Download presentation
Presentation is loading. Please wait.
1
Rossby Waves
5
Tropopause variation with latitude
6
Jet stream – wind field and temperatures
7
Isotachs and isotherms
8
Mid-latitude Cyclones Formation revisited
9
Polar front
10
Upper atmosphere pressure and winds
13
Current circulation model
14
Tropical Climate
15
Monsoon
16
Asian monsoon - 1 Winter (northern hemisphere) Cold air over Asia creates high pressure. Dry air drawn southwards from Himalaya
17
Asian monsoon - 2 Summer (northern hemisphere) Land heats to give low pressure over Asia. Moist air drawn northwards from equatorial oceans
19
Hurricane Mitch
20
Distribution of Hurricanes
21
Hurricane Damage Scale Number Category Central Pressure mb inches Wind Speeds mi/hr knots Storm Surge feet meters Observed Damage 1>=980 >=28.94 74-95 64-82 4-5 ~1.5 some damage to trees, shrubbery, and unanchored mobile homes 2965-979 28.50-28.91 96-110 83-95 6-8 ~2.0-2.5 major damage to mobile homes; damage buildings' roofs, and blow trees down 3945-964 27.91-28.47 111-130 96-113 9-12 ~2.5-4.0 destroy mobile homes; blow down large trees; damage small buildings 4920-944 27.17-27.88 131-155 114-135 13-18 ~4.0-5.5 completely destroy mobile homes; lower floors of structures near shore are susceptible to flooding 5<"920" <"27.17" >"155" >"135" >"18" >"5.5" extensive damage to homes and industrial buildings; blow away small buildings; lower floors of structures within 500 meters of shore and less than 4.5 m (15 ft) above sea level are damaged
22
Hurricane Eye Wall
23
Cross-section of hurricane
24
Spin up process Air converges from radius of order 1000 km Air that is stationary w.r.t. the earth is travelling eastwards w.r.t. a frame of reference fixed in space at a speed Hence air drawn from N travels more slowly and that from S faster than the centre of the hurricane, leading to rotation. convergence rising air, condensation release of latent heat surface low pressure R θ Ω relative to space Conserving angular momentum about eye mvr is constant so: relative to earth
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.