Page 304 - (DK) The Ultimate Visual Dictionary 2nd Ed.
P. 304

GEOLOGY, GEOGRAPHY, AND METEOROLOGY

       Weather                                                          Advancing cold   Warm air
                                                                             TYPES OF OCCLUDED FRONT
                                                                        front rises up
                                                                        over warm                  Warm
       WEATHER IS DEFINED AS THE ATMOSPHERIC CONDITIONS at a particular  front                     front
       time and place; climate is the average weather conditions for a given
       region over time. Weather is assessed in terms of temperature, wind,                         Cold air
       cloud cover, and precipitation, such as rain or snow. Good weather   Cool air
       is associated with high-pressure areas, where air is sinking. Cloudy,
       wet, changeable weather is common in low-pressure zones with               WARM OCCLUSION
       rising, unstable air. Such conditions occur at temperate latitudes,               Warm air
                                                                           Cold air                Warm
       where warm air meets cool air along the polar fronts. Here, spiraling                       front
       low-pressure cells known as depressions (mid-latitude cyclones) often   Cold front
       form. A depression usually contains a sector of warmer air, beginning   undercuts
                                                                        warm                        Cool air
       at a warm front and ending at a cold front. If the two fronts merge,   front
       forming an occluded front, the warm air is pushed upward. An
       extreme form of low-pressure cell is a hurricane (also called a             COLD OCCLUSION
       typhoon or tropical cyclone), which brings torrential rain
                                                                             FORMS OF PRECIPITATION
       and exceptionally strong winds.
                                                                       Water droplets less      Water droplets
                                                                       than 0.5 mm in              coalesce to
       TYPES OF CLOUD
                                                                       diameter fall            form raindrops
                        Cirrus           Cirrostratus                  as drizzle               0.5–5.0 mm in
                                                                                                    diameter
                                                                 13
                                                                        Rising air
        Cirrocumulus                                             12

                                                                 11
        Freezing level,                                                         RAIN FROM CLOUDS NOT
          above which                                                          REACHING FREEZING LEVEL
         clouds consist                                          10
        of  ice crystals                                                           Ice crystal    Snowflakes
                                                                        Coalesced                 grown from
                                                                  9     water droplets            ice crystals
        Cumulonimbus
                                                                        fall as rain              fall as snow
                                                                  8
                                                                                                  Snowflakes
         Altocumulus                                              7                               melt to fall
                                                                        Rising air                as rain
                                                                  6
           Altostratus
                                                                  5           RAIN AND SNOW FROM CLOUDS
                                                                               REACHING FREEZING LEVEL
             Nimbus
                                                                        Vertical air              Alternate
                                                                  4
                                                                        currents toss             freezing
        Stratocumulus                                                   frozen water              and melting
                                                                        droplets up               builds up
                                                                  3
                                                                        and down                  layers of  ice
            Cumulus
                                                                  2
         Nimbostratus                                                   Rising air                Ice falls as
                                                                  1                               hailstones
             Stratus
                                                                  0
                                                                 Altitude in
                                                                 temperate             HAIL
                       Condensation level
                                                                 regions (km)
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