the influence of sea surface temperature on translating tropical cyclones. J. Atmos. Sci., 37, 2617–2630. https://doi.org/10.1175/1520-0469(1980)037%3C2617:NSOTIO%3E2.0.CO;2
Charney, J. G., and A. Eliassen, 1964: On the Growth of the Hurricane Depression. J. Atmos. Sci., 21, 68–75,
https://doi.org/10.1175/1520-0469(1964)021%3C0068:OTGOTH%3E2.0.CO;2.
Chen, H., and D.-L. Zhang, 2013: On the rapid intensification of Hurricane Wilma (2005). Part II: Convective bursts and the upper-level warm core. J. Atmos. Sci., 70, 146–162, https://doi.org/10.1175/JAS-D-12-062.1.
Chen, X. M., M. Xue, J. Fang, 2018: Rapid Intensification of Typhoon Mujigae (2015) under different sea surface temperatures structural changes leading to rapid intensification. J. Atmos. Sci., 75, 4313–4335, https://doi.org/10.1175/JAS-D-18-0017.1.
Choi, Y., K. S. Yun, K. J. Ha, K. Y. Kim, S. J. Yoon, and J. C. Chan, 2013: Effects of asymmetric SST distribution on straight-moving Typhoon Ewiniar (2006) and recurving Typhoon Maemi (2003). Mon. Wea. Rev., 141, 3950–3967,
https://doi.org/10.1175/MWR-D-12-00207.1
Cione, J. J., 2015: The relative roles of the ocean and atmosphere as revealed by buoy air sea observations in hurricanes. Mon. Wea. Rev., 143, 904–913,
https://doi.org/10.1175/MWR-D-13-00380.1.
Črnivec, N., R. K. Smith, and G. Kilroy, 2016: Dependence of tropical cyclone intensification rate on sea-surface temperature. Quart. J. Roy. Meteor. Soc., 142, 1618 1627, https://doi.org/10.1002/qj.2752.
Emanuel, K. A., 1986: An air‐sea interaction theory for tropical cyclones. Part I: Steady state maintenance. J. Atmos. Sci., 43, 585–605,
https://doi.org/10.1175/1520-0469(1986)043%3C0585:AASITF%3E2.0.CO;2.
Frank, W. M., E. A. Ritchie, 2001: Effects of vertical wind shear on the intensity and structure of numerically simulated hurricanes. Mon. Wea. Rev., 129, 2249–2269.
Gray, W. M., 1968: Global view of the origin of tropical disturbances and storms. Mon. Wea. Rev., 96, 669–700, https://doi.org/10.1175/1520-0493(1968)096%3C0669:GVOTOO%3E2.0.CO;2.
Holland, G. J., 1997: The maximum potential intensity of tropical cyclones. J. Atmos. Sci., 54, 2519–2541,
https://doi.org/10.1175/1520-0469(1997)054%3C2519:TMPIOT%3E2.0.CO;2.
Huang, C.-Y., T.-C. Juan, H.-C. Kuo and J.-H. Chen, 2020: Track deflection of Typhoon Maria (2018) during a westbound passage offshore of northern Taiwan: Topographic influence. Mon. Wea. Rev. (2020) 148 (11): 4519–4544, https://doi.org/10.1175/MWR-D-20-0117.1.
Huang, C. Y., C. A. Chen, S. H. Chen, and D. S. Nolan, 2016: On the upstream track deflection of tropical cyclones past a mountain range: Idealized experiments. J. Atmos. Sci., 73, 3157–3180, https://doi.org/10.1175/JAS-D-15-0218.1
Hsu, L. H., S. H. Su, R. G. Fovell, and H. C. Kuo, 2018: On typhoon track deflections near the east coast of Taiwan. Mon. Wea. Rev., 146(5), 1495–1510, https://doi.org/10.1175/MWR-D-17-0208.1
Kanase, R. D., and P. S. Salvekar, 2015: Impact of physical parameterization schemes on track and intensity of severe cyclonic storms in Bay of Bengal. Meteorol. Atmos. Phys., 127, 537–559, https://doi.org/10.1007/s00703-015-0381-5
Kaplan, J., and M. DeMaria, 2003: Large‐scale characteristics of rapidly intensifying tropical cyclones in the North Atlantic basin. Wea. Forecasting, 18, 1093–1108, https://doi.org/10.1175/1520-0434(2003)018%3C1093:LCORIT%3E2.0.CO;2.
