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问题 选择题

下面是大气对地面的保温作用示意图，据图回答1—2题。

1、图中太阳辐射、地面辐射、大气辐射、大气逆辐射的数码代号按顺序依次是[ ]

A、①②③④

B、③④②①

C、④③②①

D、②③④①

2、青藏高原比长江中下游平原气温日较差较大的原因是：①离太阳近、②青藏高原比长江中下游平原太阳高度角小、③云层厚且夜晚长、④地势高、空气稀薄、⑤白天太阳辐射强、⑥夜晚大气逆辐射弱 [ ]

A、①②③

B、④⑤⑥

C、③④⑤

D、①②⑥

答案

1、C

2、B

单项选择题

下列各进制的整数中，值最大的一个是( )。

A．十六进制数78

B．十进制数125

C．八进制数202

D．二进制数10010110
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单项选择题

The ocean bottom—a region nearly 2.5 times greater than the total land area of the Earth —is a vast frontier that even today is largely unexplored and uncharted. Until about a century ago, the deep-ocean floor was completely inaccessible, hidden beneath waters averaging over 3,600 meters deep. Totally without light and subjected to intense pressures hundreds of times greater than at the Earth’s surface, the deep-ocean bottom is a hostile environment to humans, in some ways as forbidding and remote as the void of outer space.
Although researchers have taken samples of deep-ocean rocks and sediments for over a century, the first detailed global investigation of the ocean bottom did not actually start until 1968, with the beginning of the National Science Foundation’s Deep Sea Drilling Project (DSDP). Using techniques first developed for the offshore oil and gas industry, the DSDP’s drill ship, the Glomar Challenger, was able to maintain a steady position on the ocean’s surface and drill in very deep waters, extracting samples of sediments and rock from the ocean floor.
The Glomar Challenger completed 96 voyages in a 15-year research program that ended in November 1983. During this time, the vessel logged 600,000 kilometers and took almost 20,000 core samples of seabed sediments and rocks at 624 drilling sites around the world. The Glomar Challenger’s core samples have allowed geologists to reconstruct what the planet looked like hundreds of millions of years ago and to calculate what it will probably look like millions of years in the future. Today, largely on the strength of evidence gathered during the Glomar Challenger’s voyages, nearly all earth scientists agree on the theories of plate tectonics and continental drift that explain many of the geological processes that shape the Earth.
The cores of sediment drilled by the Glomar Challenger have also yielded information critical to understanding the world’s past climates. Deep-ocean sediments provide a climatic record stretching back hundreds of millions of years, because they are largely isolated from the mechanical erosion and the intense chemical and biological activity that rapidly destroy much land-based evidence of past climates. This record has already provided insights into the patterns and causes of past climatic change—information that may be used to predict future climates.

Deep-ocean sediments provide better information about the world’s past climate because they______.

A. are well protected

B. have land-based evidence
C. are in isolation


D. have a longer history
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