chapter 9 air masses and fronts
DESCRIPTION
CHAPTER 9 AIR MASSES AND FRONTS. Air masses. What’s an air mass? A large body of air with similar temperature and humidity characteristics Where do these air masses come from? (Source Regions) P = polar T = tropical A = Arctic m = maritime c = continental. Temperature. Moisture. - PowerPoint PPT PresentationTRANSCRIPT
CHAPTER 9
AIR MASSES AND FRONTS
CHAPTER 9
AIR MASSES AND FRONTS
What’s an air mass?◦ A large body of air with similar temperature and
humidity characteristics Where do these air masses come from?
(Source Regions) P = polar T = tropical A = Arctic m = maritime c = continental
Temperature
Moisture
cP: cold, dry, stable◦ Extreme case: cA - Cold air rushes down into
central U.S. from Canada: “arctic high”◦ Impacts:
Citrus crop damage in southeast Lake-effect snows near Great Lakes when cold air
moves over warmer water
mP: cool, moist, somewhat unstable◦ Air from Pacific is lifted by mountains on west
coast, producing rain and snow
Hot and dry, stable aloft but unstable near surface◦ Only really occurs in U.S. in summer in southwest◦ Few clouds and minimal precipitation◦ Impacts:
drought if a cT air mass remains in place for a long time
July 2005 heat wave
Warm, moist, unstable◦ Flow northward from Gulf of Mexico provides fuel
for thunderstorms in the eastern U.S.◦ Flow from Pacific into California◦ Impacts:
Severe weather in the central and eastern U.S. Flooding in California
The “Pineapple Express”
http://www.atmos.albany.edu/student/cordeira/WEB/PWAT/global_loop.html
0000 UTC 16 Aug 2007
Maritime Tropical air ahead of a tropical cyclone
96
0000 UTC 17 Aug 2007
250 hPa h (dam), 700 hPa (105 s1),precipitable water (mm)
850–500 hPa mean wind (kt)
96
0000 UTC 18 Aug 2007
250 hPa h (dam), 700 hPa (105 s1),precipitable water (mm)
850–500 hPa mean wind (kt)
96
0000 UTC 19 Aug 2007
250 hPa h (dam), 700 hPa (105 s1),precipitable water (mm)
850–500 hPa mean wind (kt)
96
1200 UTC 19 Aug 2007
250 hPa h (dam), 700 hPa (105 s1),precipitable water (mm)
850–500 hPa mean wind (kt)
96
Rainfall Totals (in)
cP
mT
mP
FrontsFronts
Warm Front
Cold Front
Stationary Front
Occluded Front
A Front - is the boundary between air masses; normallyrefers to where this interface intersects the ground (in all cases except stationary fronts, the symbols are placed pointing to the direction of movement)
Fig. 9.16, p. 252
Other BoundariesOther Boundaries
Dryline
Dryline - Separation of warm, moist air (from Gulf) and warm, dry air (from SW United States)(common over west Texas in spring/summer)
Cloud cover and surface dew point
Sharp change in temperature◦ Sometimes, though…
Sharp change in dew point
Shift in wind direction “Kink” in isobars Weather/Clouds
http://www.hpc.ncep.noaa.gov/sfc/namussfcwbg.gif
**(Amanda) Fanning is one of my former students!
Air mass change on Wednesday, 7 March 2012
“Dome” of dense cold air is replacing warm air Steep leading edge – may have strong upward
motion Clouds and precip. usually ahead of fast-moving cold
front, lagging behind if slow-moving
Field Before passage
During After
Wind S or SW Gusty, shifting
W or NW, often
strong
Temperature
Warm Sudden drop Dropping
Pressure Falling Reaches minimum, then sharp
rise
Rising
Clouds Ci, Cs, then Cb
Tcu or Cb Cu or Sc
Precip Brief showers
Heavy showers, severe
weather
Clearing
Dew Point High Drops sharply
Lowering
Fig. 9.15, p. 251
Warm air replacing cool air Relatively gentle slope – leads to broad area of
upward motion Warm fronts usually move slower than cold
fronts
Field Before passage
During After
Wind S or SE Variable S or SW
Temperature
Cool or cold Steady rise
Warming
Pressure Falling Leveling off
Slight rise, then fall
Clouds Ci, Cs, As, Ns, St, then
fog
Stratus Clearing
Precip Light rain, snow, sleet,
freezing rain**
Drizzle or none
None
Dew Point Steady rise Steady Rising, then
steady
Name is self-explanatory: doesn’t move much In some cases where air is moist on both sides,
stationary fronts can lead to flooding – rain forms along front and persists for many days
Fig. 9.9, p. 246
In 1-2 sentences, explain why there is no such thing as a “maritime Arctic” (mA) air mass.
BE SURE TO WRITE YOUR NAME ON YOUR PAPER
Have a great spring break and be safe!