, M. DeMaria, J. A. Knaff, 2010: A revised tropical cyclone rapid intensification index for the Atlantic and eastern North Pacific basins. Wea. Forecasting, 25, 220–241, https://doi.org/10.1175/2009WAF2222280.1.
Katsube, K., and M. Inatsu, 2016: Response of tropical cyclone tracks to sea surface temperature in the western North Pacific. J. Climate, 29, 1955–1975, https://doi.org/10.1175/JCLI-D-15-0198.1
Knaff, J. A., M. DeMaria, C. R. Sampson, J. E. Peak, J. Cummings, and W. H. Schubert, 2013: Upper oceanic energy response to tropical cyclone passage. J. Climate, 26, 2631–2650, https://doi.org/10.1175/JCLI-D-12-00038.1.
Lee, C. Y., and S. S. Chen, 2012: Symmetric and asymmetric structures of hurricane boundary layer in coupled atmosphere–wave–ocean models and observations. J. Atmos. Sci., 69, 3576–3594, https://doi.org/10.1175/JAS-D-12-046.1.
Li, D.-Y., and C.-Y. Huang 2018: The influences of orography and ocean on track of Typhoon Megi (2016) past Taiwan as identified by HWRF. Journal of Geophysical Research: Atmospheres, 123, 11, 492–11,517, https://doi.org/10.1029/2018JD029379
Lin, I.-I., C.-C. Wu, K. A. Emanuel, I.-H. Lee, C.-R. Wu and I.-F. Pun, 2005: The interaction of supertyphoon Maemi (2003) with a warm ocean eddy. Mon. Wea. Rev., 133, 2635–2649, https://doi.org/10.1175/MWR3005.1.
, C.-C. Wu, I.-F. Pun and D.-S. Ko, 2008: Upper‐ocean thermal structure and the western North Pacific category 5 typhoons. Part I: Ocean features and the category 5 typhoons′ intensification. Mon. Wea. Rev., 136, 3288–3306,
https://doi.org/10.1175/2008MWR2277.1.
Lin, Y. L., S. Y. Chen, C. M. Hill, and C. Y. Huang 2005: Control parameters for track continuity and deflection associated with tropical cyclones over a mesoscale mountain. Journal of the Atmospheric Sciences, 62, 1849–1866.
https://doi.org/10.1175/JAS3439.1
Mandal, M., U. C. Mohanty, P. Sinha, and M. M. Ali, 2007: Impact of sea surface temperature in modulating movement and intensity of tropical cyclones. Natural Hazards., 41, 413–427, https://www.researchgate.net/deref/http%3A%2F%2Fdx.doi.org%2F10.1007%2Fs11069-006-9051-8.
Mandal, M., U. C. Mohanty, and S. Raman, 2004: A Study on the Impact of Parameterization of Physical Processes on Prediction of Tropical Cyclones over the Bay of Bengal with NCAR/PSU Mesoscale Model. Natural Hazards., 31, 391–414, https://www.researchgate.net/deref/http%3A%2F%2Fdx.doi.org%2F10.1023%2FB%3ANHAZ.0000023359.24526.24
Mei, W., C.-C. Lie, I.-I. Lin, and S.-P. Xie, 2015: Tropical cyclone induced ocean response: A comparative study of the South China Sea and tropical Northwest Pacific. J. Climate, 28, 5952–5968, https://doi.org/10.1175/JCLI-D-14-00651.1.
, and C. Pasquero, 2013: Spatial and temporal characterization of sea surface temperature response to tropical cyclones. J. Climate, 26, 3745–3765,
https://doi.org/10.1175/JCLI-D-12-00125.1.
Merrill, R. T., 1988: Environmental influences on hurricane intensification. J. Atmos. Sci., 45, 1678–1687,
https://doi.org/10.1175/1520-0469(1988)045%3C1678:EIOHI%3E2.0.CO;2
Molinari, J., P. Dodge, D. Vollaro, K. L. Corbosiero, and F. Marks, Jr., 2006: Mesoscale aspects of the downshear reformation of a tropical cyclone. J. Atmos. Sci., 63, 341–354, https://doi.org/10.1175/JAS3591.1.
, and D. Vollaro, 2010: Rapid intensification of a sheared tropical storm. Mon. Wea. Rev., 138, 3869–3885, https://doi.org/10.1175/2010MWR3378.1.
Nasrollahi, N., A. Aghakouchak, J. Li, X. Gao, K. Hsu, S. Sorooshian, 2012: Assessing the impacts of different WRF precipitation physics in hurricane simulations. Weather Forecast., 27, 1003–1016, https://doi.org/10.1175/WAF-D-10-05000.1
Oey, L. Y., T. Ezer, D. P. Wang, S. J. Fan, and X. Q. Yin, 2006: Loop current warming by Hurricane Wilma. Geophys. Res. Lett., 33, L08613,
https://doi.org/10.1029/2006GL025873.
