A country's latitude, or distance from the equator,8 J6 [4 l) j* C9 b8 Z
has an important effect on its climate. In places
' s; `& H5 I5 p8 k locating at low latitudes, or near the equator, like__1__# q+ h; M3 F* T& ~( W8 V
Ecuador and northern Brazil, the amount of sunshine
" l5 H5 p' ^* a8 M% G* z changes the most during the years. At mid-latitudes, in __2__
' d- c& U6 O3 d4 P2 G, Q! ]: D0 d places like Japan or Argentina, there is less sunshine__3__1 _6 \- g* M+ Z8 v0 f$ G; ~ |
in the summer than in winter. The greatest change: M/ W- J" e8 i( ?0 N; U2 D: J
occurs at the highest latitudes, in places like northern2 a9 u$ R1 n9 @/ n9 y2 a
Canada and Alaska. In these places, the nights are very
" R; k D. @- Z G long for half the year, and the days are long during3 _3 x/ Q$ E+ @) _7 d/ l" T- a# R& G# r
other half. At the North or South Pole, sunlight lasts __4__
, ^: |( d a3 L$ x+ L# a the longest during the winter. But light and heat are __5__
- S- o) b" `6 W( s2 O- J/ _ the most intense at the equator.7 U; S+ \0 {, n% d {$ ]0 b. w
Altitude and distance from the sea also affect climate./ C. O" R ~& i
The thin air in the high mountain areas absorb less of the __6__
* N. ?4 R/ T: m( Y, d3 I* |; u sun's heat than the thicker air at sea level. The daily: j, z& ?# k( {1 p; m% C
change in temperature also increases with distance! R: {4 K* [1 L, `. k
from the sea. Snow and rain are not very important to __7__) U6 V0 K$ P% l) X% c# s( ?* F
climate. Snow reflects as much as eighty or ninety
% ^, S' N, O6 e3 ? percent of the heat from the sun, and making the __8__- v0 E' M! r* C4 e; D. u/ Z* c( q9 J
weather even colder. But a large forest area can reflect$ A V: @: v8 i* v- b) c; v! [
as little as five percent of the sun's heat. This makes5 l+ O! r2 L: N+ K3 _9 q
the weather warmer. Of course, the general effects of
q6 ?/ P" m( D0 }0 e- A4 G climate do not explain everything about the weather.
* }2 d1 H' ~$ `5 r% m For example, either the driest places in the world and __9__
) y7 R1 Z! L7 R the place with the most rainy days are located in Chile.2 b) M: e1 P8 J9 [* N' [3 Y
Calama, in the Atacama Desert, has had no rain over__10__
5 X n$ [6 J) |5 I# j 400 years. But during the year 1916, it rained in Bahia0 K4 e2 b1 D& J, d
Felix, Chile for 348 days.% N% e0 x$ ^4 ^3 e5 E
答案及解析:
" M* L, I' `, g2 P* x1 q% ~3 R4 x 1. locating—located* g* h$ z& d; Q
locate作位于解释时,常常用被动语态8 x) K' X% H( S4 @8 o. x/ F3 K' Y; i
2. most—least
' r2 A+ Q* g# b2 q/ }) d' e 根据上下文及常识,低纬度或赤道地区的日照量变化最小- ]0 V1 X- }! c1 W5 E! Z5 Y3 W
3. less—more
& I% V5 K8 h1 P# g. ^% ` R$ z 常识告诉我们,诸如日本,阿根廷等纬度不高不低的国家或地区,夏季的日照要比冬季的日照多得多& r# e6 ~. K- o6 ]- i2 F
4. 在other前加the5 Y5 G2 i- }& y- w# ?3 D0 ~
是指另外半年。other用于the、my、your、his等之后与一单一名词连用,意义为“两个中的另一个”. [) G9 v; o% ~1 M% G( {7 u
5. winter—summer1 B( _: y6 ^" E8 z) \5 J
根据常识或科普知识可得
* \. e, y3 y4 e# I1 H 6. absorb—absorbs
5 ~# @9 B6 t$ w the thin air是动词absorbs的主语, Y$ E4 e: I/ T
7. 删除not
$ V7 A3 r- Z2 \& l1 V$ E 我们的常识和下文Snow reflects as much as eighty or ninety percent of the heat from the sun, and making the weather even colder.能充分说明如果该句中有not一次是彻底错误的。
: r: C; R' o4 I( [% C1 N 8. making—makes. B5 A/ N" p6 `" t: d2 M
makes the weather even colder由and链接reflects as much as eighty or ninety percent of the heat from the sun. U0 z' r- s) Z* n4 h
9. either—both
w8 C" `0 K: W8 O2 b( {& e7 { 首先是下文的and;其次,谓语动词是are located" T7 R' B' I/ x
10. 在over前插入for
) g# S& G( Y3 E& }4 q9 ` for用于表示一段时间,作为时间状语,其修饰的谓语动词常常用完成时。 |