ch.20 notes mc neely 2010
TRANSCRIPT
Ch. 20: Weather Patterns & Severe Storms
Earth-Space Science
Bremen High School
Teacher: Aaron McNeely
Arizona monsoon storm from Kitt Peak
Observatory
Air Masses
An air mass is an immense body of air that has similar temperatures and humidity throughout
Homogenous Produce “air mass weather”, similar
conditions for a few days of time
Classifying Air Masses
The area over which an air mass gets its characteristic temperature and humidity is called its source region
Air masses are named according to their source region and temperature
Source Regions
Polar (P) air masses form at high latitudes toward earth’s poles
Tropical (T) air masses form at low latitudes closer to earth’s equator
Maritime and Continental
Surfaces: Land or water Continental (c) air masses form over
land Maritime (m) air masses form over
water
Air Masses
Polar (P)
(cold)
Tropical (T)
(warm)
Continental (c)
(land)
cP
(land, cold)
cT
(land, warm)
Maritime (m)
(water)
mP
(water, cold)
mT
(water, warm)
North American Air Masses
Air masses are classified by the region over which they form Nor’easters
SW monsoonsIndian Summer
Lake Effect Snow
When cP air masses move over warmer lake water (Great Lakes), the air mass draws heat and moisture from the lake and precipitates it as lake effect snow on the leeward shores
Leeward cities such as Rochester and Buffalo, New York are among the snowiest in the country
Great Lakes Lake Effect
•NASA Satellite view (12-5-00) of lake effect snow over Michigan and Northern Indiana
•Where is Bremen?
http://antwrp.gsfc.nasa.gov/apod/ap041130.html
SW Monsoons
The monsoons occur in Southern California, Arizona, and New Mexico during midsummer
mT air masses moving inland from over the ocean bring warm, moist air with storms and occasional heavy precipitation
Despite being a desert, monsoons make Arizona one of the lightning capitals of the United States (Florida is the top lightning capital)
Arizona Monsoon
http://www.solarhaven.org/MONSOON.htm
Indian Summer
cT air masses form in the SW United States and Mexico during summer
In the fall, cT air masses can create the Indian Summer, a short period of warm weather within the cooler autumn
FrontsSec 20.2
When two air masses meet, they form a front
A front is a boundary that separates two air masses of differing temperatures and amounts of moisture
Types of Fronts
Types of fronts Warm Cold Stationary Occluded
Warm Fronts
A warm front forms when warm air moves into an area formerly covered by cooler air
(all front symbols) http://members.aol.com/pakulda/images/
Warm Front
Cold Fronts
A cold front forms when cold, dense air moves into a region occupied by warmer air
Cold Front
Stationary Fronts
Occasionally, the flow of air on either side of a front is parallel to the front
In such cases, the surface position of the front does not move, and a stationary front forms
Occluded Front
When an active cold front overtakes a warm front, an occluded front forms
The occluded front forms when an advancing cold front wedges beneath a warm front and pushes it upward
Occluded FrontsA cold front moves toward a warm front, forcing warm air aloft
A cold front merges with the warm front to form an occluded front that drops heavy rain
Because occluded fronts can move slowly, light precipitation falls for many days
Middle-Latitude Cyclones
Middle-latitude cyclones are the main weather producing systems for the United States
Low pressure West to east
L
Cyclonic System (Low Pressure)
Note the warm, cold, and occluded fronts
Satellite View of a Cyclone
Note the counter-clockwise spiral over the continental US
ThunderstormsSec 20.3
Thunderstorms produce lightning and thunder, and frequently gusty winds, heavy rain, and hail
Cumulonimbus clouds, fronts
Occurrence of Thunderstorms
The US experiences about 100,000 thunderstorms per year mostly in the Gulf of Mexico area and Florida
Any part of the US experiences 30-100 thunderstorms per year
Development of Thunderstorms
Three stages of development:
1. Cumulus stage Strong updrafts of moist, warm air
2. Mature stage Heavy precipitation, most active stage
3. Dissipating stage Down moving air dominates, storm dies
Stages of Thunderstorm Development
Time
Tornadoes
Violent rotating windstorms Column of rotating air called a vortex The vortex extends downward from a
cumulonimbus cloud Single or multiple vortices
Occurrence of Tornadoes
United States, tornado capital About 770 tornadoes occur each year
in the US Most occur between April and June Most tornadoes form in association
with severe thunderstorms
1925 Tri-State Tornado
The deadliest tornado in US history occurred on March 18, 1925
The Tri-State or Great Tornado killed 695 people as it raced across parts of Missouri, Illinois, and Indiana
http://www.geocities.com/Heartland/7847/tornado2.htm
The Great Tornado
Hurricanes
Hurricanes are the most violent storms on earth
Generally form in the tropics Whirling tropical cyclones that produce
winds 75 mph
Hurricane Damage
Destructive waves up to 45 feet high Flooding Heavy winds Storm surges, a dome of water 40-50
miles wide that sweeps over land 50% of the US population lives within
50 miles of a coast
Cross-Section of an Hurricane
Hurricane Names
World Meteorological Association, annual list of names
Names originally all short, female; Male names were introduced in 1978
Names are given when a disturbance becomes a tropical storm (winds 38-74 mph)
2008 Hurricane Names
ArthurBertha
CristobalDolly*
EdouardFay
Gustav*
HannaIke*
JosephineKyle
LauraMarcoNana
* US landfall, major hurr’
OmarPalomaReneSally
TeddyVicky
Wilfred
2009 Hurricane Names
AnaBill
ClaudetteDannyErikaFred
Grace
HenriIda
JoaquinKateLarryMindy
Nicholas
OdettePeterRoseSam
TeresaVictor
Wanda
http://www.nhc.noaa.gov/aboutnames.shtml
Hurricane Katrina
Deadliest hurricane in US history 1,836 deaths $81.2 billion in damage, the costliest
natural disaster in US history Katrina flooded 80% of New Orleans,
devastated other cities such as Biloxi MS and Mobile AL
Katrina—August 28, 2005
New Orleans freeway submerged
Katrina NASA satellite view
http://www.katrinahelp.com/hurricane-katrina-pictures.html