Raju, P. V. S., J. Potty, and U. C. Mohanty, 2011: Sensitivity of physical parameterizations on prediction of tropical cyclone Nargis over the Bay of Bengal using WRF model. Meteorol. Atmos. Phys., 113, 125–137, https://doi.org/10.1007/s00703-011-0151-y
Reasor, P. D., M. D. Eastin, and J. F. Gamache, 2009: Rapidly intensifying Hurricane Guillermo (1997). Part I: Low-wavenumber structure and evolution. Mon. Wea. Rev., 137, 603–631, https://doi.org/10.1175/2008MWR2487.1.
Shay, L. K., G. J. Goni, and P. G. Black, 2000: Effects of a warm oceanic feature on Hurricane Opal. Mon. Wea. Rev., 128, 1366–1383,
https://doi.org/10.1175/1520-0493(2000)128%3C1366:EOAWOF%3E2.0.CO;2.
Smith, R. K., and M. T. Montgomery, 2015: Toward Clarity on understanding tropical cyclone intensification. J. Atmos. Sci., 72, 3020– 3031, https://doi.org/10.1175/JAS-D-15-0017.1.
, J. A. Zhang, and M. T. Montgomery, 2017: The dynamics of intensification in a Hurricane Weather Research and Forecasting simulation of Hurricane Earl (2010). Quart. J. Roy. Meteor. Soc., 143, 293–308, https://doi.org/10.1002/qj.2922.
Srinivas C.V., R. Venkatesan, D. V. Bhaskar Rao, and D. Hari Prasad, 2007: Numerical simulation of Andhra severe cyclone (2003): model sensitivity to boundary layer and convection parameterization. Pure Appl Geophys, 164, 1465-1487, https://doi.org/10.1007/s00024-007-0228-1
Srinivas, C.V., D. V. Bhaskar Rao, V. Yesubabu, R. Baskaran, and B. Venkatraman, 2013: Tropical cyclone predictions over the Bay of Bengal using the high-resolution Advanced Research Weather Research and Forecasting (ARW) model. Q. J. Roy. Meteor. Soc., 139, 1810–1825, https://doi.org/10.1002/qj.2064
Stern, D. P., and D. S. Nolan, 2011: On the vertical decay rate of the maximum tangential winds in tropical cyclones. J. Atmos. Sci., 68, 2073–2094,
https://doi.org/10.1175/2011JAS3682.1.
Sun, J., and L. Y. Oey, 2015: The influence of the ocean on Typhoon Nuri (2008). Mon. Wea. Rev., 143, 4493–4513, https://doi.org/10.1175/MWR-D-15-0029.1.
Sun, J., Oey, L. Y., Chang, R., Xu, F., & Huang, S. M., 2015: Ocean response to typhoon Nuri (2008) in western Pacific and South China Sea. Ocean Dynamics, 65, 735–749, https://doi.org/10.1007/s10236-015-0823-0
Tallapragada, V., L. Bernardet, M. Biswas, I. Ginis, Y. Kwon, Q. Liu, et al., 2015: Hurricane Weather Research and Forecasting (HWRF) Model: 2015 scientific documentation. NCAR/TN-522+STR, http://dx.doi.org/10.5065/D6ZP44B5.
Tang, C. K., J. C. L. Chan, 2014: Idealized simulations of the effect of Taiwan and Philippines topographies on tropical cyclone tracks. Q. J. R. Meteorol. Soc, 140, 1578–1589, https://doi.org/10.1002/qj.2240
Trivedi, D. K., P., Mukhopadhyay, and S. S. Vaidya, 2006: Impact of physical parameterization schemes on the numerical simulation of Orissa super cyclone (1999). Mausam, 57, 97–110.
Tuleya., R. E., Y. Kurihara, 1982: A note on the sea surface temperature sensitivity of a numerical model of tropical storm genesis. Mon. Wea. Rev., 110, 2063-2069, https://doi.org/10.1175/1520-0469(1980)037%3C2617:NSOTIO%3E2.0.CO;2
Wang, Y., M. T. Montgomery, and B. Wang, 2004: How much vertical shear can a tropical cyclone resist? Bull. Amer. Meteor. Soc., 85, 661-662.
