T/G Layout 1

(C. Jardin) #1
283

ey, Question 3, a–f, page 282

Pair-Share Worksheet

3a. the tropical latitudes, especially 0°

3b. Year-round direct heating of the equatorial regions causes the air to expand over
the equatorial regions and the warmed air to rise.

3 c .When the moist air reaches the “ceiling” of the troposphere (imposed by the
s t r a t o s p h e re), it will be forced to diverge—moving poleward. As it moves away fro m
the equator, the air cools—becoming more dense and sinks back toward Eart h.

3d. moist—as a result of strong surface evaporation

3e. tall thunderstorms, that is, cumulonimbus clouds

3f. yes. 10°N–10°S

K

Free download pdf