Childrens Illustrated World Atlas

(Marvins-Underground-K-12) #1

Key to map


Convergent


boundary


Less than 20 in (50 cm)


20–79 in (50–200 cm)


More than 79 in (200 cm)


December is


the southern


summer and


northern winter


Arctic Circle,


where Sun’s rays


are dispersed


Equator, where


Sun’s rays are


concentrated


March is the


northern spring


Sahara Desert


Atacama Desert,


Chile


The Sun


Rising


warm,


moist air


near


Equator


Rainforest,


Borneo


Tropic of


Capricorn


THE SEASONS


Earth spins on a tilted axis, so as it orbits the Sun once


a year the North Pole points towards the Sun in June and


away from it in December. This means that in regions


north of the tropics it is summer in June but winter


in December—and the opposite to the south of


the tropics. Near the Equator it is always warm,


but there are annual wet and dry seasons.


COLD POLE


The tropics are the hottest part of the


planet because the Sun’s rays strike them


directly, concentrating the heat energy.


Near the poles the same amount of heat


energy is spread out over a broader area,


so it does not have as much heating


effect, even in summer. At midwinter,


the entire polar region is in permanent


darkness, so it gets no solar energy at


all and is bitterly cold.


JUNGLE AND DESERT


Concentrated sunlight near the Equator heats


Earth’s surface, warming the air above. The warm


air rises, carrying moisture with it. This forms huge


clouds that spill tropical rain, fueling the growth


of rainforests. The dry, cooling air then flows north


and south and sinks over the subtropics, creating


deserts. Similar air circulation patterns affect the


climate in the far north and south.


ANNUAL RAINFALL


Some parts of the world get far more rain than others.


The wettest regions are mainly rainforest zones, where


year-round rain and warmth promote lush plant growth.


Regions of moderate rainfall are naturally forests and


grasslands, although much of this land is now used for


farming. The driest regions may be too dry for many


plants to grow, creating deserts—but they also include


some northern forest zones and polar tundra.


Descending cool,


dry air over


desert zone


Cold air (in blue)


becomes chilled in


upper atmosphere


Warm air (in red)


heats up near


Earth’s surface


Cool, dry air sinks


over desert zone


Tropic of


Cancer


Earth’s axis


v


Active Planet


South Pole


North Pole


June is the


northern


summer and


southern winter


US_iv-v_Active_Planet.indd 5 19/04/17 2:18 pm
Free download pdf