Wang, X., C. Wang, L. Zhang, and X. Wang, 2015: Multi-decadal variability of tropical cyclone rapid intensification in the Western North Pacific. J. Climate, 28, 3806–3820, https://doi.org/10.1175/JCLI-D-14-00400.1.
Wang, Y., and C.-C. Wu, 2004: Current understanding of tropical cyclone structure and intensity changes - A review. Meteorol. Atmos. Phys., 87, 257–278,
https://doi.org/10.1007/s00703-003-0055-6.
Wang, Y., M. T. Montgomery, and B. Wang, 2004: How much vertical shear can a tropical cyclone resist? Bull. Amer. Meteor. Soc., 85, 661-662.
Wu, C. C., C. Y. Lee, and I. I. Lin, 2007: The effect of the ocean eddy on tropical cyclone intensity. J. Atmos. Sci., 64, 3562–3578, https://doi.org/10.1175/JAS4051.1.
, T.-S. Huang, W.-P. Huang and K.-H. Chou, 2003: A New Look at the Binary Interaction: Potential Vorticity Diagnosis of the Unusual Southward Movement of Tropical Storm Bopha (2000) and Its Interaction with Supertyphoon Saomai (2000)., Amer. Meteor. Soc., 1289-1300,
https://doi.org/10.1175/1520-0493(2003)131%3C1289:ANLATB%3E2.0.CO;2
, T.-S. Huang and K.-H. Chou, 2004: Potential Vorticity Diagnosis of the Key Factors Affecting the Motion of Typhoon Sinlaku (2002). Mon. Wea. Rev., 132, 2084–2093, https://doi.org/10.1175/1520-0493(2004)132%3C2084:PVDOTK%3E2.0.CO;2
Wu, L., B. Wang, and S. A. Braun, 2005: Impacts of air–sea interaction on tropical cyclone track and intensity. Mon. Wea. Rev., 133, 3299–3314,
https://doi.org/10.1175/MWR3030.1
, B. Wang, 2000: A potential vorticity tendency diagnostic approach for tropical cyclone motion. Mon. Wea. Rev, 128(6), 1899-1911,
https://doi.org/10.1175/1520-0493(2000)128%3C1899:APVTDA%3E2.0.CO;2
Wu, C.-C., W.-T. Tu, I.-F. Pun, I-I. Lin, and M. S. Peng, 2016: Tropical cyclone-ocean interaction in Typhoon Megi (2010) – A synergy study based on ITOP observations and atmosphere-ocean coupled model simulations, J. Geophys. Res. Atmos., 121,153–16 7, https://doi.org/10.1002/2015JD024198
Yablonsky, R. M., I. Ginis, B. Thomas, V. Tallapragada, D. Sheinin, and L. Bernardet, 2015: Description and analysis of the ocean component of NOAA’s operational Hurricane Weather Research and Forecasting Model (HWRF). J. Atmos. Oceanic Technol., 32, 144–163, https://doi.org/10.1175/JTECH-D-14-00063.1.
Yau, M. K., Y. Liu, D.-L. Zhang, and Y. Chen, 2004: A multi-scale numerical study of Hurricane Andrew (1992). Part VI: Small-scale inner-core structures and wind streaks. Mon. Wea. Rev., 132, 1410-1433,
https://doi.org/10.1175/1520-0493(2004)132%3C1410:AMNSOH%3E2.0.CO;2
Yu, H., W. Huang, Y. H. Duan, J. C. L. Chan, P. Y. Chen, and R. L. Yu, (2007): A simulation study on pre-landfall erratic track of Typhoon Haitang (2005). Meteorol. Atmos. Phys., 97, 189–206. https://doi.org/10.1007/s00703-006-0252-1
Yun, K. S., J. C. Chan, and K. J. Ha, 2012: Effects of SST magnitude and gradient on typhoon tracks around East Asia: A case study for Typhoon Maemi (2003). Atmospheric Research, 109-110, 36–51.
https://doi.org/10.1016/j.atmosres.2012.02.012
Zhang, D. L., Y. Liu, and M. K. Yau, 2001: A multi-scale numerical study of Hurricane Andrew (1992). Part IV: Unbalanced flows. Mon. Wea. Rev., 129, 92–107,
https://doi.org/10.1175/1520-0493(2001)129%3C0092:AMNSOH%3E2.0.CO;2.
Zhao, X., and J. C. L. Chan, 2016: Changes in tropical cyclone intensity with translation speed and mixed-layer depth: Idealized WRF-ROMS coupled model simulations. Q. J. R. Meteorol. Soc., 143, 152–163. https://doi.org/10.1002/qj.2905 |