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Introduction
Chapter 1
Chapter 2
Chapter 3
Chapter 4
Chapter 5
Chapter 6
Chapter 7
Chapter 8
Chapter 9  
Chapter 10
Chapter 11
Chapter 12
Chapter 13
Chapter 14
Chapter 15
Chapter 16
Chapter 17
Chapter 18

Chapter 17 Weather Patterns

17-1    Air mass:

  1. Refers to huge body of air that has similar temperature and moisture. Small scale nonuniformity exists.

  2. Source region: when the air mass acquire its characteristics.

  3. Classification based on source region:

    • Polar (P)

    • Tropical (T)

  4. Classification based on surface feature:

    • Continental (c)

    • Maritime (m)

  5. Combination of 3 and 4: CP, CT, mP, mT.

  6. Where they are? Fig. 17.3.

  7. 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:

  1. Fronts: boundaries separate different air masses.

    • relatively narrow band.

    • mixing occurs along fronts.

  2. 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.

  3. Cold front: cold air advances to where warm air occupied before. Cold air invades. Fig. 17.7.

    • Use 4to represent. 4on the warm side.

    • Slope steep, subsiding.

    • rate of advancing fast.

    • temperature decreases.

    • moisture decreases.

  4. Stationary front: no movement of either air masses. Use both 4and w to represent. w on the cold side and 4on the warm side.

  5. 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:

  1. Middle-latitude cyclones. 

    • larger centers with low pressure.

    • counterclockwise circulation.

    • moving west to east.

    • cold front and warm front from center. Fig 17.10.

  2. 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:

  1. High cloud.

  2. Low cloud, precipitation, T rises. why? warm front.

  3. Tropical air, warm, wind direction: SW.

  4. Cold front, wind NW, dark cloud, P increases, T decreases.

  5. 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:

  1. Occurrence:

    • associated with cumulonimbus clouds.

    • occurred in tropical region often, warm air.

    • often form along or ahead of cold front.

  2. 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.