Part E: Chapter 19 Answers to  Review Questions

 

  1. In winter a cP air mass is very cold and dry, whereas in summer it is cool and dry. In both instances, such an air mass is usually associated with high pressure and clear skies. Its cool temperatures are often welcome relief in summer.

 

  2. A maritime tropical (mT) air mass is humid because it originates over water and warm because it forms in tropical latitudes. Source areas for mT air masses are the Gulf of Mexico, Caribbean Sea and adjacent Atlantic Ocean, and the Pacific, west of Mexico. Maritime polar (mP) air masses originate in the North Pacific and off the eastern coast of Canada in the North Atlantic.

 

  3. Warm, moist air (which is usually unstable) is abruptly lifted along the steeply sloping cold front. Cumulonimbus clouds are created, which may bring thunderstorms and occasionally other severe weather such as hail or tornadoes. After the front passes, a sharp temperature drop is experienced as the winds shift to the northwest.

 

  4. An occluded front forms in the late stage of development of a middle-latitude cyclone when the faster-moving cold front catches up to the warm front and the warm (mT) air is forced aloft. The warm, moisture-laden air is wedged out of the picture, and eventually the cyclone dissipates. Once there is no warm, moist air being lifted, there is little condensation and latent heat release.

 

  5. As the warm front approaches, winds will blow from the east or southeast and pressure will drop steadily. Cirrus clouds will be sighted first, followed by cirrostratus, altostratus, and finally nimbostratus. Cloud cover will progressively increase, from a few tenths coverage with cirrus, to completely overcast with the coming of the nimbostratus. Gentle precipitation will begin as the nimbostratus clouds move overhead. As the warm front passes, temperatures will rise, precipitation will cease, and winds will shift to the south or southwest. Further, the sky clears and the pressure stabilizes.

 

      Later, with the approach of the cold front, cumulonimbus clouds fill much of the sky and bring the likelihood of heavy precipitation and the possibility of hail and tornado activity. The passage of the front is accompanied by a drop in temperature, clearing skies, a wind shift to the northwest, and rising pressure. Fair weather can probably be expected for the next day or two.

 

 

  6. As the low approaches, cool temperatures are the rule, for the warm sector of the cyclone is to the south. The pressure drops and the sky becomes increasingly overcast. Further, precipitation is to be expected, and if it is winter or early spring, possibly snow, sleet, or glaze. As the occluded front slowly passes, winds shift from the north or northeast to the northwest. The sky begins to clear and the barometric pressure rises. Temperatures, however, remain cool or cold.

 

  7. Divergence aloft initiates upward air movement, reduced surface pressure, and cyclonic air movement. In contrast, convergence along the jet stream results in general subsidence of the air column, increased surface pressure, and anticyclonic surface winds.

 

  8. Tornadoes, with diameters of about 0.25 kilometer, and hurricanes, with diameters of about 600 kilometers, are both smaller and more violent than middle-latitude cyclones, whose diameters may be 1600 kilometers or more. Thunderstorms, which are characterized by up-and-down air movements rather than the inward spiral of a cyclone, are related in some manner to all three types of these cyclones.

 

  9. Since thunderstorms are produced in towering cumulonimbus clouds, a prime requirement is warm, moist, unstable air.

 

10.  In areas where warm, moist, and unstable air is very common, that is, the tropics. In the United States thunderstorms are most common during the summer months and likely most prevalent in the Southeast near the primary source of maritime tropical air.

 

11.  Because of the very low pressure within the tornado there is a very steep pressure gradient and, hence, very high wind speeds.

 

12.  Tornadoes are most often spawned along the cold front of a middle-latitude cyclone in association with severe thunderstorms. During spring, the air masses on either side of the cold front are most likely to have greatly contrasting conditions.

 

13.  Although tornadoes can occur in every month of the year, spring (April–June) is the period of greatest tornado activity.

 

14.  A tornado watch alerts the public to the fact that conditions are right for the formation of tornadoes. A tornado warning is issued when a tornado has actually been sighted in an area or is indicated by radar.

 

15.  With wind speeds between 61 and 115 kilometers per hour, a tropical storm has stronger winds than a tropical depression.

 

16.  (a) Wind speeds were probably highest on Thursday, because Hurricane Fran had a lower pressure and closer-spaced isobars on that day.

 

      (b) The hurricane moved approximately 400 miles. The average rate of movement was 400 miles/24 hours = 16.6 miles per hours (mph).

 

17.  The three broad categories of hurricane damage are (1) wind damage, (2) storm surge, and (3) inland freshwater flooding. Storm surge is responsible for the greatest percentage of hurricane-related deaths.

 

18.  The most likely cause is the heavy rains and inland flooding that can affect places far from the coast for several days.

 

19. Since the hurricane is so much larger and lasts not for a fraction of an hour but for days, the destruction it causes is considerably greater than that caused by a tornado.

 

 

Answers to Earth System Questions

 

  1.          High snowfalls on the leeward shores of the lakes occur when the atmosphere, hydrosphere (the Great Lakes), and solid Earth interact. This lake-effect snow develops during autumn and winter as cold cP air travels over the warm lakes, acquires large quantities of moisture from the water, and becomes humid and unstable. The result is often heavy snow showers over the cooler land on the downwind shores of the Great Lakes.

 

 

  2. The most devastating damage from a hurricane is caused by the storm surge. As the water moves over low-lying land, loss of life, destruction of buildings, and severe erosion are possible. Wind damage can affect a much larger area than the storm surge, often uprooting trees and destroying buildings. Heavy rains may also cause extensive flooding and severe erosion hundreds of kilometers from the coast. Following a hurricane, it may take years for the eroded land, disrupted drainage network, and destroyed natural vegetation to reestablish or be repaired.