Tropical Cyclone Motion Tropical Cyclone Motion Climatology Figure

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Tropical Cyclone Motion

Tropical Cyclone Motion

Tropical Cyclone Motion Climatology (Figure obtained from Global Perspectives on Tropical Cyclones, Ch. 4,

Tropical Cyclone Motion Climatology (Figure obtained from Global Perspectives on Tropical Cyclones, Ch. 4, © 1995 WMO. )

Tropical Cyclone Motion Climatology (Figure obtained from Global Perspectives on Tropical Cyclones, Ch. 4,

Tropical Cyclone Motion Climatology (Figure obtained from Global Perspectives on Tropical Cyclones, Ch. 4, © 1995 WMO. )

Tropical Cyclone Motion Climatology (Figure obtained from Global Perspectives on Tropical Cyclones, Ch. 4,

Tropical Cyclone Motion Climatology (Figure obtained from Global Perspectives on Tropical Cyclones, Ch. 4, © 1995 WMO. )

Tropical Cyclone Motion Climatology (Figure obtained from Global Perspectives on Tropical Cyclones, Ch. 4,

Tropical Cyclone Motion Climatology (Figure obtained from Global Perspectives on Tropical Cyclones, Ch. 4, © 1995 WMO. )

Motion by Steering Flow (Figure obtained from Chan (2005). © 2005, Annual Reviews. )

Motion by Steering Flow (Figure obtained from Chan (2005). © 2005, Annual Reviews. )

Steering Flow: Layer Determination (Figure obtained from http: //tropic. ssec. wisc. edu/misc/dlm 3. gif.

Steering Flow: Layer Determination (Figure obtained from http: //tropic. ssec. wisc. edu/misc/dlm 3. gif. )

Steering Flow: 850 -700 h. Pa Example (Figure obtained from http: //tropic. ssec. wisc.

Steering Flow: 850 -700 h. Pa Example (Figure obtained from http: //tropic. ssec. wisc. edu/. )

Steering Flow: 700 -200 h. Pa Example (Figure obtained from http: //tropic. ssec. wisc.

Steering Flow: 700 -200 h. Pa Example (Figure obtained from http: //tropic. ssec. wisc. edu/. )

Beta Effect t=0 h t = 36 h t = 72 h LINEAR NON-LINEAR

Beta Effect t=0 h t = 36 h t = 72 h LINEAR NON-LINEAR (Figure obtained from Chan (2005). © 2005, Annual Reviews. )

Beta Effect (Figure obtained from Chan (2005). © 2005, Annual Reviews. )

Beta Effect (Figure obtained from Chan (2005). © 2005, Annual Reviews. )

Non-Uniform Horizontal Flow N zonal wind Case 1: Linear Horizontal Shear, No Flow Over

Non-Uniform Horizontal Flow N zonal wind Case 1: Linear Horizontal Shear, No Flow Over TC Center

Non-Uniform Horizontal Flow N zonal wind Case 2: Non-Linear Horizontal Shear, Flow Over TC

Non-Uniform Horizontal Flow N zonal wind Case 2: Non-Linear Horizontal Shear, Flow Over TC Center

Non-Uniform Horizontal Flow Horizontal tilt of vortex strengthens anticyclonic beta gyre to NE but

Non-Uniform Horizontal Flow Horizontal tilt of vortex strengthens anticyclonic beta gyre to NE but weakens cyclonic beta gyre to SW N zonal wind Case 1, Except With Beta Gyres

Non-Uniform Horizontal Flow Horizontal tilt of vortex weakens anticyclonic beta gyre N zonal wind

Non-Uniform Horizontal Flow Horizontal tilt of vortex weakens anticyclonic beta gyre N zonal wind Case 2, Except With Beta Gyres

Vertical Wind Shear Effect on Motion (Figure obtained from Chan (2005). © 2005, Annual

Vertical Wind Shear Effect on Motion (Figure obtained from Chan (2005). © 2005, Annual Reviews. )

Fujiwhara Rotation earth-relative center of mass-relative (Figure obtained from Chan (2005). © 2005, Annual

Fujiwhara Rotation earth-relative center of mass-relative (Figure obtained from Chan (2005). © 2005, Annual Reviews. )

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