|

|
Chapter 17 Weather
Patterns
17-1 Air mass:
-
Refers to huge body of air that has similar temperature and
moisture. Small scale nonuniformity exists.
-
Source region: when the air mass acquire its
characteristics.
-
Classification based on source region:
-
Classification based on surface feature:
-
Continental (c)
-
Maritime (m)
-
Combination of 3 and 4: CP, CT, mP, mT.
-
Where they are? Fig. 17.3.
-
Weather associated with
-
cP: not with heavy precipitation, cold and dry.
-
mT: with precipitation, warm, moisture, unstable.
-
cT: southwest, hot and dry.
17-2 Fronts:
-
Fronts: boundaries separate different air masses.
-
Warm front: warm air occupies where cold air occupied
before. Thus, warm invades.
-
Use w
to represent. w
on the cold air side.
-
slope is gentle, rising.
-
represented by cirrus cloud ==> cirrostratus ==>
altostratus ==> nimbostratus. Fig. 17.5.
-
rate of advancing: slow.
-
light to moderate precipitation.
-
temperature rises.
-
moisture rises.
-
Cold front: cold air advances to where warm air occupied
before. Cold air invades. Fig. 17.7.
-
Stationary front: no movement of either air masses. Use
both 4and
w
to represent. w
on the cold side and 4on
the warm side.
-
Occluded front: when cold front meets warm front: Fig.
17.8. Use both 4and
w
to represent. w
and 4on
the same side.
17-3 Middle-Latitude cyclone:
-
Middle-latitude cyclones.
-
larger centers with low pressure.
-
counterclockwise circulation.
-
moving west to east.
-
cold front and warm front from center. Fig 17.10.
-
Life cycle:
-
Easterly cold air and westerly warm air meet. Their
relative movement is counterclockwise. Fig. 17.9A.
-
Front not strait but wave ==> warm air move north and
cold air south. Warm front and cold front forms. Fig. 17.9C.
-
Cold front moves faster. As cold front meets warm front
==> occlusion forms. == cyclone mature.
-
warm air aloft, cold air lower elvel. Both
counterclockwise flow ==> cyclone dissipates.
17-4 Weather associated with a
cyclone:
Use Fig 17.10 as an example. Along section A-E:
-
High cloud.
-
Low cloud, precipitation, T rises. why? warm front.
-
Tropical air, warm, wind direction: SW.
-
Cold front, wind NW, dark cloud, P increases, T decreases.
-
High P, clear sky.
Around L in Fig. 17.10 wind is inward. Unless other
outlet exists, the inward move won't persist. Therefore, aloft provide a way for
constant air filling into low pressure center.
17-5 Thunderstorm:
-
Occurrence:
-
associated with cumulonimbus clouds.
-
occurred in tropical region often, warm air.
-
often form along or ahead of cold front.
-
Stages:
-
supply of moisture. When heated up, air rise ==>
cumulus stage.
-
when size of rain drops too large to experience uplift,
precipitation begins ==> mature stage.
-
downdraft dominates: air cool ==> dissipating stage.
17-6 Tornadoes:
-
Often associated with severe thunderstorms.
-
Often occur in late spring when air temperature contrast
bigger.
-
Air pressure lower in the center.
-
Classified on Fujita (F-scale) based on degree of damage.
Most are F0 -F1 low damage tornadoes.
-
Often occur in great plain where cP meets mT.
17-7 Hurricanes:
-
Sometimes called typhoons or cyclones.
-
have to have minimum speed: 119 km/h rotary circulation.
-
pressure low in center, thus inward wind direction.
-
near center wind upward to form cumulonimbus tower ==>
eye wall.
-
at center, no precipitation, light wind ==> eye.
-
initial: large volume of warm air normal on ocean. Typically
late summer when water temperature is high.
-
release of latent heat cause upward movement.
-
scale set 1-5 based on wind speed and central pressure.
-
evolution from tropical depression to tropical storm to
hurricane.
-
damage due to wind, surge, and flood.
Homework:
-
Read chapter summary on p.487.
-
Use your own word to explain the key terms on page 488.
-
Answer the review questions on page 488.
|