19. According to the passage, late seventeenth- and early eighteenth-century
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Chinese records are impor- tant for which of the following reasons?
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" s. Z6 H; D2 `, S (A) They suggest that the data on which the Maunder minimum was predicated - }. w W4 o: T- f
$ d- m* Q9 y! ~" r were incorrect.
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(B) They syggest that the Maunder minimum can- not be related to climate.
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(C) Thcy suggest that the Maunder minimum might be \-'alid only for Europe.
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: |7 |+ f8 k% ]( P* f& I (D) They establish the existence of a span of unusu- ally cold weather
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$ Z6 i4 i0 W- Z) D9 B. e" {' C( r/ B worldwide at the time of the Maunder minimum.
1 r( [2 q- `+ f, P* b% C6 C
% c) a6 }; a! \* c7 q1 Y (E) They establish that solar activity at the tirne of the Maunder minimum & [" O; x$ N& { {: {" l( P
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did not significantly vary from its present pattern. 6 X9 r! c$ S# d1 ~, t9 W
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20. The author implies which of the followine about currently available
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geological and archaeoloeical evidence concerning the solar-activity cycle? S1 \/ R# V0 k
: ]8 l- _ O0 q (A) It best supports the model of solar activity described in lines 37-45.
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(B) It best supports the model of solar activity described in lines 45-52.
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(C) It is insufficient to confirtn either model of solar activity described ! x3 M- @2 G0 }7 k/ @' O: ?
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in the third paragraph. + m9 b+ t! M) x/ {8 J- Y
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(D) It contradicts both models of solar activity as they are presented in 1 P/ k1 L: h7 P/ U0 D
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the third paragraph.
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( a3 h; F- G, b' b0 p7 J+ o# y1 S (E) It disproves the theory that terrestrial weather and solar activitv are
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. ]/ n3 w: m. k linked in some way. . c2 I5 v0 g6 F6 ]+ {5 g
3 A2 ]3 ^4 p3 A$ C# ]( ` 21. Tt can be inferred from the passage that the argu- ment in favor of the
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; j% [. a1 b$ @3 |9 y model described in lines 37- 45 would be strengthened if which of the following
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: z9 z& o$ F' y; A/ S# a were found ta he tme?
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( g7 D5 o, ?- L/ i% u! h (A) Episodes of intense volcanic eruptions in the distant past occurred in
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3 K( ?+ S* \ p9 Z cycles having very long periodicities. # X7 |" o% f3 W; K9 E1 x- `- S! A
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(B) At the present time the global level of thunder- storm activity increases / \* v, \$ F, u
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and decreases in cycles with periodicities of approximately 11 years.
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* O. T: D9 M: ^' b9 I9 z0 M (C) In the distant past cyclical climatic changes had periodicities of longer & E8 G* ?' J% p: Y* v
9 h4 Z! D" B; U7 } than 200 years. ( S3 e3 j, `$ {7 M. C
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(D) In the last century the length of the sunspot cycle has been known to
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7 | v% V( J2 t; C0 g3 @ vary by as much as 2 years from its average periodicity of 11 years.
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(E) Hundreds of millions of years ago, solar- activity cycles displayed the
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same periodicities as do present-day solap-activity cycles. |