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Annual Review of Earth and Planetary Sciences, 2003
Tropical cyclones encompass virtually every subdiscipline of geophysical fluid dynamics, including cumulus convection, boundary layers, thermodynamic cycles, surface wave dynamics, upper ocean wind-driven circulations, barotropic instability, Rossby waves, and air-sea interaction.
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Tropical cyclones encompass virtually every subdiscipline of geophysical fluid dynamics, including cumulus convection, boundary layers, thermodynamic cycles, surface wave dynamics, upper ocean wind-driven circulations, barotropic instability, Rossby waves, and air-sea interaction.
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1991
Abstract : This paper discusses the question of tropical cyclone propagation or why the average tropical cyclone moves 1-2 m/s faster and usually 10-20 deg to the left of its surrounding (or 5-7 deg radius) deep layer (850-300 mb) steering current. It is shown that the primary factor causing tropical cyclones to propagate faster and to the left of ...
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Abstract : This paper discusses the question of tropical cyclone propagation or why the average tropical cyclone moves 1-2 m/s faster and usually 10-20 deg to the left of its surrounding (or 5-7 deg radius) deep layer (850-300 mb) steering current. It is shown that the primary factor causing tropical cyclones to propagate faster and to the left of ...
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1996
Abstract Tropical cyclones are among the most destructive weather systems (1-3). The impact from cyclones generally extends over a wide area, with mortality, injury, and property loss that result from strong winds and heavy rains. Often secondary events such as storm surges, flooding, landslides, and tornadoes exacerbate effects of ...
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Abstract Tropical cyclones are among the most destructive weather systems (1-3). The impact from cyclones generally extends over a wide area, with mortality, injury, and property loss that result from strong winds and heavy rains. Often secondary events such as storm surges, flooding, landslides, and tornadoes exacerbate effects of ...
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Abstract Tropical cyclones are the largest, and most destructive, vortices that can form on the surface of the earth. This chapter reviews the conditions under which they form, as well as the observational evidence as to their structure.
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Tropical Cyclone Forecasters Reference Guide 6. Tropical Cyclone Intensity.
1995Puacc reoonmg burdsn lof this colieaion o( inlonnaiion >s asInnaiAO to av«rag« i tiour par response, inciuaing ine time lor reviewing tisirucnons. searcmng eiisiing aai* sources, gatnenng «na mamtaiturig ttie data rw«3eO. »nd coiTctoting«rKJ reviewrigthe co«oaiori o( iriloriTutiori.
J-H. Chu +3 more
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Tropical Cyclone Intensity Change
1999Abstract : LONG-TERM GOALS. My long-term goal is to better determine the relationship between observed environmental wind shear and TC intensity change in order to improve prediction. OBJECTIVES. The primary objectives are to better understand the relationship between vertical shear and TC intensity using observations, and develop methods to ...
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TROPICAL CYCLONES AND HURRICANES | Tropical Cyclones
2015C.-C. Wu, Y.-H. Huang
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