Because the low latitudes of the Earth, the areas near the equator, receive more heat+ n6 K( q% A! n& o3 p) D
Than the latitudes near the poles, and because the nature of heat is to expand and move,' o4 b. j6 R" b) H" } O
Heat is transported from the tropics to the middle and high latitudes. Some of this heat is ) X" e# C% T% s: b
Line Moved by winds and some by ocean currents, and some gets stored in the atmosphere in , E% K0 u; P1 C4 o
(5) the form of latent heat. The term “latent heat” refers to the energy that has to be used to
7 O' b9 U5 m s1 {. @; vConvert liquid water to water vapor. We know that if we warm a pan of water on a stove,. A, X$ V( y X' C/ ^- d
it will evaporate, or turn into vapor, faster than if it is allowed to sit at room temperature.
+ v0 r: ~# @& `9 b2 x! u- S8 R2 R$ bWe also know that if we hang wet clothes outside in the summertime they will dry faster
. V0 \; A8 U: s1 o7 k2 mthan in winter, when temperatures are colder. The energy used in both cases to change $ U- [. U* g3 b7 f; W2 r9 p
(10) liquid water to water vapor is supplied by heat—supplied by the stove in the first case2 O; E+ ]9 [' Y: X) O1 K
and by the Sun in the latter case. This energy is not lost. It is stored in water vapor in the
8 ^! D- j" d; P' G1 ?& C% Gatmosphere as latent heat. Eventually, the water stored as vapor in the atmosphere will
8 @* M0 u1 N, l* F4 T+ Y3 [. L! I" p3 ccondense to liquid again, and the energy will be released to the atmosphere./ `$ U5 j/ y: k2 c' H. X# D) `
In the atmosphere, a large portion of the Sun’s incoming energy is used to evaporate
' O [4 S R/ e3 C- r- w2 R(15) Water, primarily in the tropical oceans. Scientists have tried to quantify this proportion
9 Q" M, V% H# _- rof the Sun’s energy. By analyzing temperature, water vapor, and wind data around the
! ^& E6 z5 b, p4 }8 Q$ d: }globe, they have estimated the quantity to be about 90 watts per square meter, or nearly 2 {/ M4 l/ `* _! j3 J+ q6 |2 o
30 percent of the Sun’s energy. Once this latent heat is stored within the atmosphere, it 9 z) G# I* y$ [1 u; c4 P
can be transported, primarily to higher latitudes, by prevailing, large-scale winds. Or it
( S; k4 r+ \8 E/ h# R(20) can be transported vertically to higher levels in the atmosphere, where it forms clouds' l- V' v* V1 d& J" |9 C: _$ H
and subsequent storms, which then release the energy back to the atmosphere.
$ O2 i' L0 d; ?. K8 H; z! s: E0 ?. Q31. The passage mainly discusses how heat ( {* W% D9 l* ] w, L
is transformed and transported in the Earth’s atmosphere
5 E) ? ]0 u& h3 Ois transported by ocean currents V- y, b c+ y' O- W8 p" U4 ~( i
can be measured and analyzed by scientists
; Z5 t7 e5 h$ v( m9 R" _% x& mmoves about the Earth’s equator
: C! i; W3 D8 L0 U32. The passage mentions that the tropics differ from the Earth’s polar regions in which of the following ways?( y! U$ c- W, s: `! F0 X- I$ _ i
The height of cloud formation in the atmosphere& a6 `1 O, C$ Q) W5 t( i7 X( v
The amount of heat they receive from the Sun
" i, a8 W- z, A( E2 FThe strength of their largescale winds.
- q" P- F( e# W0 i. ~The strength of their oceanic currents8 L, @2 J) ? \0 |6 ~6 b
33. The word “convert” line 6 is closest in meaning to
7 B3 Y8 e- o5 ^mix4 y+ {7 M( V/ @! n, m! ? m
change4 @! h1 Q0 _: B/ J
adapt1 t% }4 c& Q6 {
reduce1 P$ \9 T6 F2 G; d# q
/ f+ n) M1 M* U% ~, ^
34. Why does the author mention “the stove” in line 10?7 z7 K) [. _- o6 j8 V$ X+ `
To describe the heat of the Sun% K- e4 |) q D) D2 V- o
To illustrate how water vapor is stored# E# d2 Y1 f ]$ i) D+ J3 p [
To show how energy is stored" |5 u2 M! E) Q2 p! [
To give an example of a heat source |