Page 604 - 9780077418427.pdf
P. 604

/Volume/201/MHDQ233/tat78194_disk1of1/0073378194/tat78194_pagefile
          tiL12214_ch23_565-596.indd Page 581  9/23/10  11:07 AM user-f465
          tiL12214_ch23_565-596.indd Page 581  9/23/10  11:07 AM user-f465             /Volume/201/MHDQ233/tat78194_disk1of1/0073378194/tat78194_pagefiles







                                                                           Polar




                                                                 Temperate







                                                                    Tropical





                                                                     Temperate



                                                                           Polar




                        FIGURE 23.24  The principal climate zones are defined in terms of yearly temperature averages, which are determined by the amount of
                        solar radiation received at the different latitude groups.


                           during the other part. Overall temperatures are cooler than
                           in the low latitudes and have a wide seasonal variation.
                         3. Th e high latitudes receive a maximum amount of radiation
                             during one part of the year and none during another part.
                             Overall temperatures are low, with the highest range of
                           annual tem peratures.
                           The low, middle, and high latitudes provide a basic frame-
                       work for describing Earth’s climates. These climates are asso-
                       ciated with the low, middle, and high latitudes illustrated in
                       Figure 23.23, but they are defined in terms of yearly temperature
                       averages. It is necessary to define the basic climates in terms of
                       temperature because land and water surfaces  react differently
                       to incoming solar radiation, creating a different temperature.
                       Temperature and moisture are the two most  important climate
                       factors, and temperature will be considered first.
                           The principal climate zones are defined in terms of
                       yearly tem perature averages, which occur in broad regions (Fig-
                       ure 23.24). They are                                      FIGURE 23.25  A wide variety of plant life can grow in a tropical
                                                                               climate. Here is a tropical plant with an orange and red flower.
                         1.  the tropical climate zone of the low latitudes (Figure 23.25),
                         2. the polar climate zone of the high latitudes (Figure 23.26),
                                                                               during some winter days. Overall, the polar climate zone is cold.
                           and
                                                                               Average monthly temperatures stay below 10°C (50°F), even
                         3. the temperate climate zone of the middle latitudes
                                                                               during the warmest month of the year.
                           (Figure 23.27).
                                                                                  The temperate climate zone is between the polar and tropi-
                       The tropical climate zone is near the equator and receives the   cal zones, with average temperatures that are neither very cold
                       greatest amount of sunlight throughout the year. Overall, the   nor very hot. Average monthly temperatures stay between 10°C
                       tropical climate zone is hot. Average monthly temperatures stay   and 18°C (50°F and 64°F) throughout the year.
                       above 18°C (64°F), even during the coldest month of the year.  General patterns of precipitation and winds are also associ-
                           The other extreme is found in the polar climate zone, where   ated with the low, middle, and high latitudes. An idealized model
                         the Sun never sets during some summer days and never rises   of the global atmospheric circulation and pressure patterns was

                        23-17                                                                  CHAPTER 23  Weather and Climate   581
   599   600   601   602   603   604   605   606   607   608   609