Download presentation
Presentation is loading. Please wait.
1
Severe Weather
2
Air masses are classified on the basis of their source region
3
Air masses and weather Continental polar (cP)
From northern Canada and interior of Alaska Winter – brings cold, dry air Summer – brings cool relief Responsible for lake-effect snows cP air mass crosses the Great Lakes Air picks up moisture from the lakes Snow occurs on the leeward shores of the lakes
4
Air masses and weather Maritime tropical (mT)
From the Gulf of Mexico and the Atlantic Ocean Warm, moist, unstable air Brings precipitation to the eastern United States
5
Air masses and weather Continental tropical (cT) Southwest and Mexico
Hot, dry Seldom important outside the source region
6
Air masses and weather Maritime polar (mP)
Brings precipitation to the western mountains Occasional influence in the northeastern United States causes the "Northeaster" in New England with its cold temperatures and snow
7
Fronts Types of fronts Warm front Warm air replaces cooler air
Shown on a map by a line with semicircles Small slope (1:200) Clouds become lower as the front nears Slow rate of advance Light-to-moderate precipitation
8
Warm Front / High pressure system
Cold Front / Low pressure system Rain!
9
Fronts Types of fronts Cold front Cold air replaces warm air
Shown on a map by a line with triangles Twice as steep (1:100) as warm fronts Advances faster than a warm front Associated weather is more violent than a warm front Weather behind the front is dominated by Cold air mass Subsiding air Clearing conditions
10
Warm Front / High pressure system
Cold Front / Low pressure system Warm Front / High pressure system Rain/Snow Thunderstorms
11
Fronts Types of fronts Stationary front Occluded front
Flow of air on both sides of the front is almost parallel to the line of the front Surface position of the front does not move Occluded front Active cold front overtakes a warm front Cold air wedges the warm air upward Weather is often complex Precipitation is associated with warm air being forced aloft
12
Middle-latitude cyclone
Primary weather producer in the middle-latitudes
13
Middle-latitude cyclone
Idealized weather Middle-latitude cyclones move eastward across the United States First signs of their approach are in the western sky Require two to four days to pass over a region Largest weather contrasts occur in the spring
14
Cloud patterns typically associated with a mature middle-latitude cyclone
15
Stages in the development of a thunderstorm
16
Severe weather types Tornadoes
A rapidly spinning column of air descending from a large thunderstorm Have the highest wind speeds of any other weather phenomenon. In the U.S., tornadoes move northeast at speeds up to 100 km/hr (62 mph) Rotating wind speeds sometimes in excess of 500 km/hr (310 mph)
17
Severe weather types Tornadoes How a Tornado Forms
Moist air from Gulf of Mexico Fast moving cold, dry air mass from Canada Jet stream moving east at 150 mph Sets up shearing conditions
18
Severe weather types Tornadoes How a Tornado Forms
Warm moist Gulf air releases latent heat, creates strong updraft Updraft sheared by polar air, then twisted in a different direction by jet stream
19
Severe weather types Tornadoes
Why do some thunderstorms spawn tornadoes while others do not? Super Cell Thunderstorms
20
Severe weather types Tornadoes Scales
The Fujita-Pearson Scale measures wind speed The size of a tornado is not necessarily an indication of its intensity Large tornadoes can be weak, and small tornadoes can be violent
22
Severe weather types Hurricanes
Only natural disaster that is given a human name Actually large tropical cyclones Convert heat in the ocean into winds Exports excess heat from the tropics to the midlatitudes
23
Severe weather types Hurricanes How a Hurricane Works
Tropical disturbance Low pressure zone develops and draws in clusters of thunderstorms and winds
24
Severe weather types Hurricanes How a Hurricane Works
Tropical disturbance Tropical depression Surface winds strengthen, move about the center of the storm Central core funnels warm moist air up towards stratosphere Air cools, vapor condenses, latent heat released Fuels more updrafts, cycle repeats, storm grows
25
Severe weather types Hurricanes How a Hurricane Works
Tropical disturbance Tropical depression Tropical Storm Storm has sustained surface wind speeds of +39 mph
26
Severe weather types Hurricanes How a Hurricane Works
Tropical disturbance Tropical depression Tropical Storm Hurricane Surface winds consistently over 74 mph
27
Severe weather types Hurricanes How a Hurricane Works
Tropical disturbance Tropical depression Tropical Storm Hurricane The Eye As wind speed increases, winds are spiraled upwards prior to reaching the center A distinctive clear “eye” is formed Strongest winds are located on the walls of the eye
29
Hurricane Origins Form in the tropics ~ 5° and 20 ° latitude
Cannot form at the equator (Coriolis effect = 0)
30
Hurricanes Hurricane Damages Storm Surges
Large mound of water builds up beneath the eye Reaches land as a surge of water
31
Hurricanes Hurricane Damages Storm Surges
Wind speed varies depending upon which side of the hurricane you’re on Amount of damage on the coastline will vary accordingly
32
Hurricanes Hurricane Damages Heavy Rains
Mudflows and Debris Avalanches Flooding
33
~ End ~
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.